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SUNSTONE METALS LTD Capital/Financing Update 2025

Oct 13, 2025

65870_rns_2025-10-13_d2b2049c-3ad1-46a9-ba9f-4aad40dd72e2.pdf

Capital/Financing Update

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~~ASX ANNOUNCEMENT~~

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14 OCTOBER 2025

- Bramaderos Gold Copper Project, Southern Ecuador

Sunstone targeting an updated Mineral Resource following successful completion of surface sampling program

Program is aimed at enhancing the already-substantial 2.7Moz AuEq[1,2] resource ahead of a scoping study

Key Points

Planned Brama-Alba Mineral Resource upgrade and scoping study

  • A major 1,543m surface sampling program has been successfully completed at Brama-Alba

  • This is the first stage of a program to upgrade geology interpretations and expand the existing 2.7Moz AuEq[1,2] Mineral Resource estimate ahead of a planned Bramaderos scoping study

  • The program targeted gold soil anomalies to expand the existing known mineralised area within the Brama-Alba porphyry resource and within the planned open pit area, as well as linking Alba to the adjacent Melonal gold copper porphyry

  • Assays for the 773-sample program are expected this month

Copete Gold and Copper Porphyry

  • All remaining assays from the Copete gold-copper surface definition ravine sampling program have been received with interpretations suggesting that the Copete gold-copper porphyry mineralisation may be contiguous with the adjacent Porotillo gold-copper porphyry mineralisation.

Sunstone Metals Ltd (ASX: STM) is pleased to provide an update on its latest exploration activity at its Bramaderos Gold-Copper Project in southern Ecuador.

Sunstone Managing Director Patrick Duffy said: “Our technical team continues to do exceptional exploration work while Sunstone progresses its strategic corporate and asset discussions.

Sunstone Metals Limited L31, 120 Collins St +61 3 7044 2627 ABN 68 123 184 412 Melbourne V 3000 [email protected] ASX: STM Australia sunstonemetals.com.au

REGISTERED OFFICE

The completion of a campaign-scale surface sampling and mapping program around the Brama and Alba gold and copper porphyry system is part of our strategy to upgrade the porphyry Mineral Resource and to prepare for a Scoping Study for the Bramaderos project.

“With multiple avenues for rapid resource growth and strengthening gold prices, we have very high confidence in the compelling economics of our resource at the Bramaderos Project which the proposed low-cost scoping study will deliver and also reevaluating the resource and conceptual open pit using recent gold prices.

“At Copete, additional channel sampling assays and compilation of data by our geology team are opening up the possibility that the Copete and Porotillo porphyry systems are contiguous. This is an exciting development that will focus our ongoing assessment of these adjacent porphyry systems”.

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Figure 1: The cluster of four porphyry gold-copper systems in the central area of the Bramaderos concessions (BramaAlba, Melonal, Copete and Porotillo), showing the two areas of completed surface sampling and geological mapping activity at Copete (blue outline) and around the periphery of Brama-Alba (blue channel sampling lines).

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1. Brama-Alba Surface Channel Sampling Campaign

A Mineral Resource estimate was undertaken at the Brama - Alba porphyry system in 2022 (see ASX announcement dated 13 December 2022), along with a modelled economic open-pit outline and definition of porphyry exploration targets within and under the modelled open-pit. This work clearly identified potential for the Brama-Alba resource to grow on several sides and at depth below the modelled pit.

Gold and copper prices have significantly increased (over 100%) since the initial resource estimate in late 2022. Consequently, the company sees value in rapidly progressing studies on the Brama-Alba porphyry system, in parallel with its exploration initiatives at the outcropping, higher-grade Limon epithermal gold-silver system, as well as the other Bramaderos porphyry targets.

This has the potential to result in a larger Mineral Resource estimate at Brama Alba, which will underpin a Scoping Study for the eventual multi-decade, large-tonnage, low-cost gold-copper mining operations at Bramaderos.

As part of this strategy, a significant campaign of surface channel sampling was completed during September at Brama-Alba and on the northeast side of Melonal. This work involved sampling a series of vehicle access roads, drill rig access tracks and ravines over gold soil anomalies that lie within and adjacent to the 2022 modelled open-pit shell (see Figures 2 and 3). The aims of this work are to:

  • identify additional zones of mineralisation that lie outside the current resource;

  • identify if mineralisation is contiguous between Alba and Melonal;

  • refine the surface geology map and the deposit sub-surface 3D lithology model;

  • acquire additional samples from surface on the northeast side of Melonal so that a future Mineral Resource update can bring part of the area into the resource; and,

  • provide further constraints for detailed vein and alteration modelling of the Brama - Alba deposit.

Areas of stockwork veining were encountered along sampling line 5 north of Brama, along sampling lines 6 and 7 between Melonal and Alba, and along parts of sampling line 8 on the south side of Brama (see Figures 2 and 3). All assays for sampling lines 1-13 are due in October 2025.

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Figure 2: Southward-looking view over Alba and Brama showing 4 of 13 surface rock-sampling lines surrounding the edges of the current resource.

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Figure 3: Location of 13 lines of surface rock channel sampling (blue lines) located over soil gold anomalies around the edges of the Brama-Alba resource and within or close to the margins of the planned pit shell as modelled in 2022 (red outline.

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Figure 4: Areas of new channel sampling and mapping along access tracks and ravines off the southern and western edges of the Brama-Alba gold and copper orebody.

5

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Figure 5: Porphyry stockwork veining sampled from along sections of sampling lines 6 and 7 located along and off the northeast edge of the Melona! porphyry system (see Figure 3). The rocks pictured above contain oxidised sheeted and stockwork veins at up to 15 veins per metre dominated by quartz and iron-oxide minerals such as goethite, limonite and hematite. The abundances of these iron-oxide minerals are around several percent, but do not necessarily translate to mineralisation. The maximum veins per metre estimates are based on field observations of the number of veins per metre of rock exposed in channel cuts. The photographs are not of specific mineralisation, and there are no visual-based estimates of grade due to the highly oxidised nature of these surface samples. Assay results for the sampling program discussed in this announcement are due and expected to be reported in late October 2025.

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2. Discussion of Results - Copete

Final assays were received from the completed program of ravine rock channel sampling at Copete that covered an area of 400m by 350m (see Figures 6 and 7).

An earlier trench at Copete (Trench ML01) yielded 214m @ 0.5 g/t Au-Eq and included 113m @ 0.64 g/t AuEq (see ASX announcement dated 12 November 2024).

The ravine mapping and sampling at Copete identified two mineralised intrusions that cover an area of 300m by >250m and are strongly stockwork veined. Assays from the first set of ravines (ravines 2 - 6) were announced in an ASX release dated 4 September 2025. Assays from the second set of ravines, QC-1, QC-3Ext, QC-7, QC-11, QC-12 and QC-13, have been received, and significant intersections are listed in Table 1.

This work has identified a core zone of higher gold grade in QC-2 and QC-3ext associated with two syn-mineral intrusions, and show that the high-grade mineralisation in Trench ML01 extends downslope to the north and south. This core zone at Copete appears to extend southward towards the Porotillo system.

The mineralised quartz diorite porphyry intrusion at Copete is open to the south and extends under cover below the valley floor that lies between Copete and Porotillo.

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Figure 6: Compilation map showing all sampled ravines at Copete (QC-1 to QC-7 and QC-11 to QC-13) in relation to Trench ML01, which yielded 214m @ 0.50 g/t Au-Equivalent (see ASX announcement dated 12 November 2024). Five exploration holes have been planned as a first-pass drill test of the Copete porphyry system (indicated by red hole traces).

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Table 1: Rock channel assay results from the recently completed program at Copete. New assays from ravines QC-1,

QC-3ext, QC-7, QC-11, QC-12 and QC-13.

There is increasing evidence that the strongest parts of the exposed Copete and Porotillo porphyry systems may be cojoined. They may be part of a 700m-long coherent and tabular mineralised zone that passes under the valley floor that separates Copete from Porotillo (Figure 6). Highly mineralised soil samples along this northeasterly porphyry trend strengthen this interpretation (Figure 7).

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Figure 7: Overview of the developing geometry and linkage of the Copete and Porotillo porphyry systems. Strong cores of mineralisation at surface at both Copete and Porotillo may be part of a large system whose surface expression is a 700mlong tabular zone that passes under the intervening valley floor.

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Geological work is ongoing to further test this hypothesis. If correct, this area could provide a third avenue for substantial porphyry resource growth on the Bramaderos property beyond the current 2.7 Moz Au-Eq[1,2] resource at Brama-Alba:

  1. Phase 1 expansion: Grow the Brama-Alba resource laterally and at depth;

  2. incorporate the Melonal Exploration Target into the Bramaderos Mineral Resource; and

  3. incorporate Copete-Porotillo into an Exploration Target and, with further drilling, a maiden Mineral Resource.

3. Ongoing Work

Ongoing geological work is currently focused on updating geological models at the Brama-Alba system to support a planned updated Mineral Resource estimate and commencing the Bramaderos Scoping Study.

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, has both at-surface and deeper porphyry goldcopper systems and contains an initial Mineral Resource estimate of 156Mt at 0.53g/t AuEq for 2.7Moz AuEq[1,2] .
JORC
Classification
Tonnage (Mt) Au (g/t) Cu (%) Ag (g/t) AuEq2 (g/t) AuEq2 (Mozs)
Indicated 9 0.38 0.09 1.1 0.53 0.2
Inferred 147 0.35 0.11 1.3 0.53 2.5
Total 156 0.35 0.11 1.3 0.53 2.7

Additionally, the Bramaderos Project has a porphyry Exploration Target of between 3.3Moz and 8.6Moz AuEq within 255Mt to 360Mt at a grade between 0.40 and 0.74g/t AuEq[1,2] , and the Limon epithermal gold-silver Exploration Target of 0.9 - 1.7Moz AuEq[4] within 30Mt - 44Mt at a grade between 0.9 - 1.2g/t AuEq[3,4] .

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.

  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

1 Refer ASX Announcement on 13 December 2022.

2 The gold equivalent 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 used were US$1,800/oz gold and US$9,500/t copper and US$22/oz silver. Recoveries are estimated at 89% for gold, 85% for copper, and 60% for silver based on metallurgical studies. Grades for the Exploration Target are 0.24g/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

3 Refer ASX Announcement on 5 February 2024.

4 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

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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[5,6] for 1.2Moz AuEq[6] .

JORC Classification Tonnage
Mt
Average Grade Average Grade Average Grade Average Grade Average Grade Material Content Material Content Material Content Material Content
AuEq6
(g/t)
Au
(g/t)
Ag
(g/t)
Cu
(ppm)
Cu
(%)
AuEq6
(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

Additionally, the El Palmar Project has a porphyry Exploration Target[7] of between 15Moz and 45Moz AuEq within 1.0 to 1.2Bt at a grade between 0.3 - 0.7g/t gold and 0.1 – 0.3% copper[5] .

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 to the host communities seriously and have endeavoured to implement the highest ESG standards throughout our business. Sunstone released its inaugural Sustainability Report in 2023, which details the level of support and engagement with local communities and project stakeholders.

5 Refer ASX Announcement on 22 October 2024.

6 The gold equivalent 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

7 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.

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Figure 8: The Bramaderos concession showing the location of Limon and other gold-copper porphyry (black outlines) and gold-silver epithermal targets (yellow outlines). The background image is gold-in-soil, highlighting the potential scale increase to be delivered with more drilling at Bramaderos across multiple targets. Drilling activity during 2024 focused on the Limon gold-silver epithermal opportunity.

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

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

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

Mr Patrick Duffy Media: Managing Director Paul Armstrong Sunstone Metals Ltd Read Corporate Tel: 03 7044 2627 +61 8 9388 1474 Email: [email protected]

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Competent Persons Statement

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.

The information relating to the Bramaderos Mineral Resource is extracted from the ASX announcement on 13 December 2022. 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.

Information on Exploration Targets

Bramaderos

The Bramaderos porphyry Exploration Target within the Bramaderos concession is estimated from 3 areas – the extensions to the Brama-Alba system that are not captured in the Mineral Resource estimate (MRE), and mineralisation drilled at the targets of Melonal and Limon porphyry mineralisation.

The Exploration Target does not include known porphyry mineralisation at Sandia, Porotillo, Playas, Copete or Yeso. It was decided to not include these areas because Sunstone has not yet completed any or sufficient drilling in these areas. Some historical drilling has been completed at Porotillo. 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 all material within a ‘Mineralisation Wireframe’, and within an economically modelled pit. Some drill holes that intersected mineralisation are outside the mineralisation wireframe, and either within or outside the pit. Inadequate drilling exists in these areas to show continuity. Furthermore, the effect of the reasonable prospects of economic extraction was to exclude 14% 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.

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.

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.

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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.

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.

Drilling at Limon has also intersected a high sulphidation system in holes LMDD004 and 006, which included intersections of 13.3m at 0.43% copper and 0.11g/t gold, within 59.6m at 0.16% copper.

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 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 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 two years, 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 to not 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 the areas 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 intersection 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 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.

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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 results announced here are from rock chip and
channel samples collected during geological mapping
programs.
Include reference to measures taken to ensure sample
representivity and the appropriate calibration of any
measurement tools or systems used.
• Rock chip samples and channel samples were
representative of the outcrop and alteration domains.
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.
• Rock chip and channel sampling points have been
guided by geological mapping. The samples were dried,
crushed to 70% passing 2mm, Split 1000g and
pulverised to 85% passing 75microns. A 20g portion of
this sample was used for multi-element analysis (IMS-
230) and a 30g sample for Fire Assay Au (FAS-111).
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). _
• Previous drilling by Sunstone is diamond core drilling
and has drilled to various depths. 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.
Drill sample
recovery
Method of recording and assessing core and chip sample
recoveries and results assessed.
• This announcement does not report drilling results.
Measures taken to maximise sample recovery and ensure
representative nature of the samples.
• This announcement does not report drilling results.
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.
• This announcement does not report drilling results.
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.
• Rock chip and channel samples were logged for
lithology,
weathering,
structure,
mineralogy,
mineralisation, colour, and other features. Sampling
was carried out according to Sunstone’s internal
protocols and QAQC procedures which comply with
industry standards.
Whether logging is qualitative or quantitative in nature.
Core (or costean, channel, etc.) photography.
• Rock chip and channel samples are logged for
lithology,
weathering,
structure,
mineralogy,
mineralisation, colour, and other features.
The total length and percentage of the relevant
intersections logged.
• The areas of outcrop are logged in full, and each
sampled outcropis individuallydescribed.
Sub-sampling
techniques
and sample
preparation
If core, whether cut or sawn and whether quarter, half or
all core taken.
• N/A – no drilling.
If non-core, whether riffled, tube sampled, rotary split,
_etc. and whether sampled wet or dry. _
• N/A.
For all sample types, the nature, quality and
appropriateness of the sample preparation technique.
• Surface samples 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, crushing to size fraction 70%
<2mm and splitting the sample to a 250g portion by
riffle or Boyd rotary splitter. The 250g sample is then
pulverised to >85% passing 75 microns and then split
into two 50g pulp samples. Then one of the pulp
samples was sent to the MS Analytical Laboratory in
Vancouver(Unit1,20120102ndAvenue,Langley,BC

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Criteria JORC Code explanation Commentary
V1M 4B4, Canada) for gold and base metal analysis.
• The sample preparation is carried out according to
industry standard practices using highly appropriate
sample preparationtechniques.
Quality control procedures adopted for all sub-sampling
stages to maximise representivity of samples.
• Sunstone
used
an
industry
standard
QAQC
programme involving Certified Reference Materials
“standards” and blank samples, which were introduced
in the assay batches.
• Standards (Certified Reference Materials) or analytical
blanks were submitted at a rate of approximately 1 in
28 samples. Field duplicates were also taken at a rate
of approximately 1 in 30 samples.
• The check or duplicate assay results are reported along
with the sample assay values in the final analysis
report.
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.
• Once assay results are received the results from
duplicate
samples
are
compared
with
the
corresponding routine sample to ascertain whether the
sampling is representative.
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 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 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.
• This analysis technique is 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
mapping, are used as a guide to areas of potential
mineralisation and samples from these areas are sent
for laboratory analysis as described above.
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.
• Standards, blanks and duplicates are inserted ~1/28
samples. The values of the standards 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.
• The check sampling results are monitored, and
performance issues are communicated to the
laboratoryif necessary.
Verification of
sampling and
assaying
The verification of significant intersections by either
independent or alternative company personnel.
• Procedure checks have been completed by the
Competent Person for exploration results for this
announcement.
The use of twinned holes. • Twin holes have not been drilled in these areas.
Documentation of primary data, data entry procedures,
data verification, data storage (physical and electronic)
protocols.
• Sunstone sampling data were imported and validated
using Excel.
Discuss any adjustment to assay data. • Assay data were not adjusted.
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.
• Sample co-ordinates are located by GPS.
Specification of the grid system used.
Ecuadorprojectionparameters:
Parameter
Value
Reference Ellipsoid
International 1924
Semi Major Axis

16

Criteria JORC Code explanation Commentary
Inverse Flattening (1/f)
Type of Projection
Central Meridian:
Latitude of Origin
Scale on Central Meridian
False Northing
False Easting
UTM Zone -17S (Datum
PSAD56)
-81.0000
0.0000
0.9996
10000000
500000
Quality and adequacy of topographic control. • The topographic control was compared against
published maps and satellite imagery and found to be
goodquality.
Data spacing
and
distribution
Data spacing for reporting of Exploration Results. • The samples were collected from various outcropping
areas during mapping. For the channel sampling most
samples were collected at around 2m intervals.
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 data from these samples does not contribute to any
resource estimate nor implies any grade continuity.
Whether sample compositing has been applied. • No sample compositing was done.
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.
• Rock chip locations were appropriate for the
interpreted geology providing representative samples.
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.
• No sampling bias is expected at this stage.
Sample
security
The measures taken to ensure sample security. • Sunstone 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.
• MS Analytical is an internationally accredited
laboratory that has all its internal procedures heavily
scrutinised in order to maintain their accreditation. MS
Analytical is accredited to ISO/IEC 17025 2005
Accredited Methods.
Audits or
reviews
The results of any audits or reviews of sampling
techniques and data.
• Sunstone’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 are to industry standards.
• All historical data has been validated to the best
degreepossible 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 is located in
the Loja Province of southern Ecuador. The concession
was granted to La Plata Minerales S.A. (“PLAMIN”) in
January 2017. PLAMIN is a subsidiary of Sunstone
Metals Ltd. The concession is subject to a Joint Venture
between SolGold Canada Inc. (12.5%) and Sunstone
Metals Ltd. (87.5%). There are no declared wilderness
areas or nationalparks within or adjoiningthe concession

17

Criteria JORC Code explanation Commentary
area. There are no established native 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 Bramaderos Exploration Concession was granted to
La Plata Minerales S.A. (“PLAMIN”) in January 2017.
PLAMIN is now a subsidiary of Sunstone Metals Ltd.
The Bramaderos Concession is subject to a Joint Venture
between Sunstone Metals and SolGold. Sunstone has an
87.5% interest in the JV. SolGold’s 12.5% interest is loan
carried.
Exploration
done by other
parties
Acknowledgment and appraisal of exploration by other
parties.
• The historic exploration at Bramaderos was completed
by various groups over the period 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 (10426m).
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 Limon is a volcanic arc setting of Cretaceous
age intrusions.
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.
• Details of the samples discussed in this announcement
are in the body of the text.
• See Figures 1-7 for the location of rock chip and surface
channel sampling.
If 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, the Competent Person should clearly
explain why this is the case.
• Information included in announcement.
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.
• Weighted averages were calculated over reported
intervals according to sample length.
• No grade cut-offs were applied.
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.
• No aggregating of intervals undertaken at this stage.
The assumptions used for any reporting of metal
equivalent values should be clearly stated.
• Preliminary metallurgical studies are indicating a
standard grind with a flotation circuit. Stage one will
recover copper and the majority of gold as a saleable
concentrate. Stage two is a finer grind with a cyanide
leach for gold on site. Current, overall estimated
recoveries for the combined process are 86% for copper
and 89% forgold.
Relationship
between
If the geometry of the mineralisation with respect to the
drill-hole angle is known, its nature should be
reported.
• Figures 6-7 show the interpreted strike orientation of the
mineralised lodes based on mapping and interpretation
of detailed alteration and structural data.

18

Criteria JORC Code explanation Commentary
mineralisation
widths and
intercept
lengths
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’).
• True widths of mineralised lodes are not known at this
stage.
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.
• See Figures 1-2 and 6-7 for maps showing distribution
of samples.
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.
• Figures 1-2 and 6-7 show the current interpretations of
geology.
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
method of treatment; metallurgical test results; bulk
density,
groundwater,
geotechnical
and
rock
characteristics; potential deleterious or contaminating
substances.
• Figures 1-2 and 6-7 above show various datasets that are
being used to identify target areas and to guide current
and future drilling.
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). _
• The planned exploration program is outlined in the
announcement.
Diagrams clearly highlighting the areas of possible
extensions,
including
the
main
geological
interpretations and future drilling areas, provided this
information is not commercially sensitive.
• See Figures 1-2 and 6-7 which show areas for further
exploration.

19