Skip to main content

AI assistant

Sign in to chat with this filing

The assistant answers questions, extracts KPIs, and summarises risk factors directly from the filing text.

SUNSTONE METALS LTD Capital/Financing Update 2025

Nov 23, 2025

65870_rns_2025-11-23_8fbf8a7b-86de-468a-a77b-3f9ddc5550de.pdf

Capital/Financing Update

Open in viewer

Opens in your device viewer

ASX ANNOUNCEMENT

24 NOVEMBER 2025

==> picture [283 x 46] intentionally omitted <==

- Bramaderos Gold Copper Project, Southern Ecuador Resource jumps 33% to 3.6Moz AuEq[1] underlining project’s world-class scale Expanded inventory includes Indicated Resources of 600,000oz AuEq; Huge scope for more growth with the Exploration Target rising 17%

Key Points

  • Bramaderos Mineral Resource Estimate (MRE) increases by 900,000oz AuEq[1] to 3.6Moz AuEq[1]

  • The Resource includes 600,000oz AuEq in the Indicated category (a 200% increase on the previous 200,000 AuEq[2] ), establishing a strong foundation on which to commence scoping studies at Bramaderos for an open-pit mine development

  • The Resource is limited to the pit-constrained Brama-Alba-Melonal porphyry deposits, further demonstrating scope for growth

  • Future drill programs are expected to drive rapid Resource growth

Plus Gold and Copper Exploration Target of 5Moz - 13Moz AuEq[1]

  • New Copete-Porotillo Exploration Target of between 135 - 180Mt at a grade between 0.4 - 0.6g/t AuEq[1] for 1.7Moz – 3.5Moz AuEq reflects the highly successful 2025 exploration program

  • High confidence in overall Porphyry Exploration Target of between 315 - 505Mt at a grade between 0.41 and 0.69g/t AuEq[1 ] for 4Moz – 11Moz AuEq

  • Large cluster of porphyry systems at Bramaderos across an area of 2km by 2km, all at surface and expected to be developed as a straightforward low-cost open-pit operation

  • Exploration Target covers Brama-Alba (in addition to MRE), Melonal, Copete-Porotillo and the upper section of Limon porphyry. All systems are at surface

  • Complements existing Limon higher-grade epithermal Exploration Target of between 30 - 40Mt at a grade between 0.9-1.2g/t AuEq[3] for 0.9Moz – 1.7Moz AuEq[3]

  • The potential quantity and grade of the Exploration Targets is conceptual in nature. There has been insufficient exploration to estimate a Resource for the reported exploration target areas. It is uncertain if further exploration will result in the estimation of a Resource

1 The gold equivalent (AuEq) calculation formula for porphyry gold-copper-silver mineralisation at Bramaderos is AuEq (g/t) = ((Au grade x Au price x Au recov / 31.1035) + (Ag grade x Ag price x Ag recov / 31.1035) + (Cu grade x Cu price x Cu recov / 100)) / (Au price x Au recov / 31.1035). The prices applied were US$1,800/oz gold, US$4.50/lb copper and US$22/oz silver. Recoveries are estimated at 88% for gold, 85% for copper and 60% for silver based on metallurgical studies. In Sunstone’s opinion, all the elements included in the metal equivalents calculation have reasonable potential to be recovered and sold.

2 Refer to ASX announcement 13 December 2022 – Maiden MRE Brama-Alba, Figure 2 below and Table 1 Section 3 below

3 The gold equivalent calculation formula for the Limon epithermal gold-silver mineralisation is AuEq(g/t) = Au(ppm) + (Ag (ppm)/82). The prices used were US$1,800/oz gold and US$22/oz silver. Recoveries are estimated at over 90% for gold and 90% for silver from metallurgical studies. In Sunstone’s opinion all the elements included in the metal equivalents calculation have reasonable potential to be recovered and sold

Sunstone Metals Limited ABN 68 123 184 412 ASX: STM

L31, 120 Collins St +61 3 7044 2627 Melbourne V 3000 [email protected] Australia sunstonemetals.com.au

REGISTERED OFFICE

Sunstone Managing Director Patrick Duffy said: “This is an outstanding result which adds huge additional value to Bramaderos and shows beyond doubt that it is rapidly emerging as a world-class project in an ideal location.

“The project now boasts a resource of 3.6Moz of gold-equivalent, with grades that outperform those of many other major open-pit porphyry projects and has a clear path to rapid, substantial increases.

“The resource is all comfortably within open pit depths and with 600,000oz AuEq now in the higher-confidence Indicated category, we will undertake a scoping study that will underscore the project’s immense value”.

==> picture [472 x 540] intentionally omitted <==

Figure 1 : Overview of key prospects on the Bramaderos project, the Brama-Alba-Melonal resource area, and Exploration Target areas defined on the Bramaderos properties.

2

1. November 2025 Bramaderos Mineral Resource estimate

The November 2025 Bramaderos MRE is 220Mt at 0.5g/t AuEq[1] (0.33g/t gold, 0.10% copper and 1.2g/t silver) for 3.6 Moz AuEq[1] at a cut-off grade of 0.3g/t AuEq[1] (reported in accordance with the JORC Code[4] , see Table 1 below for more details). Preliminary pit optimisation was applied to the deposit to constrain the MRE and demonstrate the potential to be mined economically by open pit methods (Figures 4, 5, 6 and 7). A very low strip ratio is implied by the block model geometry within the pit.

Table 1. November 2025 Bramaderos Mineral Resource estimate at a 0.30g/t AuEq cutoff grade

Grades Grades Contained Metal Contained Metal Contained Metal
Deposit Classification Tonnes
(Mt)
AuEq
(g/t)
Au
(g/t)
Ag
(g/t)
Cu
%
AuEq
(Koz)
Cu
(Mlbs)
Cu
(Kt)
Bramaderos Indicated 40 0.56 0.38 1.26 0.10 600 90 40
Bramaderos Inferred 190 0.49 0.32 1.14 0.10 2,900 410 190
Bramaderos Total 220 0.50 0.33 1.16 0.10 3,600 490 220

Notes:

  • Figures may not sum due to rounding.

  • Significant figures do not imply an added level of precision.

  • Reported at 0.30g/t AuEq cutoff grade – Sunstone criteria

  • AuEq (g/t and ounces) accounts for Au (g/t), Cu (%) and Ag (g/t) value and AuEq (g/t and ounces) is not be totalled to Cu (% and/or lbs and/or tonnes) or Ag (g/t and/or ounces).

  • Sunstone metallurgical investigations at Base Met Labs Kamloops, the Au recovery is 88%, Ag recovery is 60% and Cu recovery is 85%

  • Sunstone metal price investigations and projections, Au price US$1800/oz, Ag price US$22/oz and Cu price US$$4.50/lb (US$9,921/t).

The November 2025 MRE is based on 59 drill holes (53 drilled by Sunstone from June 2019 to February 2023 and 6 drilled by Ecuador Gold in 2007) for a total of 29,006 metres of drilling, and 5,385 linear metres of trenching and channelling from 32 trenches and channels. Several historic holes were excluded from the resource because they did not meet QA/QC requirements.

Sunstone engaged Spiers Geological Consultants (SGC), an independent consulting firm, to prepare the updated Bramaderos MRE.

Sighter metallurgical test work has been completed on various mineralisation styles from the Brama-AlbaMelonal gold-copper porphyry deposit. Studies were conducted by Base Metallurgical Laboratories in Kamloops, British Columbia. The test work shows that recoveries of over 85% for copper and 88% for gold can be achieved with a combined flotation and leach circuit when aiming for a saleable concentrate grade above 20% copper (see ASX release dated 19 July 2022). The geology of other targets included in the Exploration Target shows strong similarities to Brama-Alba-Melonal (not uncommon in a clustered porphyry geological environment), and it is considered valid to apply metallurgical testwork results to these other areas when deriving a metal equivalent value.

The 33% increase (900koz’s AuEq both Indicated and Inferred) in the Bramaderos Mineral Resource (December 2022 versus November 2025) is driven by:

  1. The addition of Inferred material from drilling at Melonal (355koz’s AuEq).

4 Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves. The JORC Code, 2012 Edition. Prepared by: The Joint Ore Reserves Committee of The Australasian Institute of Mining and Metallurgy, Australian Institute of Geoscientists and Minerals Council of Australia (JORC).

3

  1. A greater contribution from Brama-Alba (533koz’s AuEq). For Brama-Alba, the updated geological model incorporates new data from Brama-Alba proximal to Melonal, which accounted for the majority of the increase.

  2. The impact from pricing assumptions was very minor (12koz’s AuEq), with the gold price remaining at US$1800/oz and copper increasing from US$4.20 to US$4.50/lb.

Melonal contains no Indicated mineral resources, and the increase to 600koz of Indicated resources from 200koz in 2022 is due to the addition of new drillholes and trenching data, providing both closer-spaced information and the ongoing refinement of the geological model in the Brama-Alba area.

==> picture [496 x 178] intentionally omitted <==

Figure 2: Comparison of 2022 to 2025 Bramaderos MRE

Table 2 below presents the mineral resource estimate across a range of cut-off grades. The pricing assumptions and cut-off grade applied—outlined in Section 3.9—were selected conservatively based on peer group benchmarking. It should be noted that under a long-term gold price scenario of $4,000/oz, a significantly larger open pit would be generated when considering Reasonable Prospects for Eventual Economic Extraction, and a substantially lower cut-off grade would be appropriate.

Table 2– Bramaderos November 2025 Mineral Resource estimate at various cut-off grades (Total of both Indicated and Inferred)

COG Tonnes
(Mt)
AuEq
(g/t)
Au
(g/t)
Ag
(g/t)
Cu
(g/t)
Cu
%
AuEq
(Moz)
Au
(Moz)
Cu
(Kt)
0.1 370 0.38 0.25 0.95 770 0.08 4.5 2.9 280
0.2 300 0.44 0.29 1.05 880 0.09 4.2 2.7 260
0.3 220 0.50 0.33 1.16 990 0.10 3.6 2.3 220
0.4 150 0.58 0.38 1.28 1110 0.11 2.8 1.8 170
0.5 90 0.66 0.45 1.38 1230 0.12 1.9 1.3 110
0.6 50 0.76 0.52 1.49 1350 0.14 1.2 0.8 70

Notes:

  • Figures may not sum due to rounding.

  • Significant figures do not imply an added level of precision.

AuEq (g/t and ounces) accounts for Au (g/t), Cu (%) and Ag (g/t) value and AuEq (g/t and ounces) is not totalled to Cu (% and/or lbs and/or tonnes) or Ag (g/t and/or ounces).

  • Sunstone metallurgical investigations at Base Met Labs Kamloops, Au recovery is 88%, Ag recovery is 60% and Cu recovery is 85%

  • Sunstone metal price investigations and projections, Au price US$1800/oz, Ag price US$22/oz and Cu price US$$4.50/lb (US$9,921/t).

4

==> picture [487 x 397] intentionally omitted <==

Figure 3: Brama-Alba-Melonal drill status plan showing the status of Sunstone drilling, historical drilling, plus trenching and surface channel sampling for the November 2025 MRE on a backdrop of gold-in-soil results.

5

==> picture [489 x 398] intentionally omitted <==

Figure 4: Plan view of Brama-Alba-Melonal and showing the updated optimised model open-pit outline (blue outline), the updated resource block model, and the location of a long-section (A-A’) and two cross-sections (B-B’ and C-C’) as shown in Figures 5, 6 and 7.

6

==> picture [488 x 369] intentionally omitted <==

Figure 5: Long-section (100m section thickness) through Brama-Alba and showing the November 2025 block model, diamond drillholes with AuEq assays and the modelled pit. Areas are also show where the resource remains open below the pit and form part of the Brama-Alba porphyry exploration target. Location of section (A-A’) is shown in Figure 4.

7

==> picture [489 x 430] intentionally omitted <==

Figure 6: Cross-section through Brama and showing the November 2025 block model, diamond drillholes with AuEq assays and the modelled pit. Areas are also shown where the resource remains open below the pit and form part of the Brama-Alba porphyry exploration target. Location of section (B-B’) is shown in Figure 4.

8

==> picture [488 x 348] intentionally omitted <==

Figure 7: Cross-section through Melonal and Alba and showing the November 2025 block model, diamond drillholes with AuEq assays and the modelled pit. Areas are also shown where the resource remains open below the pit and form part of the Brama-Alba and Melonal porphyry exploration targets. Location of section (C-C’) is shown in Figure 4.

9

==> picture [489 x 552] intentionally omitted <==

Images 1 and 2: Views across the Porphyry Exploration Targets of Melonal and Porotillo (top), and across part of the resource area of Brama-Alba-Melonal as viewed from the northern end of the Copete-Porotillo Porphyry Exploration Target (bottom).

10

2. Bramaderos Exploration Target

The total Exploration Target within the Bramaderos concessions is based on two deposit styles and is estimated from five areas:

  1. The new Porphyry Exploration Target at Copete-Porotillo

  2. The extensions to the Brama-Alba porphyry system that are not captured in the MRE (see ASX announcement 13 December 2022), excluding component converted to updated Nov-25 resource.

  3. Porphyry Exploration Target at Melonal (see ASX announcement 13 December 2022), excluding component converted to updated Nov-25 resource.

  4. Porphyry Exploration Target at Limon (limited to upper section from surface) (see ASX announcement 13 December 2022)

  5. Limon Epithermal Exploration Target (see ASX announcement 5 February 2024)

The Exploration Target does not include known porphyry mineralisation at Sandia, Playas or Yeso. It was decided not to include these areas because Sunstone has not yet completed any or sufficient drilling in these areas. Further work in these areas may be undertaken in future to assess if they can contribute to an expanded future Exploration Target and Mineral Resource.

Table 3: Summary of Exploration Targets at the Bramaderos Project (in addition to the November 2025 Brama-Alba MRE).

Exploration Target Min Tonnage Max Tonnage Metal Content Metal Content Metal Content Metal Content
(MT) (MT) Min kAuEq Max kAuEq Min Moz AuEq Max Moz AuEq
ounces ounces
New Copete-Porotillo(Po) 135 180 1,700 3,500 1.70 3.50
Updated Brama-Alba-Melonal-Limon(Po)5 180 325 2,400 7,700 2.40 7.70
SUB-TOTAL PORPHYRY 315 505 4,100 11,200 4.10 11.20
Limon (Epithermal)6 30 44 900 1,700 0.90 1.70
BRAMADEROS PROJECT TOTAL 345 549 5,000 12,900 5.00 12.90
Exploration Target Min Tonnage Max Tonnage Min Grade Au Min Grade Cu Min Grade Ag Min Grade
(MT) (MT) (g/t) (%) (g/t) AuEq (g/t)
New Copete-Porotillo(Po) 135 180 0.25 0.10 - 0.40
Updated Brama-Alba-Melonal-Limon(Po)5 180 325 0.26 0.10 - 0.41
SUB-TOTAL PORPHYRY 315 505 0.26 0.10 - 0.41
Limon (Epithermal)6 30 44 0.80 - 12 0.90
BRAMADEROS PROJECT TOTAL 345 549 0.30 0.09 1.0 0.45
Exploration Target Min Tonnage Max Tonnage Max Grade Au Max Grade Cu Max Grade Ag Max Grade
(MT) (MT) (g/t) (%) (g/t) AuEq (g/t)
New Copete-Porotillo(Po) 135 180 0.40 0.12 - 0.60
Updated Brama-Alba-Melonal-Limon(Po)5 180 325 0.54 0.12 - 0.74
SUB-TOTAL PORPHYRY 315 505 0.48 0.12 - 0.68
Limon (Epithermal)6 30 44 1.10 - 15.8 1.20
BRAMADEROS PROJECT TOTAL 345 549 0.54 0.11 1.3 0.73

Notes:

  • Figures may not sum due to rounding.

  • Significant figures do not imply an added level of precision.

5 See ASX announcement 13 December 2022

6 See ASX announcement 5 February 2024

11

The previous Porphyry Exploration Target range of contained gold-equivalent ounces estimated in 2022 was between 255 - 360Mt at a grade between 0.40 - 0.74g/t AuEq for 3.3 MOz AuEq to 8.6 MOz AuEq[5] , while the Limon Epithermal Exploration Target range of contained gold-equivalent ounces estimated in 2023 was between 30 - 40Mt at a grade between 0.9-1.2g/t AuEq for 0.9 MOz AuEq to 1.7 MOz AuEq[6] .

Adjusting for the enlarged Brama-Alba-Melonal MRE, a small portion of the Melonal and Brama-Alba Exploration Target has been reduced.

With the addition of the new Porphyry Exploration Target defined for Copete-Porotillo, and including the Limon Epithermal Exploration Target, the Total Bramaderos Project Exploration Target (covering both porphyry and epithermal deposit styles) is now between 345 - 549Mt at a grade between 0.45g/t AuEq and O.73 g/t AuEq for 5.0 and 12.9 Moz AuEq.

2.1. New Copete-Porotillo Exploration Target

The initial Copete-Porotillo Exploration Target is between approximately 135Mt and 180Mt at a grade between approximately 0.4g/t to 0.6g/t AuEq (0.25g/t to 0.40g/t gold and approximately 0.10% to 0.12% copper) for contained metal of between 1.7Mozs to 3.5Mozs AuEq (see Table 3).

The Copete-Porotillo Exploration Target has been reported in accordance with the JORC Code[4] . The potential quantity and grade of the Exploration Target is conceptual in nature. There has been insufficient exploration to estimate a Mineral Resource for the target area reported. It is uncertain if further exploration will result in the estimation of a Mineral Resource.

Table 4 summarises the Copete-Porotillo Exploration Target components, which are further described in the section ‘Exploration Target Methodology and Summary of Additional Material Information’.

Table 4 – Copete-Porotillo Exploration Target

Zone Min
Tonnage
(Mt)
Max
Tonnage
(Mt)
Min
Grade g/t
AuEq
Max Grade
g/t
AuEq
Min.
AuEq
(Moz)
Max.
AuEq
(Moz)
Copete-Porotillo 120 160 0.40 0.60 1.5 3.1
Porotillo 15 20 0.4
0.36 0.60 0.2
TOTAL COPETE-POROTILLO
EXPLORATION TARGET
135 180 0.4 0.6 1.7 3.5

Note: Figures may not sum due to rounding.

12

==> picture [488 x 432] intentionally omitted <==

Figure 8: Plan view of the Copete and Porotillo porphyry exploration target footprints at surface projected onto surface mineralisation defined in trenches, channel samples, rockchip samples and soil samples, and underlying mineralisation intersected in 13 historical drillholes.

13

3. Summary of Material Information – Mineral Resources

3.1. Geology and Geological Interpretation

The deposit styles include intrusion-related and stockwork-hosted porphyry gold-copper systems, as well as epithermal gold-silver-polymetallic veins. The geological setting is a volcanic arc of Cretaceous-age intrusions.

At least eight distinct intrusion phases span the entire mineralisation-alteration sequence, with the main orebearing phases comprising of distinct intrusion phases, with the main ore-bearing phases comprising porphyry diorite intrusions and associated crystalline intrusion breccias.

The principal rock types are assigned to four broad units: (1) the pre-mineralisation sedimentary and dacitic to andesitic volcanic rocks; (2) two early-mineralisation intrusive phases; (3) three syn-mineralisation porphyry intrusion and associated intrusion breccia phases that span the alteration-mineralisation sequence; and (4) late-mineralisation intrusions, mill breccia dykes and post-mineralisation andesite dykes.

The MRE covers the Brama-Alba porphyry system and the upper northeast part of the Melonal porphyry system. A series of geological models was created to inform the estimation process. The lithology model covering Brama-Alba was expanded to include areas of recent surface sampling around Brama-Alba and Melonal, and was important for constraining the estimation.

An alteration model was also created in Leapfrog 3D modelling software to assist in defining the geometry of mineralisation at Brama-Alba-Melonal. The alteration model was created from 17 sets of 50m-spaced manual long-section interpretations through Brama-Alba and an additional six level-plan interpretations at Melonal. These 23 interpretations were georeferenced into Leapfrog software and were used to guide the creation of 3D surfaces around the modelled alteration domains. The alteration model was used to validate the reliability of the lithology model in the estimation process.

A series of vein models were also created to assess if they could be used to subdomain the estimation area. Four sets of vein models were created using Leapfrog software’s 3D contouring algorithms and using search ellipses that reflect the deposit geometry. Models were created for “A-type”, “B-type” porphyry quartz vein abundances, “M-type” porphyry magnetite vein abundances and for “A+B+M-type” vein abundances. The models validated the broad geometry defined in the lithology and alteration models and thus provided further support for the use of the lithology model for subdomaining in the estimation process.

A weathering model was generated using Leapfrog Geo and follows the topography profile. Strongly weathered, moderately weathered and fresh zones were modelled.

In addition to the weathering model, an interpretation was made of the boundary between oxide and sulphide copper minerals. Oxide copper (mainly cuprite) is restricted to a shallow supergene blanket (~8-10m thick) in areas of mineralisation and extends further down along faults in isolated areas. This boundary allowed the removal of oxide material prior to resource reporting, given that it is not likely to be recovered during processing.

3.2. Sampling and Sub-Sampling Techniques

Diamond core and trench sampling were adopted for the project.

For Sunstone holes, the routine sample procedure is to always take the half core to the right of the orientation line (looking down the hole) or the cut line (when the orientation line was unreliable). The drill core sampling was carried out using half core, generally at 1 to 2 m intervals.

14

Trench samples were collected at 1-2 m intervals using a portable cutting machine, a hammer, and a chisel, depending on rock hardness, and then arranged in numbered plastic bags. Sampling intervals honour changes in lithology, weathering, alteration, mineralisation, and structural information.

Drill core and trench samples from Bramaderos were sent to the LAC y Asociados Cia. Ltda. Sample Preparation Facility in Cuenca. The pulps were then sent to the MSA Analytical Laboratory in Vancouver for gold and base metal analysis. The standard sample preparation for drill core samples (Code PRP-910) involves drying the sample, crushing to a size fraction of 70% < 2mm, and splitting the sample into a 250 g portion for trenches and a 1,000 g portion for drill core using a riffle or Boyd rotary splitter. The 250/1000g sample is then pulverised to >85% passing 75 microns and then split into two 50g pulp samples.

Limited details are available on sampling and sub-sampling techniques used by Ecuador Gold. It is known, however, that half of the core samples were dispatched by bus to the Inspectorate sample preparation laboratory in Quito, from where pulps were subsequently shipped to Peru for analysis.

Quality control (QC) data indicate acceptable sampling precision for all reported elements.

3.3. Drilling and Trenching Techniques

All drilling completed at the project is diamond core.

Drilling commenced in the project area in 1999 and has been carried out in three phases as follows:

  • Ecuanor S.A. completed 13 diamond holes (CURI01-13) from 1999 through 2000.

  • Ecuador Gold S.A. completed 22 diamond holes (EGCU001-022) from 2006 through 2007.

  • Sunstone completed 130 diamond holes (BMDD001-050, ESDD001-011, LMDD001-054, WZDD001008, SADD001-003, MEDD001-002 and PLDD001-002) from 2019 through 2024.

Ecuanor S.A. holes were not used in this MRE due to the absence of QC data and an apparent inconsistency between the tenor of mineralisation and that observed in nearby recent holes.

Core sizes are not known for the Ecuador Gold holes.

Sunstone holes constitute the majority of the data used for this MRE. There are 53 Sunstone holes (including one wedge) totalling 27,052 metres, along with six historical holes measuring 1,954 metres, bringing the total to 34,390 metres. The holes were drilled using either HTW (70.9mm) or NTW (56mm). Drill core was oriented with a Reflex ACT II tool. Diamond core recovery was recorded for each drill run and documented in digital logging software. The data has been reviewed, and core recovery was nearly 100% throughout. The Bramaderos Project database contains 130 drill holes by Sunstone Metals, but only 53 holes fall within the immediate area of the MRE. Sunstone holes constitute the majority of the data used for this MRE.

A total of 73,225 metres has been drilled on the Bramaderos property, including all historical drilling (10,426 metres) and STM drilling in areas both outside and within the resource (27,052 metres).

A total of 86 trenches and 42 surface channel sample runs were excavated by Sunstone from 2017 to 2025 using a combination of handheld tools (pick and shovel), reaching depths of up to 2m with a minimum width of 1m. A supervising geologist oversaw the excavations. Only 13 trenches are situated within the immediate area of the MRE. Channel and trench samples are carefully collected and surveyed using DGPS for the start, end, and midpoint of each sample.

3.4. Location of Data Points

The grid system used is Geocentric Datum of Ecuador PSAD56 Zone 17 South.

15

A topographic digital terrain model (DTM) generated from DGPS data using the following equipment:

  • 1x Sokkia 630RK Total Station with a precision of 6 seconds

  • 3x Trimble R4 GNSS differential RTK with a precision of ± 2cm RTK.

  • 1x CHCNav i90 Pro

Total Station methods were used for closed areas, and GPS RTK for open areas.

All drill holes completed by Sunstone have been located (collars) using a DGPS. Downhole surveys were completed using a Reflex Gyro Sprint-IQ Gyroscope at 5 metre intervals. Validation involves measuring the differences between the input and output measurements. The measurement is within the acceptable range when the maximum difference is less than 1%.

Trenches and channels have been surveyed using a DGPS, with pickups at the start, midpoint, and end.

Each hole has one survey record at the collar. The original collar positions of two of the six holes used for the resource were identified, and a DGPS survey was carried out. The original collar locations are within an acceptable range of deviation from the updated DGPS measurements. A single-shot magnetic Pajari tool was employed to measure the dip and azimuth at the collar.

3.5. Criteria used for Classification

The Mineral Resource has been classified following due consideration of all criteria contained in Section 1, Section 2 and Section 3 of JORC 2012 Table 1. The Mineral Resource has been classified as either Indicated or Inferred based on data quality, sample spacing, mineralisation continuity, confidence in the geological interpretations, estimation quality statistics, and metallurgical processing knowledge. No Measured material has been defined. After evaluating data quality, data distribution, and geological and grade continuity, the following approach was adopted when classifying the Mineral Resource:

  • Broadly speaking, areas of the deposit were classified as Indicated where the deposit is tested on a pattern which approximates 20–40 m E by 20–40 m RL. Geological evidence is considered sufficient to assume geological and grade continuity between points of observation where data and samples are gathered. A wireframe was created to capture this area.

  • Broadly speaking, areas of the deposit were classified as Inferred where drilling had been completed on a pattern which approximates 40–80 m E by a 40–80 m RL. Geological evidence is considered sufficient to imply, but not to verify, geological and grade continuity.

  • In both instances, in addition to drilling density search, data minimum criteria were required to be met. For Indicated, a minimum of 2 drill holes over a minimum of 4 octants and a minimum of 12 data points were required; for Inferred, the same conditions were employed, with the minimum data reduced to 6.

  • Estimation domain continuity was also taken into account within the regional and local scale structural context from the viewpoint of lithological, alteration and vein density variability when assessing final classification decision making.

3.6. Sample Analysis Method

Sunstone uses a Fire Assay gold technique for Au assays (FAS-111) and a four-acid multi-element technique (IMS-230) for a suite of 48 elements. FAS-111 involves Au by Fire Assay on a 30g aliquot, fusion and atomic absorption spectroscopy (AAS) at trace levels. IMS-20 is considered a near-total 4-acid technique using a 20g aliquot, followed by multielement analysis by ICP-AES/MS at ultra-trace levels.

16

Ecuador Gold used a 30g fire assay method for gold analysis, and a multi-element suite was analysed using a four-acid multi-element technique (IMS–230).

QC data demonstrates that acceptable analytical accuracy has been achieved for all reported elements, and there were no issues with carry-over contamination.

3.7. Geological models for Resource estimation

Lithology and alteration models were created from initial interpretations of drilling data on multiple-level plans or long sections. Lithology and alteration outlines were then digitised into 2D polylines in Leapfrog, from which three-dimensional solids were created.

The weathering model was generated using Leapfrog Geo and broadly follows the topography profile. Strongly weathered, moderately weathered and fresh zones were modelled.

Copper sulphide species, mainly chalcopyrite, are found in many trenches and drill hole collars above the mineralisation zone. Logged copper sulphides and assay results are analysed, and areas potentially containing oxides are sent for petrographic analysis. This approach shows that the surface conditions of the porphyry zones, from the surface to depths of about 4-10 metres, are typically transitional, with sulphides incompletely oxidised and copper and gold still recoverable.

3.8. Estimation Methodology

The Ordinary Kriging technique was considered appropriate by the competent person for estimation purposes (using third-party software) based on statistical analysis, which revealed that the datasets in question exhibited low coefficients of variation across all modelling domains and elements, suggesting adequate homogeneity and local stationarity across key modelling domains.

Grade interpolation and search ellipses were developed based on variography and geometric modelling outcomes. Modelling was conducted in three passes with parent block sizes being 25.0 m E by 25.0 m N by 10.0 m RL.

In the first pass, the data and octant criteria used were at least 12 data points, no more than 32, and a minimum of 4 octants. Consistent with the initial structure ranges of the prevailing variogram analysis, the search radii applied were 20 mE by 30 mN by 15 mRL, with rotations aligned with the prevailing lithological controls and the potential plunge of the host and controlling units, following the right-hand rule.

An expansion factor of 1 was applied, so in the second pass, the same data and octant criteria were seen with an expanded search to 40mE by 60mN by 30mRL.

The third pass saw Minimum Data=6, maximum Data=32, Minimum Octants=2. The search radii were 40mE by 60mN by 30mRL. A final extended pass was completed, whereby the search radii employed were akin to the third structure ranges of the variogram analysis at or near 60mE by 75mN by 30mRL.

Top cutting was applied to domains and elements that displayed very strongly skewed distributions, outliers, and high-end members, in accordance with the prevailing coefficients of variation.

No dilution was explicitly added to the model; however, domaining was primarily driven by lithological, alteration, vein density, and grade domains, which tend to incorporate the full population range in the lithological domains and a constrained population range in the grade domains, in line with the grade domain statistical constraints.

The interpretation or domain model was primarily driven by lithology/geology, alteration, vein density, oxidation state, structural interventions, and mineralised trends observed across the various project areas. Grade was used as a secondary domain driver to define boundary conditions where deemed appropriate.

17

The model was validated in third-party software using section and plan comparisons back to the original data, as well as using swath plots to assess local grade variability between the model and the original data.

3.9. Cut-off Grades

The MRE is reported above a cut-off grade of 0.3g/t AuEq. The cut-off grade was selected based on the proposed open-pit mining method and preliminary pit optimisation results. Tonnages were estimated on a dry basis.

Pit optimisation was implemented to enable constraints on reporting and as the basis for Reasonable Prospects for Eventual Economic Extraction.

Table 5 – Base case pit optimisation parameters Parameter Value Unit
Au metal price 1,800 US$/oz
Cu metal price 4.50 US$/lb
Ag metal price 22 US$/oz
Mining cost 2.10 US$/t mined
Mining losses 0 %
Mining dilution 0 %
Processing cost 6.80 US$/t ore
G&A 1.50 US$/t ore
Transportation, Shipping, Smelting, Refining 2.00 US$/t ore
Sustaining Capital 1.60 US$/t ore
Recovery – Copper 85 %
Recovery – Gold 88 %
Recovery – Silver 60 %
Pit slope 35 Degrees
Rehabilitation of Waste Dump?? 0.10 $/t of waste
Grade-control drilling of Ore 0.10 $/t of ore

3.10. Assessment of Reasonable Prospects for Eventual Economic Extraction

Clause 20 of the JORC Code (2012) requires that all reports of Mineral Resources must have reasonable prospects for eventual economic extraction, regardless of the classification of the Mineral Resource. The Competent Person deems that there are reasonable prospects for eventual economic extraction of mineralisation on the following basis:

  • Mineralisation at Bramaderos is continuous and has been delineated by drilling over a strike length of approximately 1.2 km, while at Alba, mineralisation is continuous for 0.2 km along strike. Mineralisation at Melonal also appears to be relatively continuous. Given the broad widths of mineralisation, strip ratios will be low and minimal dilution and ore loss are expected.

  • Access to power infrastructure.

  • Metallurgical test work results were encouraging. Furthermore, metallurgical head assays indicated no interference from deleterious elements.

18

  • Preliminary pit optimisation results show that the deposit has the potential to be mined economically by open pit methods.

  • There is significant potential for the discovery of additional Mineral Resources within the Bramaderos concession. This will allow Sunstone to continue to benefit from the economies of scale potential at Bramaderos.

4. Exploration Target Methodology and Summary of Additional Material Information

The Exploration Target within the Bramaderos concession is estimated from five areas:

  1. The new Porphyry Exploration Target at Copete-Porotillo;

  2. The extensions to the Brama-Alba porphyry system that are not captured in the MRE;

  3. Porphyry Exploration Target at Melonal;

  4. Porphyry Exploration Target at Limon (limited to upper section from surface); and,

  5. Limon Epithermal Exploration Target

The Exploration Target does not include known porphyry mineralisation at Sandia, Playas, or Yeso. It was decided not to include these areas because Sunstone has not yet completed any drilling in them, or sufficient drilling. Further work in these areas may be undertaken in future to see if they can contribute to an expanded Exploration Target.

4.1. New Exploration Target – Copete-Porotillo

A new porphyry exploration target has been defined over an area that spans the Copete and Porotillo porphyry systems.

Substantial exploration activity has occurred over these two areas. This includes grid soil sampling at a 100 x 50m spacing (37 elements) at Porotillo, grid soil sampling at a 50 X 50m spacing (37 elements) at Copete, acquisition of helimagnetic, ground magnetic and radiometric data plus lithology and alteration mapping over both prospects, historical and Sunstone rock chip sampling at Porotillo (187 samples) and Copete (122 samples), three historic trenches at Porotillo (33 samples), one trench ML-01 at Copete (149 samples), channel sampling along 12 ravines at Copete (348 samples), plus historic drilling at both prospects. Eleven historic drillholes were drilled at Porotillo by Ecuanor S.A. and Ecuador Gold S.A. (for 4194.41m) whilst two historic drill holes were drilled at Copete by Ecuador Gold S.A. (for 580.02m).

Both the Copete and Porotillo porphyry systems lie within a single large and enveloping gold-in-soil geochemical anomaly greater than 0.2 g/t gold and greeater than 350 ppm Cu.

At Copete on the northeast side of the soil geochemical anomaly, there are two syn-mineral intrusions at surface that exhibit strong quartz stockwork mineralisation within the intrusions and with weaker stockworks in the surrounding host rock. These intrusions cover an area of up to approximately 270m by 240m and exhibit silicic-argillic, argillic and minor advanced argillic alteration from the lower parts of a lithocap that overprint remnant potassic alteration. Trench ML-01 across the central part of these outcropping mineralised intrusions yielded 214m @ 0.50 g/t AuEq (ASX announcement 12 November 2024) whilst channel sample from ravines QC-02A and QC-03 yielded 63.7m @ 0.44 g/t AuEq and 60.20m @ 0.44 g/t AuEq respectively. The mapped mineralised intrusions are open to the southwest where they plunge under shallow alluvial cover of a narrow valley floor that runs between Copete and Porotillo.

At Porotillo within the main body of the gold-in-soil geochemical anomaly, an extensive early-mineral quartz diorite intrusion hosts overprinting porphyry-related, disseminated and vein stockwork mineralisation over an area spanning up to approximately 530m by 310m. Very substantial historic drill intersections were

19

encountered at Porotillo and included EGCU003 (74m @ 0.73 g/t AuEq), EGCU005 (390m @ 0.40 g/t AuEq, and CURI05 (157.04m @ 0.54 g/t AuEq which included 23.9m @ 1.47 g/t AuEq (1.21 g/t Au, 0.17% Cu)).

On the basis of the extensive surface and sub-surface geochemical datasets at Porotillo and Copete, two domains were identified where there is coherent and elevated mineralisation defined in soil samples, rockchip samples, channel and trench samples, and in historical drilling.

The first mineralised domain for which an exploration target has been defined (“Copete-Porotillo”; see Table 4 and Figure 8) is approximately 700m long by approximately 200m wide, trends northeast and spans the Porotillo and Copete prospects. This domain contains sheeted porphyry-related quartz veins at both the Copete and Porotillo ends of the domain, which strike northeast-southwest parallel to the mineralised domain, which reinforces its geometry. The surface area of this domain was calculated in QGIS to be 129,745m[2] . The zone has been tested in three historic drill holes down to vertical depths of 140m, 370m and 530m in historical holes CURI05, EGCU005 and EGCU006. The target tonnage for this domain was based on the surface area footprint of mineralisation, a depth of 400m and a rock density of 2.7 g/cc, with estimated tonnage centered within the quoted range of 120 to 160 Mt. The assigned grade range of 0.40 g/t AuEq to 0.60 g/t AuEq was selected to span the calculated average grade (0.46 g/t AuEq) of the series of 10 bulk intersections encountered in six historical drill holes, a surface trench and three surface ravines which averaged 0.46 g/t AuEq. The upper end of the grade range was selected to account for evidence of significant areas at surface at Porotillo where grade in surface samples range from 0.71 g/t Au to 6.64 g/t Au.

The second mineralised domain for which an exploration target has been identified (“Porotillo”; see Table 4 and Figure 8) is an ovoid domain of up to approximately 255m by 170m in dimension that lies on the northwest side of the main Porotillo gold-in-soil anomaly. This domain is hosted in an early mineral quartz diorite intrusion locally transected by a mapped syn-mineral quartz diorite dyke and associated intrusion breccia. The surface area of this domain was calculated in QGIS to be 36,830m[2] . The zone has been tested in two historic drill holes, down to vertical depths of 185m and 135m, in EGCU008 and EGCU009, respectively. The target tonnage for this domain was based on the surface area footprint of mineralisation, a depth of 200m and a rock density of 2.7 g/cc, with estimated tonnage located at the upper end of the quoted range of 15 to 20 Mt.

The assigned grade range of 0.36 g/t AuEq to 0.60 g/t AuEq was selected to span the calculated average grade (0.38 g/t AuEq) of the 2 bulk intersections encountered in historical drill holes EGCU008 and EGCU009. The upper end of the grade range was selected to account for evidence of significant areas at the surface, based on the eleven surface rockchip samples within the domain footprint, which averaged 0.54 g/t Au.

4.2. Existing Exploration Target - Brama-Alba Extensions

See ASX release – 13 December 2022.

Several areas of mineralisation have been identified outside of the area of the MRE. Further drilling is planned to assess the opportunity to move these areas into a future update of the MRE.

The November 2025 MRE captured all material above 0.3 g/t AuEq within a pit. Some drill holes that intersected mineralisation are widely spaced and inadequate drilling exists in these areas to show continuity. Furthermore, the effect of the RPEEE was to exclude 31% of material. This material has been captured in the Exploration Target.

Six domains were identified as having clear potential for additional mineralisation and these were reviewed either on a depth slice basis, or a block basis. Volumes were calculated and grade was assigned based on nearby data and on comparison with the overall Brama-Alba grade.

20

These areas have been included in an Exploration Target where more drilling is required to allow inclusion in a Mineral Resource estimate. The contribution of Brama-Alba extensions to the porphyry exploration target has been reduced to account for that part of this exploration target that has been converted to resource in the current MRE update.

4.3. Existing Exploration Target - Melonal

See ASX release – 13 December 2022.

The Melonal target is a continuation of the Brama-Alba system. It is geologically grouped with Brama-Alba. Recent drilling by Sunstone, and historical drilling from 2007, has confirmed that the Melonal target is mineralised, and that mineralisation is hosted in rocks the same as those drilled at the nearby Brama-Alba deposit. The mineralised rocks are coincident with a discrete sub-vertical magnetic anomaly measuring up to 400m in diameter, and with a vertical extent of over 1,000m. The Exploration Target for Melonal was considered to a depth of 500m. The Melonal target straddles the Sunstone Bram-01 concession and the Sunstone Bram-02 concession. The contribution of Melonal to the porphyry exploration target has been reduced to account for that part of this exploration target that has been converted to resource in the current MRE update.

4.4. Existing Exploration Target - Limon Porphyry

See ASX release – 13 December 2022.

Sunstone has drilled eight effective diamond holes at the Limon porphyry target. Mineralisation has been intersected in a number of holes. A trench was completed at Limon prior to drilling in an area of outcropping stockwork veining and minor secondary copper mineralisation. It returned 97m at 0.73g/t gold and 0.23% copper. A recent hole drilled under the trench has intersected similar stockwork veined intrusive and contains chalcopyrite.

Additional exploration holes into the deep central part of the Limon porphyry system will be planned.

4.5. Existing Exploration Target - Limon Epithermal

See ASX release – 5 February 2024.

Drilling at the Limon epithermal system has intersected an intermediate sulphidation epithermal system in numerous drill holes including LMDD017, 26, 30, 32, 38, 40, 43 and 46-51. Drill Intersections include 185m @ 2.85 g/t AuEq (include 31m @ 12.93 g/t AuEq) in LMDD026, and 269m @ 1.05 g/t AuEq (include 11m @ 14.15 g/t Au) in LMDD040.

The volume ranges for the initial Exploration Target in the Central Shoot were estimated using cross sections and 3-D modelling in Leapfrog software, based upon an analysis of drilling, mineralised rock types, grade distribution, potential for extrapolation of mineralisation continuity and interpreted geological risk.

The volume ranges for the other components were estimated from geological interpretation and guided by the extent of surface geochemical anomalism, supplemented by preliminary drilling. A conservative approach was taken to the potential distribution of gold and silver-bearing veins.

The Central Shoot has been outlined based on the geological interpretation of the gold- and silver-bearing mineralised fault and vein networks with both NE and NW trending trends, and dissemination of gold and silver into various host rocks. Within the Central Zone there are sub-domains of very high grade – as seen in holes LMDD017, 026, 038, and 040. These very high grades are interpreted to be associated with hydrothermal breccias at fault intersections. The Exploration Target assumes that at least one other sub-domain of high

21

grade will be drilled during subsequent drill programs. This will likely increase the overall grade and increase contained ounces.

Grade ranges in Table 3 have been selected based on average intervals from existing drilling over broad intersections.

4.6. Exploration Target Planned Activities and Timeframe

A scoping study on the development of the Brama-Alba resource is about to commence following completion of this MRE update, and will aim to demonstrate a base case for a porphyry development at Brama-Alba during the first half of 2026.

There are several priorities for ongoing work on the exploration target components, which will be prioritised as the scoping study progresses. The immediate priorities are to continue to expand the Bramaderos Resource inventory in 2026 and include drilling at the Limon epithermal system, Brama-Alba-Melonal porphyry system and the new Copete-Porotillo target.

==> picture [418 x 448] intentionally omitted <==

Figure 9: Location of Sunstone’s Bramaderos, El Palmar, and Verde Chico projects in Ecuador.

22

For further information, please visit www.sunstonemetals.com.au

Mr Patrick Duffy Media:
Managing Director Paul Armstrong
Sunstone Metals Ltd Read Corporate
Email:[email protected] +61 8 9388 1474

Mr Patrick Duffy, Managing Director of Sunstone Metals Ltd., has authorised this announcement to be lodged with the ASX.

About Sunstone Metals

Sunstone Metals Limited (“Sunstone” or “Company”) is an ASX-listed mineral exploration company with two world-class gold and copper projects in Ecuador:

  1. The Bramaderos Project , located in Southern Ecuador, contains the November 2025 Mineral Resource estimate of 220Mt at 0.50g/t AuEq for 3.6Moz gold-equivalent[1] .
JORC
Classification
Tonnage
(Mt)
Au
(g/t)
Cu
(%)
Ag
(g/t)
AuEq1
(g/t)
AuEq1
(Mozs)
Indicated 40 0.37 0.11 1.26 0.56 0.6
Inferred 190 0.32 0.10 1.19 0.49 2.9
Total 220 0.33 0.10 1.20 0.50 3.6

Additionally, the Bramaderos Project has a Porphyry Exploration Target of between 4.1Moz and 11.2Moz AuEq[1] within 315 to 505Mt at a grade between 0.41 and 0.68g/t, and the Limon epithermal gold-silver Exploration Target of between 0.9 and 1.7Moz AuEq[3,6] within 30 to 44Mt at a grade between 0.9 and 1.2g/t.

  1. The El Palmar Project is located in northern Ecuador, 60km north-west of Ecuador’s capital Quito. The property sits on the regionally significant Toachi Fault Zone that hosts a number of world-class copper porphyry systems. The Project has both at-surface and deeper porphyry gold-copper systems and an initial Mineral Resource estimate of 64Mt at 0.60g/t AuEq[7,8] for 1.2Moz AuEq[8] .
JORC Classification Tonnage
Mt
Average Grade Average Grade Average Grade Average Grade Average Grade Material Content Material Content Material Content Material Content
AuEq8
(g/t)
Au
(g/t)
Ag
(g/t)
Cu
(ppm)
Cu
(%)
AuEq9
(Koz)
Au
(Koz)
Ag
(Koz)
Cu
(Kt)
Indicated 5 0.63 0.42 0.81 1,456 0.15 100 100 100 7
Inferred 59 0.59 0.40 0.65 1,290 0.13 1,100 700 1,200 70
TOTAL 64 0.60 0.41 0.66 1,301 0.13 1,200 800 1,300 80

7 Refer ASX Announcement on 22 October 2024.

8 The AuEq calculation formula for porphyry gold-copper-silver mineralisation at El Palmar is AuEq (g/t) = ((Au grade x Au price x Au recov / 31.1035) + (Ag grade x Ag price x Ag recov / 31.1035) + (Cu grade x Cu price x Cu recov / 100)) / (Au price x Au recov / 31.1035). The prices applied were US$1,800/oz gold, US$4.50/lb copper and US$22/oz silver. Recoveries are estimated at 90% for gold, 78% for copper (excluded for oxide material), and 60% for silver based on metallurgical studies. Grades for the Exploration Target are 0.30g/t Au and 0.10% Cu. In Sunstone’s opinion all the elements included in the metal equivalents calculation have reasonable potential to be recovered and sold

23

Additionally, the El Palmar Project has a porphyry Exploration Target[9] of between 15Moz and 45Moz AuEq[8] within 1.0 to 1.2Bt at a grade between 0.3 - 0.7g/t gold and 0.1 – 0.3% copper.

Strategy

The porphyry projects at Bramaderos and El Palmar have the potential to evolve into multi-decade goldcopper mining centres. At Bramaderos, the Limon epithermal deposit has been prioritised as a potential nearsurface high-grade gold-silver development opportunity. This strategy allows for a scalable operation to be established first before developing the much larger porphyry gold-copper-silver opportunities at Bramaderos.

The Company continues to evaluate potential new opportunities to continue to grow our business in Ecuador, where clear shareholder value can be demonstrated. It is also evaluating potential partnerships for its projects where this may maximise the value of the portfolio.

Track Record

The team at Sunstone has been involved in significant discoveries of porphyry and epithermal copper-gold mineralisation at Tujuh Bukit in Indonesia and Cascabel in Ecuador, and the successful development of the King of the Hills Gold Mine in Western Australia and Koniambo Nickel Mine and Smelter in New Caledonia. The Company continues to attract specialist resources executives and is well-placed to repeat that success at Bramaderos and El Palmar.

Excellent infrastructure

All projects are supported by established infrastructure close to power, road and rail infrastructure and ports.

Community support

The Board and Management Team take their responsibilities towards the host communities seriously and have endeavoured to uphold the highest ESG standards across our business. Sunstone published its inaugural Sustainability Report in 2023, outlining the level of support and engagement with local communities and project stakeholders.

9 The potential quantity and grade of the Exploration Target is conceptual in nature. There has been insufficient exploration to estimate a Resource for the exploration target area reported. It is uncertain if further exploration will result in the estimation of a Resource.

24

Competent Persons Statement

The information in this report that relates to Mineral Resources is based on information compiled by Mr Rob Spiers. Mr Rob Spiers is a full-time employee of Spiers Geological Consultants (SGC), and is a Member of the Australasian Institute of Geoscientists (AIG). Mr Spiers has sufficient experience relevant to the style of mineralisation and type of deposit under consideration and to the activity which he is undertaking to qualify as a Competent Person as defined in the 2012 Edition of the Australasian Code for the Reporting of Exploration Results, Mineral Resources and Ore Reserves (JORC Code). Mr Spiers holds 0.016% of the ordinary shares on issue of Sunstone Metals, and this shareholding does not constitute a substantial holding in the Company, nor does it impair Mr Spiers’s ability to provide an objective and unbiased assessment. The shareholding is disclosed in accordance with the JORC code transparency provisions. Mr Spiers consents to the disclosure of the information in this report in the form and context in which it appears.

The information relating to the El Palmar Mineral Resource is extracted from the ASX announcement on 22 October 2024. The company confirms that it is not aware of any new information or data that materially affects the information included in the original market announcements and that all material assumptions and technical parameters underpinning the estimates in the relevant market announcements continue to apply and have not materially changed. The company confirms that the form and context in which the Competent Person’s findings are presented for their respective Mineral Resource estimates have not been materially modified from the original market announcements.

The information in this report that relates to exploration results and Exploration Targets is based upon information reviewed by Dr Bruce Rohrlach, who is a Member of the Australasian Institute of Mining and Metallurgy. Dr Rohrlach is a full-time employee of Sunstone Metals Ltd and has sufficient experience which is relevant to the style of mineralisation and type of deposit under consideration and to the activity which he is undertaking to qualify as a Competent Person as defined in the 2012 Edition of the “Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves”. Dr Rohrlach consents to the inclusion in the report of the matters based on his information in the form and context in which it appears.

Information on Exploration Targets

Bramaderos

The Bramaderos porphyry Exploration Target within the Bramaderos concession is estimated from four areas – the extensions to the Brama-Alba system that are not captured in the Mineral Resource estimate (MRE), the majority of the Melonal system that is not captured in the Mineral Resource estimate (MRE), and mineralisation drilled at the targets of Limon and Copete-Porotillo porphyry mineralisation.

The Exploration Target does not include known porphyry mineralisation at Sandia, Playas or Yeso. It was decided to not include these areas because Sunstone has not yet completed any or sufficient drilling in these areas. Further work in these areas will be undertaken and they are expected to contribute to an expanded Exploration Target in future.

Several areas of mineralisation have been identified outside of the area of the MRE. The MRE captured material that was drilled to sufficient density an economically modelled pit. Inadequate drilling exists in some areas both within and outside the modelled pit to show mineralisation continuity. Furthermore, the effect of the reasonable prospects of eventual economic extraction was to exclude 31% of material. This material has been captured in the Exploration Target.

Six domains were identified as having clear potential for additional mineralisation and these were reviewed either on a depth slice basis, or a block basis. Volumes were calculated and grade was assigned based on nearby data and on comparison with the overall Brama-Alba grade. This exploration target was reduced by the amount of material within it that was converted to resource by the latest MRE update.

25

The Melonal target is a continuation of the Brama-Alba system. It is geologically grouped with Brama-Alba. Recent drilling by Sunstone, and historical drilling from 2007, has confirmed that the Melonal target is mineralised, and that mineralisation is hosted in rocks the same as those drilled at the nearby Brama-Alba deposit. The mineralised rocks are coincident with a discrete sub-vertical magnetic anomaly measuring up to 400m in diameter, and with a vertical extent of over 1,000m. The Exploration Target for Melonal was considered to a depth of 500m. The Melonal target straddles the approved Bramaderos-01 and Bramaderos02 concessions. This exploration target was reduced by the amount of material within it that was converted to resource by the latest MRE update.

Sunstone has drilled 8 effective diamond holes at the Limon porphyry target. Mineralisation has been intersected in a number of holes. A trench (LM_TR_01) was completed at Limon prior to drilling in an area of outcropping stockwork veining and minor secondary copper mineralisation. It returned 97m at 0.73g/t gold and 0.23% copper. A recent hole drilled under the trench has intersected similar stockwork veined intrusive and contains chalcopyrite.

This area around Trench TR_LM_01 has been included in the porphyry Exploration Target where more drilling is required to allow inclusion in a Mineral Resource estimate.This target area will be further explored with drilling programs to be executed over the next two years, subject to the Company’s funding ability.

Copete and Porotillo

The Copete and Porotillo exploration targets are areas of outcropping porphyry stockwork veining that occur within an extensive gold and copper soil geochemical anomaly. These areas have seen substantial historical drilling (13 drill holes) with extensive mineralised intersections, plus widespread rockchip sampling of surface mineralisation, channel sampling in ravines and an extensive mineralised trench ML-01 at Copete that assayed 214m @ 0.50 g/t AuEq (ASX announcement 12 November 2024).

At Porotillo, within the main body of the gold-in-soil geochemical anomaly, an extensive early-mineral quartz diorite intrusion hosts overprinting porphyry-related, disseminated and vein stockwork mineralisation over an area spanning up to approximately 530m by 310m. Very substantial historic drill intersections were encountered at Porotillo and included EGCU003 (74m @ 0.73 g/t AuEq), EGCU005 (390m @ 0.40 g/t AuEq, and CURI05 (157.04m @ 0.54 g/t AuEq which included 23.9m @ 1.47 g/t AuEq (1.21 g/t Au, 0.17% Cu)).

Two domains were modelled to generate the Copete-Porotillo exploration target to depths of 200m and 400m below surface.

This target area will be further explored with drilling programs to be executed over the next two years, subject to the Company’s funding ability.

Limon epithermal

The Limon epithermal Exploration Target was estimated on target prospects where there was a combination of diamond drilling (by Sunstone), geological mapping, trenching, geochemistry (soils) and to a lesser extent geophysical data (magnetics) which could support the geological and mineralisation concept model.

The Limon alteration area has been covered with soil sampling on a 50m x 50m grid. This survey is an important exploration method which identified several gold-in soil anomalies that are primary targets for drilling. The soil geochemical data is further interpreted using related element associations typical of epithermal systems, such as areas of somewhat coincident gold, silver, zinc, lead, copper, tellurium and arsenic. Target areas have also been strengthened using alteration mineralogy from a hand-held Terraspec instrument. These data assist in mapping the alteration zones most likely to be associated with epithermal mineralisation.

26

Drilling at Limon has also intersected an intermediate sulphidation epithermal system in numerous drill holes including LMDD017, 26, 30, 32, 38, 40, 43 and 46-51. Drill intersections include 185m @ 2.85 g/t AuEq (include 31m @ 12.93 g/t AuEq) in LMDD026, and 269m @ 1.05 g/t AuEq (include 11m @ 14.15 g/t Au) in LMDD040..

Standard geological mapping and rock chip sampling has also been undertaken across the Limon target area.

The volume ranges for the initial Exploration Target in the Central Shoot were estimated using cross sections and 3-D modelling in Leapfrog software, based on drilling, mineralised rock types, grade distribution, potential for extrapolating mineralisation continuity, and interpreted geological risk.

The volume ranges for the other components were estimated from geological interpretation and guided by the extent of surface geochemical anomalism, supplemented by preliminary drilling. A conservative approach was taken to the potential distribution of gold and silver-bearing veins.

This target area will be further explored with drilling programs to be executed over the next year, subject to the Company’s funding ability.

El Palmar

The Exploration Target within the El Palmar concession is estimated from within the T1, T2 and T3 areas.

The Exploration Target does not include interpreted or known porphyry mineralisation at the T4 and T5 target areas. It was decided not to include these areas because Sunstone has not yet completed any drilling at T4 and has conducted only minor drilling at T5. Further work in these areas will be undertaken and they are expected to contribute to an expanded Exploration Target in future.

The components of the exploration target are based on a combination of diamond drilling conducted by Codelco (during 2012) and by Sunstone (during 2022 and 2023), ground magnetics, multi-element soil sampling, multi-element rock chip and channel sampling, mulit-element trench sampling and deep magnetic inversion anomalies modelled from ground magnetic data.

Wireframes of domains within the Exploration Target areas were created in Leapfrog software using data interpreted from the Mineral Resource block model, iso-surface contours of modelled magnetic intensities, and grade ranges in available diamond drill holes. The volumes were multiplied by a specific gravity of 2.72g/cc (the average density of the T1 resource) to determine the tonnage range of the target. Grade ranges were determined with reference to drill intersections and surface rock chip assays.

The next step in testing these targets is primarily diamond drill testing. The targets have been adequately defined, but drill programs still require further detailed planning regarding the number of drill holes, their azimuths, dips, and final depths. Drilling of these targets will be undertaken over the next two years, subject to the company's funding availability.

27

TABLE 1 – Section 1: Sampling Techniques and Data

Criteria JORC Code explanation Commentary
Sampling
techniques
Nature and quality of sampling (e.g. cut channels,
random chips, or specific specialised industry
standard measurement tools appropriate to the
minerals under investigation, such as downhole
gamma sondes, or handheld XRF instruments, etc.).
These examples should not be taken as limiting the
broad meaning of sampling.
The sampling database for Bramaderos project (the
Project) includes diamond drilling (DD) and trench
data.
Sampling in the Project area has been compiled
from information collected under ownership of the
companies listed below:

Sunstone Metals (2019 to 2025)

Ecuador Gold S.A. (2006 to 2007)

Ecuanor S.A. (1999 to 2000).
Only datasets collected by Sunstone Metals and
Ecuador Gold S.A. have been used in the
preparation of the Mineral Resource estimate
which is reported herein. Accordingly, only this
data is summarised in this table. The vast majority
of the data used in the Mineral Resource estimate
was collected by Sunstone from 2019 through
2025.
The Competent Person considers that the sampling
techniques adopted are appropriate for the style of
mineralisation.
Include reference to measures taken to ensure sample
representivity and the appropriate calibration of any
measurement tools or systems used.
For drillhole data, half core is generally submitted
for assay (from 2021 to 2025), however from 2019
through 2021, quarter core (rather than half core)
was submitted as the primary sample. Samples are
taken at 1–2 m intervals and honour different rock
types, alteration zones and mineralised zones as
defined by geologists. Core is cut along the
longitudinal axis using a core saw. A duplicate
sample was obtained by quartering the core
sample.
Trench sampling was carried out at 1–2 m intervals
using a portable cutting machine or a hammer and
chisel depending on rock hardness and honouring
different rock types. Samples honour different rock
types, alteration zones and mineralised zones as
defined by geologists. A duplicate sample was
obtained by quarteringtheprimarytrench sample.
Aspects of the determination of mineralisation that
are Material to the Public Report. In cases where
‘industry standard’ work has been done this would be
relatively simple (e.g. ‘reverse circulation drilling was
used to obtain 1 m samples from which 3 kg was
pulverised to produce a 30 g charge for fire assay’). In
other cases, more explanation may be required, such
as where there is coarse gold that has inherent
sampling
problems.
Unusual
commodities
or
mineralisation types (e.g. submarine nodules) may
warrant disclosure of detailed information.
Diamond drilling and trench sampling points have
been guided by geological logging and mapping.
Sunstone Metals
The core samples from Brama-Alba were dried,
crushed to 70% passing 2 mm, split (1 kg) and
pulverised to 85% passing 75 microns. A 20 g
portion of this sample was used for multi-element
analysis (IMS-230) and a 30 g sample for Fire Assay
Au (FAS-111).
Trench samples adopted the same sample
preparation and analytical techniques, with the
exception that after crushing, the sample is split to
a 250g portion usinga riffle or Boyd rotarysplitter

28

Criteria JORC Code explanation Commentary
while drill core is split to 1 kg,
Ecuador Gold
Limited details on the logging, sample preparation
and analytical methods used by Ecuador Gold are
available.
According to historical documentation, samples
were sent to the Inspectorate sample preparation
laboratory, from where pulps were subsequently
shipped to Peru for analysis. 30-gram fire assay
methods were used for gold analysis, and a multi-
element suite was analysed using the IMS-230
method.
Drilling
techniques
Drill type (eg core, reverse circulation, open-hole
hammer, rotary air blast, auger, Bangka, sonic, etc)
and details (e.g. core diameter, triple or standard
tube, depth of diamond tails, face-sampling bit or
other type, whether core is oriented and if so, by what
method, etc).
Sunstone Metals
All drilling is diamond core. Holes have been drilled
to various depths, up to 720 m. The diamond core
was drilled delivering either HTW (70.9mm) or
NTW (56mm) core. Drill core is oriented using a
Reflex ACT II tool for bottom of hole.
Ecuador Gold
Drilling by Ecuador Gold is also diamond core
drilling;however,the core sizes are not known.
Drill sample
recovery
Method of recording and assessing core and chip
sample recoveries and results assessed.
Sunstone Metals
Drilling recoveries are recorded for diamond core
samples as part of geotechnical logging. Diamond
core recovery was measured for each drill run and
captured in a digital logging software package. The
data has been reviewed and core recovery was
approximately 100% throughout.
Ecuador Gold
Core recoveries for the Ecuador Gold holes were
not recorded but are likelyto be veryhigh.
Measures taken to maximise sample recovery and
ensure representative nature of the samples.
Recovery of drill core is maximised by using drilling
techniques and drilling fluids suited to the ground
conditions. The core is sawn in half using a core
saw, following mark-up by geologists to ensure
representivity.
Whether a relationship exists between sample
recovery and grade and whether sample bias may
have occurred due to preferential loss/gain of
fine/coarse material.
No relationship between sample recovery and
grade has been established.
Logging Whether core and chip samples have been
geologically and geotechnically logged to a level of
detail to support appropriate Mineral Resource
estimation, mining studies and metallurgical studies.
Sunstone Metals
Drill hole logging is completed at the core shed by
trained geo-technicians and geologists on a tablet
or laptop directly into a Microsoft Excel based
spreadsheet which has been designed for the
project. Logging was carried out according to
Sunstone’s
internal
protocols
and
quality
assurance (QA) procedures which comply with
industry standards.
Logging is divided into two categories, namely
geological
and
geotechnical.
There
is
a
corresponding operational procedure for the
geological andgeotechnical logging. A template

29

Criteria JORC Code explanation Commentary
with codes has been set up to ensure consistent
collection of relevant geological information.
Mineralisation, mineralogy, alteration, lithology,
colour,
structure,
veining
and
weathering
information are collected into different tables
using standalone codes. Magnetic susceptibility
and XRF readings for some estimation elements are
recoded in separate tables.
The geologist completes mapping of the trenches
by recording lithology, alteration, mineralisation
and colour of each sample. The geologist also
checks the collected samples with a hand lens to
observe details of mineralisation or alteration that
cannot be observed while mapping the trench.
Sample numbers of the collected samples were
clearly marked along the trench surface using
aluminium plates for future reference.
Ecuador Gold
All drill core was logged using lithology codes
specific to the project. Detail surrounding data
entry/capture procedures in the field was not
available.
Whether logging is qualitative or quantitative in
nature. Core (or costean, channel, etc.) photography.
Logging is generally quantitative, but which
includes some aspects that are qualitative in
nature.
All core is stored at site and has been
photographed in wet and dryconditions.
The total length and percentage of the relevant
intersections logged.
The drill holes and trenches are logged in full
(100%), from start to finish of the hole or
excavation.
Sub-sampling
techniques and
sample
preparation
If core, whether cut or sawn and whether quarter, half
or all core taken.
Sunstone Metals
The routine sample procedure is to cut the core in
half using a core saw to the right of the orientation
line (looking down hole) or the cut line (in cases
where the orientation line was not reliable). Half
core (or quarter core from 2019 through 2021) was
used to provide the samples that were submitted
for assay from 2021 to 2025...
Ecuador Gold
The routine sample procedure for core cutting was
not recorded in the available reports.
If non-core, whether riffled, tube sampled, rotary split,
etc. and whether sampled wet or dry.
Trench and channel sampling was carried out by
Sunstone Metals from 2017 through 2025.
Trench and channel samples were collected using a
portable cutting machine hammer and chisel
dependingon the rock hardness.
For all sample types, the nature, quality and
appropriateness of the sample preparation technique.
Sunstone Metals
Drill core and trench samples from Brama-Alba
were sent to the LAC y Asociados Cia. Ltda. Sample
Preparation Facility in Cuenca, Ecuador for sample
preparation. The standard sample preparation for
drill core samples (Code PRP-910) is: Drying the
sample,crushingto size fraction 70% <2 mm and

30

Criteria JORC Code explanation Commentary
splitting the sample to a 250 g portion by riffle or
Boyd rotary splitter. The 250 g sample is then
pulverised to >85% passing 75 microns and then
split into two 50 g pulp samples. One of the pulp
samples was sent to the MS Analytical Laboratory
in Vancouver (Unit 1, 20120 102nd Avenue,
Langley, BC V1M 4B4, Canada) for gold and base
metal analysis.
Sample preparation is carried out according to
industry standard practices.
Ecuador Gold
Limited details on the sample preparation
technique are available, however it is known that
samples were sent to the Inspectorate sample
preparation laboratory from where pulps were
subsequentlyshipped to Peru for analysis.
Quality control procedures adopted for all sub-
sampling stages to maximise representivity of
samples.
Sunstone Metals
Sunstone use an industry standard QA programme.
Certified Reference Materials (CRMs), blanks and
field duplicates were introduced in the assay
batches. For core samples, each quality control
(QC) sample type was submitted at a rate of 1 in 28
samples. The results are reported along with the
sample assay values in the final analysis report.
For trench samples, CRMs, blanks and duplicates
are submitted. CRMs correspond to every 50th
sample, while blanks correspond to the 25th, and
duplicate samples correspond to every 33rd
sample.
Ecuador Gold
Ecuador Gold used an industry standard QA
programme. CRMs, blanks and field duplicates
were introduced in the assaybatches.
Measures taken to ensure that the sampling is
representative of the in-situ material collected,
including
for
instance
results
for
field
duplicate/second-half sampling.
Sunstone Metals
For diamond core, the routine sample procedure is
to always take the half/quarter core to the right of
the orientation line (looking down hole) or the cut
line (in cases where the orientation line was not
reliable). Field duplicates were taken every 28th
sample on average by quarter coring.
For trench samples duplicate samples were taken
~ 1 in every 33 samples by quartering the primary
sample.
Once assay results are received the results from
duplicate samples are compared with the
corresponding
routine
sample
to
ascertain
whether the sampling is representative.
Ecuador Gold
For diamond core, field duplicates were taken,
however only limited data on how the core
duplicates were collected.
Whether sample sizes are appropriate to the grain
size of the material being sampled.
Sample sizes are considered to be appropriate for
the style of sampling undertaken and the grainsize

31

Criteria JORC Code explanation Commentary
of the material, and correctly represent the style
and type of mineralisation at the exploration stage.
Quality of assay
data and
laboratory tests
The nature, quality and appropriateness of the
assaying and laboratory procedures used and
whether the technique is considered partial or total.
Sunstone Metals
MS Analytical is an internationally accredited
laboratory that has its internal procedures
scrutinised in order to maintain their accreditation.
MS Analytical is accredited to ISO/IEC 17025 2005
Accredited Methods.
Sunstone Metals uses a fire assay gold technique
for Au assays (FAS-111) and a four acid multi
element technique (IMS-230) for a suite of 48
elements. FAS-111 involves Au by Fire Assay on a
30-gram aliquot, fusion and atomic absorption
spectroscopy (AAS) at trace levels. IMS-20 is
considered a near total 4 acid technique using a
20g aliquot followed by multi-element analysis by
ICP-AES/MS at ultra-trace levels.
The analysis techniques are considered suitable for
this style of mineralisation.
Ecuador Gold
30-gram fire assay methods were used for gold
analysis, and a multi-element suite was analysed
by IMS-230.
The analysis techniques are considered suitable for
this style of mineralisation.
For geophysical tools, spectrometers, handheld XRF
instruments,
etc.,
the
parameters
used
in
determining the analysis including instrument make
and model, reading times, calibrations factors
applied and their derivation, etc.
Handheld XRF data, together with detailed
geological logging, were used by Sunstone Metals
as a guide to areas of potential mineralisation only.
No geophysical tools were used to directly support
thepreparation of this Mineral Resource estimate.
Nature of quality control procedures adopted (e.g.
standards, blanks, duplicates, external laboratory
checks) and whether acceptable levels of accuracy
(i.e. lack of bias) and precision have been established.
Sunstone Metals
CRMs, blanks and field duplicates are inserted in
the sample stream at a rate of ~1/28 samples. The
values of the CRM range from low to high grade
and are considered appropriate to monitor
performance of values near cut-off and near the
mean grade of the deposit. Pulps and coarse
rejects were also submitted to an umpire
laboratory to further check the accuracy of the
data. The QC results are monitored, and
performance issues are communicated to the
laboratory if necessary.
Following review of all the QC results that are
available, the Competent Person considers that
acceptable levels of precision and accuracy have
been established.
Ecuador Gold
CRMs, blanks and field duplicates were inserted in
the sample stream.
Following review of all the QC results that are
available, the Competent Person considers that
acceptable levels of precision and accuracy have
been established.

32

Criteria JORC Code explanation Commentary
Verification of
sampling and
assaying
The verification of significant intersections by either
independent or alternative company personnel.
Procedure checks and calculation of significant
intersections have been completed by the
Competent Person for exploration results for this
announcement.
The use of twinned holes. Twin holes have not been drilled and are not
considered necessary given a high level of
confidence exists in the dataset supporting this
Mineral Resource estimate.
Documentation
of
primary
data,
data
entry
procedures, data verification, data storage (physical
and electronic) protocols.
Sunstone Metals
Logging is completed by trained geo-technicians or
geologists on a tablet or laptop directly into a
Microsoft Excel based spreadsheet which has been
designed for the Project.
Logging is divided into two categories namely
geological
and
geotechnical.
There
is
a
corresponding operational procedure for the
geological and geotechnical logging.
Logging is carried out at a core shed. A template
with codes has been set up to ensure consistent
collection of relevant geological information
Mineralisation, alteration, lithology, structure,
veining information are collected into different
tables
using
standalone
codes.
Magnetic
susceptibility readings and XRF for quantitative
estimation elements are recoded in separate
tables.
Core is photographed in wet and dry conditions at
the core shed. Core photographs are stored on the
server for future reference.
All the data is backed up on a server.
Ecuador Gold
Data was provided to SGC in an Access database in
a clean format, however the data entry procedures
at the time the data was collected are not known.
Discuss any adjustment to assay data. No adjustments were made to the analytical data,
other than replacing below detection results with
a value equal to half the detection limit.
Location of data
points
Accuracy and quality of surveys used to locate drill
holes (collar and down-hole surveys), trenches, mine
workings and other locations used in Mineral
Resource estimation.
Sunstone Metals
All the recent drill hole collars and trench profiles
were located using a differential global position
system (DGPS) with an accuracy of +5 cm
horizontally and +10 cm vertically.
Downhole surveys for the Project were completed
by the drilling contractors using a Reflex Gyro
Sprint-IQ Gyroscope. The downhole surveys are
taken every 5 m down the hole and adjusted for
magnetic declination. The data is digitally
uploaded into the database from the instrument
output files. Validation consists of measuring
differences between the input and output
measurements. The measurement is within the
acceptable range when the maximum difference
does not exceed 1%. The drill casingis held in situ

33

Criteria JORC Code explanation Commentary
until the gyroscope data has been verified and
passes the maximum difference of 1% check. The
data is verified using the IMDEX HUB-IQ online
platform. When the information is accepted, it is
entered into the company's spreadsheet designed
to register individual borehole dip and azimuth
data. In the case of exceeding the acceptable
tolerance of up to 1%, the survey is repeated.
Ecuador Gold
Collar location methods are not known. A single
shot Pajari tool was used to take one dip and
azimuth
measurement
at
the
collar
only.
Accordingly, the hole paths for these holes are
subject to some uncertainty.
Specification of the grid system used. The grid system used is Geocentric Datum of
Ecuador PSAD56 Zone 17 South.
Quality and adequacy of topographic control. Sunstone provided a topographic digital terrain
model (DTM) generated from DGPS data using the
following equipment:

1x Sokkia 630RK Total Station with a precision of
6 seconds

3x Trimble R4 GNSS differential RTK with a
precision of ± 2cm RTK.

1x CHCNav i90 Pro
Total Station methods were used for closed places
and GPS RTK for open places. The scale of the survey
is 1:1000.
The software used for data processing was Trimble
Business Centre, Trimble Access, and Sokkia Link.
Civil CAD, QGIS, Global Mapper, and Excel were used
togenerate figures and compile the data.
Data spacing and
distribution
Data spacing for reporting of Exploration Results. Drill spacing varies over the deposit area due to the
steep terrain of the area. Typically, drilling is at
approximately 50 m - 100 m spacings (along strike)
and up to approximately 100 m down dip. However,
many of the holes have been fanned to achieve the
current drill spacing.
Whether the data spacing, and distribution is
sufficient to establish the degree of geological and
grade continuity appropriate for the Mineral Resource
and Ore Reserve estimation procedure(s) and
classifications applied.
The Competent Person believes the mineralised
domains have sufficient geological and grade
continuity to support the classifications applied to
the Mineral Resources given the drill pattern.
Whether sample compositing has been applied. Compositingwas not applied at the samplingstage.
Orientation of
data in relation
to geological
structure
Whether the orientation of sampling achieves
unbiased sampling of possible structures and the
extent to which this is known, considering the deposit
type.
The drilling has been undertaken at various
orientations, given the steep terrain and the
restriction in the location of the drilling platforms.
The nature of the terrain has resulted in some drill
holes being drilled oblique to the overall strike of
the mineralisation.
The mineralisation is intersected at various angles
to the overall strike of the mineralised zone.

34

Criteria JORC Code explanation Commentary
If the relationship between the drilling orientation and
the orientation of key mineralised structures is
considered to have introduced a sampling bias, this
should be assessed and reported if material.
The relationship between the drilling orientation
and the orientation of key mineralised structures is
not considered to have introduced a sampling bias.
Sample security The measures taken to ensure sample security. Sunstone Metals
Drill core trays were registered upon entering the
camp area which is monitored by cameras and
security agents.
Sunstone Metals sampling procedures indicate
individual samples were given due attention.
Sample security was managed through sealed
individual samples and sealed bags of multiple
samples for secure delivery to the laboratory by
permanent staff of the joint venture.
Ecuador Gold
Core boxes were stored briefly at the drill rig site
during each drill shift before transport (1-2 km) by
truck to the core shed at the main camp within the
concession. The core shed was kept locked and
under the guard of two employees. Samples were
packed in double-layer plastic bags, labelled, tied,
and then sent to Catacocha (30 minutes by road)
using Ecuador Gold’s trucks and a driver
accompanied by a company geologist. The samples
were subsequently dispatched by bus to Quito,
directly to the Inspectorate sample preparation
laboratory.
Audits or reviews The results of any audits or reviews of sampling
techniques and data.
Sunstone Metal’s sampling techniques and data
have been audited multiple times by independent
mining
consultants
during
various
project
assessments. These audits have concluded that the
sampling techniques and data management
systems are consistent with industry standards.
All historical data has been validated to the best
degree possible and migrated into a database.

TABLE 1 – Section 2: Exploration Results

Criteria JORC Code explanation Commentary
Mineral
tenement and
land tenure
status
Type, reference name/number, location and
ownership including agreements or material issues
with third parties such as joint ventures,
partnerships, overriding royalties, native title
interests, historical sites, wilderness or national park
and environmental settings.
The Bramaderos Exploration Concession (Concession
Code 60000334) and Bramaderos02 (Concession
Code 60000598) are located in the Loja Province of
southern Ecuador and covers a total of 4,948 hectares
and 38 hectares respectively.
The concession was granted to La Plata Minerales S.A.
(“PLAMIN”) on 27 December 2016 for a period of 25
years. PLAMIN is a subsidiary of Sunstone Metals Ltd.
The concession is subject to a Joint Venture between
Cornerstone Capital Resources Inc. (12.5%) and
Sunstone Metals Ltd. (87.5%). There are no declared
wilderness areas or national parks within or adjoining
the concession area. There are no established native

35

Criteria JORC Code explanation Commentary
title interests.
The security of the tenure held at the time of
reporting along with any known impediments to
obtaining a licence to operate in the area.
The Exploration Concessions are in good standing and
no known impediments exist.
Exploration done
by other parties
Acknowledgment and appraisal of exploration by
other parties.
Historic exploration at Bramaderos was completed by
various groups over the periods 1970-1984, 2001-
2002 and 2004-2007. Most of the readily available
historic data has been acquired and compiled into
databases and a GIS project.
Exploration by other parties has included stream
sediment surveys, geological mapping, rock chip
sampling (888 samples) and grid-based soil sampling
(1324 samples), trenching and channel sampling (17
trenches),
ground
magnetic
surveys
(31-line
kilometres), electrical IP surveys and diamond drilling
(10,426 m).
Geology Deposit type, geological setting and style of
mineralisation.
The deposit style being explored for includes
intrusion-related and stockwork hosted porphyry Au-
Cu systems plus epithermal gold-silver-polymetallic
veins. The setting at Brama-Alba is a volcanic arc
setting of Cretaceous age intrusions.
The lithology of the Brama and Alba deposits
comprise at least eight different intrusion phases
spanning
the
entire
mineralisation-alteration
sequence with the main ore-bearing phases consisting
of a large porphyry diorite intrusion and associated
crystalline intrusion breccias.
The principal rock types at Brama/Alba are assigned
here to four broad units; (1) the pre-mineralisation
sedimentary and dacitic to andesitic volcanic rocks;
(2) two early-mineralisation phases; (3) three syn-
mineralisation porphyry intrusion and associated
intrusion breccia phases spanning the alteration-
mineralisation sequence; and (4) late-mineralisation
intrusions, mill breccia dykes and post-mineralisation
andesite dykes.
Drill hole
Information
A summary of all information material to the
understanding of the exploration results including a
tabulation of the following information for all
Material drill holes:
a. easting and northing of the drill hole collar
b. elevation or RL (Reduced Level – elevation
above sea level in metres) of the drill hole
collar
c. dip and azimuth of the hole
d. down hole length and interception depth
e. hole length.
Exploration Results are not being reported.
Suppose the exclusion of this information is justified
on the basis that the information is not Material and
this
exclusion
does
not
detract
from
the
understanding of the report. In that case, the
Exploration Results are not being reported.

36

Criteria JORC Code explanation Commentary
Competent Person should clearly explain why this is
the case.
Data aggregation
methods
In
reporting
Exploration
Results,
weighting
averaging techniques, maximum and/or minimum
grade truncations (e.g. cutting of high grades) and
cut-off grades are usually Material and should be
stated.
Exploration Results are not being reported.
Where aggregate intercepts incorporate short
lengths of high-grade results and longer lengths of
low-grade results, the procedure used for such
aggregation should be stated and some typical
examples of such aggregations should be shown in
detail.
Exploration Results are not being reported.
The assumptions used for any reporting of metal
equivalent values should be clearly stated.
Metal equivalent values are reported in the Mineral
Resource table. Recovery assumptions are supported
by metallurgical test work. Key information is
provided below, with additional detail provided in the
full technical report supporting the Mineral Resource
estimate.
Metallurgical head assays further indicate no
interference from deleterious elements is expected,
with respect to concentrate quality. Deleterious
elements are present in low concentrations and these
elements are not anticipated to report to the
concentrate phase in concentrations that will incur
penalty charges.
Test work confirmed that the anticipated copper
recovery equates to 85%, whilst the flotation-tail
cyanidation route yielded an overall gold recovery of
88% when normalizing the results, for a target 20%
copper concentrate grade. Silver recoveries are
expected to be lower at around 60%. Work is ongoing.
Relationship
between
mineralisation
widths and
intercept lengths
If the geometry of the mineralisation with respect to
the drill-hole angle is known, its nature should be
reported.
Exploration Results are not being reported.
If it is not known and only the down hole lengths are
reported, there should be a clear statement to this
effect (e.g. ‘down hole length, true width not
_known’). _
Exploration Results are not being reported.
Diagrams Appropriate maps and sections (with scales) and
tabulations of intercepts should be included for any
significant discovery being reported. These should
include, but not be limited to a plan view of drill hole
collar locations and appropriate sectional views.
Relevant maps and diagrams are included in the body
of the announcement.
Balanced
reporting
Where comprehensive reporting of all Exploration
Results is not practicable, representative reporting
of both low and high grades and/or widths should
be practiced to avoid misleading reporting of
Exploration Results.
Exploration Results are not being reported.
Other substantive
exploration data
Other exploration data, if meaningful and material,
should be reported) including (but not limited to):
geological observations; geophysical survey results;
geochemical survey results; bulk samples – size and
No substantive exploration data not already
mentioned in this table has been used in the
preparation of this Mineral Resource estimate, and
the Exploration Target.

37

Criteria JORC Code explanation Commentary
method of treatment; metallurgical test results;
bulk density, groundwater, geotechnical and rock
characteristics;
potential
deleterious
or
contaminating substances.
Further work The nature and scale of planned further work (e.g.
tests for lateral extensions or depth extensions or
large-scale step-out drilling).
Sunstone Metals intends to complete additional
drilling at Brama-Alba and nearby prospects. The
Bramaderos drilling will aim to increase confidence in
the Mineral Resource estimate. Drilling at nearby
prospects aims to discover additional Mineral
Resources, which will add to the Mineral Resource
inventory
and
improve
project
economics.
Metallurgical test work is ongoing.
Diagrams clearly highlighting the areas of possible
extensions,
including
the
main
geological
interpretations and future drilling areas, provided
this information is not commercially sensitive.
Diagrams have been included in the body of this
report.

TABLE 1 – Section 3 Estimation and Reporting of Mineral Resources

Criteria JORC Code explanation Commentary
Database
integrity
Measures are taken to ensure that data has not
been corrupted by, for example, transcription or
keying errors, between its initial collection and use
for Mineral Resource estimation purposes.
The database is managed using Geobank software.
Data is logged directly into a Microsoft Excel sheet
logging system with drop down field lists. Validation
checks are written into the importing program
assured that all data is of high quality. Digital assay
data is obtained from the Laboratory, QA/QC
checked and imported. Results are exported to CSV
files and imported directly to the Micromine
software used for the MRE.
Data validation procedures used. The combined database was provided for the MRE.
Validation of the data import includes checks for the
following: o Duplicate drill hole or trench names, e.g:
• One or more drill hole collar or trench
coordinates missing in the collar file,
• FROM or TO missing or absent in the assay file,
• FROM > TO in the assay file,
• Sample intervals overlap in the assay file,
• The first sample is not equal to 0 m in the assay
file,
• The first depth is not equal to 0 m in the survey
file,
• Several downhole survey records exist for the
same depth,
• Azimuth is not between 0 and 360° in the
survey file,
• Dip is not between 0 and 90° in the survey file,
• Azimuth or dip is missing in the survey file,
• Total depth of the holes is less than the depth

38

Criteria JORC Code explanation Commentary
of the last sample,
• Total length of trenches is less than the total
length of all samples.
• Negative sample grades.
• No logical errors were identified in the
analytical data.
Site visits Comment on any site visits undertaken by the
Competent Person and the outcome of those visits.
If no site visits have been undertaken, indicate why
this is the case.
Rob Spiers from Spiers Geological Consultants (SGC)
visited the site from 28 October through 31 October
2025 as the Competent Person. The site visit aimed
to review activities relevant to local geology,
operational procedures, drilling, logging, sampling,
QA/QC, documentation of primary data, data entry
procedures, and data storage.
The overall finding was that the site team have a
good knowledge of the deposit geology, data
collection procedures are consistent with industry
good practice..
Geological
interpretation
Confidence in (or conversely, the uncertainty of) the
geological interpretation of the mineral deposit.
A high level of confidence exists in the mineralisation
interpretation.
Nature of the data used and of any assumptions
made.
The weathering model was generated by Sunstone
Metals using logged weathering and snapping the
strings to the drillholes and the topography using
Leapfrog Geo. Three surfaces representing the
strongly weathered, moderately weathered and
fresh zones were identified from the logging. Peer
review of the interpretations was completed by SGC.
A 3D model of the lithology, early alteration phases
and veining were created to assist in determining the
best sub-domaining approach during the resource
estimate process. Strings were digitised around the
lithology and alteration units and then linked to form
a 3D solid model.
The effect, if any, of alternative interpretations on
Mineral Resource estimation.
Alternative interpretations are likely to moderately
impact the domain modelling, tightening the
periphery of domain interpretations as drilling
density increases, however it is considered that the
impacts on the Mineral Resource estimate on a local
basis will be minimal, with little to no impact on
global estimates other than to potentially expand
resources inventory.
The use of geology in guiding and controlling
Mineral Resource estimation.
Geological logging of drill holes and limited mapping
have been used to guide Mineral Resource
estimation. The controls on the mineralisation are
both
lithological
and
structural,
and
this
understanding has governed the resource estimation
approach.
The factors affecting continuity both of grade and
geology.
Continuity of mineralisation is very good and is
significantly controlled by the presence of a diorite
unit. The centralpart of the diorite intrusion is

39

Criteria JORC Code explanation Commentary
mineralised while the outer margins are not. The
tenor of mineralisation is variable within the central
diorite and linked primarily to vein intensity..
Dimensions The extent and variability of the Mineral Resource
expressed as length (along strike or otherwise),
plan width, and depth below surface to the upper
and lower limits of the Mineral Resource.
The Mineral Resource at Brama-Alba is contained
within an area defined by a strike length of around
1,600 m in the northwest-southeast direction, locally
up to 550m in the northeast-southwest direction,
and depth extent up to around 500 m. The plan width
is in the order of 300 m metres on average. The
Melonal mineralisation as estimated in the MRE is
continuous for approximately up to 400m by 300m
and with an average depth extent locally up to about
400 m. Mineral Resources are reported within a pit
shell which was generated by STM to demonstrate
reasonable
prospects
for
eventual
economic
extraction.
Estimation and
modelling
techniques
The nature and appropriateness of the estimation
technique(s)
applied
and
key
assumptions,
including treatment of extreme grade values,
domaining,
interpolation
parameters
and
maximum distance of extrapolation from data
points. If a computer assisted estimation method
was chosen include a description of computer
software and parameters used.
Ordinary Kriging technique was employed using third
party software based on low coefficient of variation
between samples in the mineralised domain.
Grade interpolation and search ellipses were based
on variography and geometry modelling outcomes.
Modelling was conducted in three passes with block
sizes being 20.0 m E by 20.0 m N by 30.0 m RL;
discretisation was 5x5x2 for all project areas
In the first pass data and octant criteria used were,
Minimum Data=12, maximum Data=32, Minimum
Octants=4. Search radii was 30 mE by 80 mN by 20
mRL with rotations of Z=-50, Y=0 and X=88 according
to the right-hand rule.
An expansion factor of 1 was applied so in the second
pass saw the same data and octants criteria with an
expanded search to 60mE by 160mN by 40mRL.
The third pass saw Minimum Data=6, maximum
Data=32, Minimum Octants=2. Search radii was
60mE
by
160mN
by
40mRL.
Top cutting was applied to domains and elements
which displayed a very strongly skewed nature as
summarise in the report reference and in accordance
with the prevailing coefficients of variation.
Secondary attributes including the modelling of
density which was also modelled on three passes (as
above) which included the same data and octant
criteria as above.
No dilution was expressly added to the SGC model.
However, domaining was largely driven by geological
and grade domains created by STM and provided to
SGC which tends to incorporate the full population
range in the geological domains and a constrained
population range in the grade domains in-line with
the grade domain constraints.
No assumptions were made bySGC regardingthe

40

Criteria JORC Code explanation Commentary
recovery of by-products.
Gold, silver and copper were modelled as elements.
The interpretation or domain model was largely
driven by the lithology / geology, oxidation state, and
structural intervention and mineralised trends
observed over the various project areas. Grade was
used as a secondary domain driver for the definition
of boundaries conditions where deemed appropriate
by the STM resource team.
The model was validated in a third-party software
using section and plan comparisons back to original
informing data as well as with the use of swath plots
to assess local grade variability between the model
and informing data.
The availability of check estimates, previous
estimates and/or mine production records and
whether the Mineral Resource estimate takes
appropriate account of such data.
CSA Global produced a previous mineral resource
estimate in December 2022 which totalled 156Mt @
0.35g/t Au, 0.11% Cu, 1.3 g/t Ag, 0.53g/t AuEq, for a
total of 2.7Moz AuEq.The Indicated was: 9Mt @
0.38g/tAu, 0.09% Cu, 1.1g/t Ag, 0.53g/t AuEq, for a
total of 0.2 Moz AuEqandthe inferred was: 147Mt @
0.35g/t Au, 0.11% Cu, 1.3g/t Ag, 0.53g/t AuEq, for a
total of 2.5Moz AuEq.
The2024 MRE appropriately accounts forthe
previous estimate and is considered reasonable,
given the additional drill holes and surface trenches
undertaken in the ensuing two years.
The assumptions made regarding recovery of by-
products.
Sunstone Metals Ltd has portrayed to SGC that
metallurgical studies have indicated no issues are
likely with deleterious elements
Both copper and gold are assumed to be recovered
by flotation, with gold undergoing additional cyanide
leach treatment.
Estimation of deleterious elements or other non-
grade variables of economic significance (eg.
sulphur for acid mine drainage characterisation).
Metallurgical studies have indicated no issues are
likely with deleterious elements. Inverse distance
squared was used to interpolate S, Pb, Zn and As
grades into the block model to support future mining
studies.
In the case of block model interpolation, the block
size in relation to the average sample spacing and
the search employed.
As noted in the earlier section “Estimation and
Modelling techniques” search and data criteria were
employed inline with statistical analysis and
geometry modelling which also guided the selection
of the prevailing block size used in estimation which
at this time is 25mE by 25mN by 10mRL and is
considered consistent with half the prevailing data
spacing, is consistent with variogram first and second
structure ranges in key domain areas and potential
future mining considerations.
Any assumptions behind modelling of selective
mining units.
No assumptions have been made regarding selective
mining units.

41

Criteria JORC Code explanation Commentary
Any assumptions about correlation between
variables.
No
assumptions
were
made
regarding
the correlation between variables.
Description of how geological interpretation was
used to control the resource estimates.
The domain approach was driven primarily by the
lithology, alteration and vein density models put
forth by STM from which boundary conditions were
analysed. Lithological domain solids for Di_SM,
Di_SMb, IBXA and IBXB were initially employed using
a hard boundary approach, after which all other
lithological domain solids were employed with a soft
boundary approach to include all data available in
the search neighbourhood. Alteration and vein
density domain solids were employed in the
assessment of boundary conditions for fine tuning of
potential sub-domain definition but were not
directly employed as domain constraints.
Discussion of basis for using or not using grade
cutting or capping.
Top cuts were selected following statistical analysis,
primarily
reviewing
log-probability
plots
and
histograms. The point on the histogram at which the
number of samples supporting the high-grade tail
diminishes was the primary method.
The process of validation, the checking process
used, the comparison of model data to drill hole
data, and use of reconciliation data if available.
Drillhole grades were initially visually compared with
block model grades. Domain drillhole and block
model statistics were compared. Swath plots were
then created to compare drillhole grades with block
model grades for easting, northing and elevation
slices throughout the deposit. The block model
reflected the tenor of the grades in the drillhole
samples both globally and locally.
Moisture Whether the tonnages are estimated on a dry basis
or with natural moisture, and the method of
determination of the moisture content.
Tonnages are estimated on a dry basis. No moisture
data is available.
Cut-off
parameters
The basis of the adopted cut-off grade(s) or quality
parameters applied.
The Mineral Resource reported above a cut-off grade
of 0.3 g/t AuEq within a pit shell. The cut-off grade
and pit shell were selected following a pit
optimisation study.
Mining factors or
assumptions
Assumptions made regarding possible mining
methods, minimum mining dimensions and internal
(or, if applicable, external) mining dilution.
It was assumed that open pit mining methods will be
employed.
This
is
reasonable
given
the
mineralisation is close to surface.
Metallurgical
factors or
assumptions
The basis for assumptions or predictions regarding
metallurgical amenability. It is always necessary as
part of the process of determining reasonable
prospects for eventual economic extraction to
consider potential metallurgical methods, but the
assumptions regarding metallurgical treatment
processes and parameters made when reporting
Mineral Resources may not always be rigorous.
Where this is the case, this should be reported with
an explanation of the basis of the metallurgical
assumptions made.
Metallurgical recoveries been estimated following
metallurgical test work. A number of metallurgical
studies have been undertaken, which are detailed in
the body of the detailed technical report which
supports this Mineral Resource estimate. Results
indicate excellent recoveries can be achieved via
flotation for gold and copper (88% and 85%
respectively). Silver recoveries are expected to be
lower at around 60%. Work is ongoing.
The metallurgical head assays further indicated that
no interference from deleterious elements is

42

Criteria JORC Code explanation Commentary
expected, with respect to concentrate quality.
Elements
of
interest
are
present
in
low
concentrations and these elements are not
anticipated to report to the concentrate phase in
concentrations that will incur penalty charges.
Environmental
factors or
assumptions
Assumptions made regarding possible waste and
process residue disposal options.
Environmental considerations have not been
considered in detail at the current stage of project
development. It is therefore assumed that waste
could be disposed in accordance with a site-specific
mine and rehabilitation plan.
Bulk density Whether assumed or determined. If assumed, the
basis for the assumptions. If determined, the
method used, whether wet or dry, the frequency of
the
measurements,
the
nature,
size
and
representativeness of the samples.
Bulk density determinations dominantly adopted the
water displacement method. A total of 3,756
measurements were available within the immediate
area for resource estimation taken from drill core. An
additional 289 measurememts were available from
surface channel samples within the resource
estimation area.
The bulk density for bulk material must have been
measured by methods that adequately account for
void spaces (vugs, porosity, etc), moisture and
differences between rock and alteration zones
within the deposit.
No wax was applied to the sample segments selected
from competent rock with no visible fractures while
porous and weathered samples were coated with
wax. 1 full diamond core segments were coated with
wax while 3,615 samples were not waxed. Very
limited voids exist hence the data is considered
accurate.
Discuss assumptions for bulk density estimates
used in the evaluation process of the different
materials.
Density values were interpolated into the fresh
domain of the mineralised block model cells using
ordinary kriging. Inverse distance was used to
estimate density into the strongly weathered and
moderately weathered domains of the mineralised
zone. Composited density values were used for the
interpolation.
Estimation
was
confined
to
weathering domain boundaries. Variogram models
and parameters determined from the QKNA were
used to guide density interpolation process.
Density estimation in the waste domain was
completed in a similar way to the density
interpolation in mineralised domain.
Classification The basis for the classification of the Mineral
Resources into varying confidence categories.
The Mineral Resource has been classified following
due consideration of all criteria contained in Section
1, Section 2 and Section 3 of JORC Code 2012 Table
1. The Mineral Resource has been classified as either
Indicated or Inferred based on data quality, sample
spacing, mineralisation continuity, confidence in the
geological interpretations, quality of the grade
estimations and metallurgical processing knowledge.
No Measured material has been classified.
The classification criteria are deemed appropriate by
SGC.
Whether appropriate account has been taken of all Appropriate account has been taken of all relevant

43

Criteria JORC Code explanation Commentary
relevant factors (i.e., relative confidence in
tonnage/grade estimations, reliability of input data,
confidence in continuity of geology and metal
values, quality, quantity and distribution of the
data).
criteria including data quality, sample spacing,
mineralisation
continuity,
confidence
in
the
geological interpretations, quality of the grade
estimations and metallurgical processing knowledge.
Whether the result appropriately reflects the
Competent Person’s view of the deposit.
The Mineral Resource appropriately reflects the
Competent Person’s views of the deposit
Audits or reviews The results of any audits or reviews of Mineral
Resource estimates.
The current model has not been audited by an
independent third-party.
Discussion of
relative
accuracy/
confidence
Where appropriate a statement of the relative
accuracy and confidence level in the Mineral
Resource estimate using an approach or procedure
deemed appropriate by the Competent Person. For
example,
the
application
of
statistical
or
geostatistical procedures to quantify the relative
accuracy of the resource within stated confidence
limits, or, if such an approach is not deemed
appropriate, a qualitative discussion of the factors
that could affect the relative accuracy and
confidence of the estimate.
The Mineral Resource accuracy is communicated
through the classification assigned to this Mineral
Resource. The Resource has been classified in
accordance with the JORC Code (2012 Edition) using
a qualitative approach.
All factors that have been considered have been
adequately communicated in Section 1 and Section 3
of this table.
Mineral resource estimate technique was deemed
appropriate by an internal peer review by SGC as
were the estimates themselves.
The statement should specify whether it relates to
global or local estimates, and, if local, state the
relevant tonnages, which should be relevant to
technical and economic evaluation. Documentation
should include assumptions made and the
procedures used.
The Mineral Resource statement relates to a global
tonnage and grade estimate. Grade estimates have
been made for each block in the block model.
All factors that have been considered have been
adequately communicated in Section 1 and Section 3
of this table.
These statements of relative accuracy and
confidence of the estimate should be compared
with production data, where available.
No previous mining has taken place at the project,
and production data is not available to reconcile
against the block model estimates.

44