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FLAGSHIP MINERALS LIMITED Capital/Financing Update 2021

Dec 6, 2021

64923_rns_2021-12-06_12f8aeda-d122-4f07-a8df-9c7bb9d0073f.pdf

Capital/Financing Update

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ASX Announcement | December 07, 2021

Drilling Update Reung Kiet Lithium Prospect, Thailand

HIGHLIGHTS

  • Positive assay results from another four (4) holes completed at the Reung Kiet Lithium Project in southern Thailand.

  • Results include:

  • RKDD027: from 6.9m to 64m hosts 26.35m of composite mineralisation @ 0.84% Li2O.

Incl. 6.40m @ 0.51% Li2O , 406ppm Sn, 263ppm Ta2O5, 821ppm Cs, 0.39% Rb and 2.90% K from 55.80m to 64.20m,

  • and 10.6m @ 1.24% Li2O , 540ppm Sn, 144ppm Ta2O5, 400ppm Cs, 0.43% Rb and 3.21% K from 28.3m-38.9m.

  • RKDD028: from 66m to 68m @ 0.51% Li2O, 667ppm Sn, 70ppm Ta2O5, 127ppm Cs, 0.22% Rb and 2.61% K.

  • RKDD029: from 61m to 73.2m hosts 12.2m @ 0.66% Li2O, 970ppm Sn, 117ppm Ta2O5, 209ppm Cs, 0.31% Rb and 3.03% K.

  • RKDD030: from 11.0m to 83.8m hosts 35.35m of composite mineralisation @ 0.65% Li2O.

Incl. 20.7m @ 0.66% Li2O , 1149ppm Sn, 128ppm Ta2O5, 216ppm Cs, 0.35% Rb and 2.66% K from 46.2m to 66.9m,

  - _and_ 8.25m @ 0.52% Li2O _, 981ppm Sn, 98ppm Ta2O5, 186ppm Cs, 0.28% Rb and 2.76% K from 72m to 80.25m._
  • Tin, tantalum rubidium, cesium and potassium mineralisation occur in association with lithium, and are identified as lithium indicator elements in spot hand-held XRF analysis of drill core.

  • Drilling is ongoing at Reung Kiet.

  • Assay results for holes RKDD031-035 are expected by year end.

  • Samples from holes RKDD036-042 have recently been dispatched to the

  • laboratory.

  • Mineral Resources and Exploration Targets anticipated 1[st] Quarter, 2022, followed by a Scoping Study.

PAN ASIA METALS LIMITED

Level 3, 8 Robinson Road, ASO Building, Singapore, 048544 Level 23, 52 Thaniya Plaza, Silom Road, Bangrak, Bangkok, 10500 www.panasiametals.com

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Specialty metals explorer and developer Pan Asia Metals Limited (ASX: PAM) (‘PAM’ or ‘the Company’) is pleased to provide an update for four (4) more drill holes completed at the Reung Kiet lithium prospect in southwest Thailand. These new holes and the results from previously reported holes continue to support the geological model of extensive lithium mineralisation hosted in lepidolite rich pegmatite dykesveins and adjacent metasediments. The mineralised zone is currently defined over a strike length of 1km, which remains open along strike to the north and south, and at depth on many sections.

Pan Asia Metals Managing Director Paul Lock said: “As per our recent release we continue to be very satisfied with the results we are seeing, which compare very favourably with the lithium mica peer group. We remain on track to deliver a Mineral Resource in 1[st] Quarter 2022. Our drilling results suggest that a 10,000 tonne per annum lithium chemical plant is a realistic objective. Once delivered we of course will be seeking to expand on this with further targets identified in the Reung Kiet blocks as well as in our nearby Kata Thong blocks which are currently under application.”

The Reung Kiet Lithium Project (RKLP) is one of PAM’s key assets. RKLP is a hard rock lithium project with lithium hosted in lepidolite/mica rich pegmatites chiefly composed of quartz, albite, lepidolite and muscovite, with minor cassiterite and tantalite as well as other accessory minerals including some rare earths. Previous open pit mining extracting tin from the weathered pegmatites was conducted into the early 1970’s.

PAM’s objective is to continue drilling with the aim of reporting a Mineral Resource in accordance with the JORC Code 2012. The Mineral Resource will be used as part of a Scoping Study that plans to consider initial production of up to 10,000tpa of LCE and associated by-products. PAM is focusing on lepidolite as a source of lithium as peer group studies indicate that lithium carbonate and lithium hydroxide projects using lepidolite as their plant feedstock have the potential to be placed at the bottom of the cost curve. Lepidolite has also been demonstrated to have a lower carbon emission intensity than other lithium sources.

Reung Kiet Prospect (RK)

The RK Prospect was a relatively large open cut tin mine. The old pit is about 500m long and up to 125m wide (see Figure 1).

Mining of the weathered pegmatites extended up to 25m below surface, to the top of hard rock. Pan Asia has identified a prospective zone at least 1km long in association with extensive surface indications of lithium in trenching, rock-chips and

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soil anomalies, which are now supported by drilling results along the whole of the trend. Lithium mineralisation remains open to the north and south and at depth on many sections (see Figure 1).

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Figure 1. Reung Kiet Prospect, Phang Nga Province, southern Thailand

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Reung Kiet Prospect - Drilling

Pan Asia Metals has been drilling at the Reung Kiet Lithium prospect since mid-March, 2021. PAM has recently received assay results for drillholes RKDD027 to RKDD030.

Collar details for these and other relevant holes are provided in Table 1 - Reung Kiet Drillhole Collars, located in Appendix 1. Assay intersections are presented in Table 2. Further technical details are provided in Appendix 2, being JORC Table 1. Appropriate plans and sections are provided throughout this report.

Assay results for holes RKDD006-012 were previously reported in PAM ASX Announcement dated June 29 and titled “Drilling Update Reung Kiet Lithium Prospect, Thailand”. Assay results for holes RKDD013-015 were reported in PAM ASX Announcement dated August 16 and titled “Drilling Update Reung Kiet Lithium Prospect, Thailand”. Assay results from drillholes RKDD016-022 were reported in PAM ASX Announcement on Sept. 14 titled “Drilling Update-Reung Kiet Lithium Prospect”. Assay results for drillholes RKDD023-026 were reported in recent PAM ASX Announcement on December 3[rd] titled “Drilling Update-Reung Kiet Lithium Prospect”.

As outlined in those announcements, many drillholes have returned zones of lithium mineralisation associated with a swarm of lepidolite rich pegmatite dykes and veins and adjacent altered siltstone.

Technical Discussion

The RK pegmatite trend is divided into two main parts, RK North and RK South, each about 500m long (see Figure 1). RK North includes the old open cut and immediate surrounds. RK South extends along strike to the southeast and encompasses a prominent knoll.

At RK North the pegmatite dykes and veins dip at 65-70 degrees to the south-east. The Main dyke intersected in drilling beneath the pit can be up to 30m wide, narrower dykes and veins also occur, particularly to the east. At RK South the pegmatites form a dyke and vein swarm that dips at angles of 60 to 30 degrees. The pegmatite dykes and veins at RK South are typically more numerous when compared to RK North. The dykes and veins host the bulk of the lithium mineralisation however, it is relatively common for adjacent and intercalated meta-siltstone to contain lithium above the cut-off grade selected.

Along the whole trend from west to east the pegmatite swarm at RK South is approximately 100m wide and may taper slightly to the northeast as RK North is approached (see Figure 2).

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Figure 2. Reung Kiet Prospect, drill collars, sections and surface geochemistry

The whole 1km long trend remains open to the north, south and down dip on many sections. Additional infill and extensional drilling are being undertaken. Drill spacings are designed with the aim of estimating Mineral Resources. With continued success PAM expects to report Mineral Resources in 1[st] Quarter, 2022.

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In this report assay results for drillholes RKDD027-RKDD030 are discussed, and cross sections are presented as shown in Figure 2. Other holes that have been drilled on these sections, but for which assay results are awaited are also discussed.

On Section H, in the central parts of the mineralized trend RKDD027, 036 and 037 were drilled to infill the drill spacing in between drillholes on adjacent sections (see Figure 2).

RKDD027 intersected the pegmatite swarm from 4.2m to 122.6m. The best intersections included 10.6m @ 1.24% Li2O, 540ppm Sn, 144ppm Ta2O5, 400ppm Cs, 0.43% Rb and 3.21% K from 28.3m-38.9m, and 6.40m @ 0.51% Li2O, 406ppm Sn, 263ppm Ta2O5, 821ppm Cs, 0.39% Rb and 2.90% K from 55.80m to 64.20m (see Figure 3). Several other zones of mineralisation are also present in the drillhole (see Table 2). This includes 5m @ 0.86% Li2O from 6.9m.

Drillhole RKDD036 was to test for mineralisation down-dip of RKDD027. RKDD036 intersected the dyke swarm from 48m to 242m. The main part of the swarm occurred from 104m to 223m in which 44.5m of composite pegmatite was intersected. Individual dykes range up to 6.9m wide (see Figure 3). Lepidolite is visible in variable amounts through many sections of pegmatite. Spot hand-held XRF of the drill core has yielded elevated readings for lithium indicator elements such as Rb, Cs and Mn. Additional narrow pegmatites also occur up and downhole from the central part of the dyke swarm (see Figure 3).

Drill RKDD037 was drilled as an infill hole between RKDD027 and 036. In RKDD037 the main part of the pegmatite swarm occurs from approximately 54-154m. This section hosts 29.2m of composite pegmatite thickness, in two main zones from 5470m and 114-154m (see Figure 3). The pegmatites within these intervals contain varying amounts of lepidolite. Spot hand-held XRF of the drill core has returned elevated readings for lithium indicator elements such as Rb, Cs and Mn which are generally associated with lepidolite bearing pegmatites.

This drilled section supports the current interpretation of a wide zone which contains a swarm of pegmatite veins and dykes. Importantly the pegmatite swarm remains open at depth beneath RKDD036.

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Figure 3. Section H showing RKDD027 , RKDD036 and RKDD037.

On Section J, RKDD028 and 035 were drilled as infill holes between previous 100m spaced sections (see Figure 2). RKDD028 intersected generally narrow pegmatites with patchy Li2O grades (see Table 2). RKDD035 intersected the main part of the pegmatite swarm from 104-223m, which hosted a composite pegmatite thickness of 44.5m. Spot hand-held XRF indicates that many of the pegmatites intersected contain elevated lithium indicator elements such as Rb, Cs, Mn as well as Sn and Ta.

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The two drillholes on this section serve to define a zone approximately 110m wide which contains numerous pegmatite veins and dykes (see Figure 4). Assays are awaited for RKDD035 and these results will determine the potential for depth extensions and subsequent drill targeting.

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Figure 4. Section J showing RKDD028 and RKDD035

On Section N, RKDD029 and 040 were targeting mineralisation beneath the old open cut and were drilled as infill holes between previously 100m spaced sections (see

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Figure 2). RKDD029 intersected pegmatite from 49.49m-73.2m, which hosted 12.2m @ 0.66% Li2O from 61m-73.2m (see Figure 5). This zone also contained 0.10% Sn and 117ppm Ta2O5. The remaining pegmatite above this zone from 49.95m-61m returned 13.05m 0.07% Li2O, 0.10% Sn and 113ppm Ta2O5. Cs, Rb and K are also elevated in both intersections (see Table 2).

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Figure 5. Section N showing RKDD029 and RKDD040.

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RKDD040 was drilled to test the down-dip extension of the mineralized zone in RKDD029 and intersected the main pegmatite zone from approximately 116m-157m which contained composite pegmatite thickness of 31.9m. Spot hand-held XRF analysis of pegmatites in this zone commonly returned elevated values for lithium indicator elements Rb, Cs, Mn, Sn and Ta. This was repeated in the narrower pegmatites that occurred above the main zone (see Figure 5). Assays for RKDD040 are expected in early 2022.

On section P holes RKDD030 and 041 were drilled as infill holes targeting mineralisation beneath the old open cut (see Figure 2). RKDD030 retuned several intervals containing lithium and related mineralisation including 20.7m @ 0.69% Li2O from 46.2m and 8.25m @ 0.52% Li2O from 72m (see Figure 6). These zones of mineralisation also contained elevated Sn, Ta, Cs, Rb and K (see Table 2). RKDD030 was drilled to 136m to test for a deeper footwall pegmatite. This target was not intersected.

RKDD041 was drilled to test for mineralisation down-dip of RKDD030. RKDD041 intersected the main pegmatite zone from approximately 108m-140m, which contained a composite pegmatite thickness of 25.1m. Spot hand-held XRF of pegmatites in this zone commonly returned elevated values for lithium indicator elements Rb, Cs, Mn, Sn and Ta. Assays for RKDD041 are expected in early 2022. Additional drilling targeting the pegmatite zone down-dip of RKDD041 maybe warranted subject to assay results.

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Figure 6. Section P showing RKDD030 and RKDD041.

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Forward planning

PAM has further drill holes planned at both the Reung Kiet and Bang I Tum lithium prospects, with the aim of defining Mineral Resources and Exploration Targets. At Reung Kiet drilling will focus on deeper holes at RK South seeking to extend higher grade zones down-dip. Further drilling will also target potential for mineralisation north of the old pit as well as geochemical targets on the eastern and western side of RK South.

The Company looks forward to keeping Shareholders and the market updated on the drilling progress and results obtained from the drilling program at the Reung Kiet Lithium Project.

Ends

Authorised by: Board of Directors

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About the Reung Kiet Lithium Project

The Reung Kiet Lithium Project is a lepidolite style lithium project located about 70km north-east of Phuket in the Phang Nga Province in southern Thailand. Pan Asia holds a 100% interest in 3 contiguous Special Prospecting Licences (SPL) and 1 Exclusive Prospecting License Application covering about 40km².

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Regional map: Location of Phang Nga and the Reung Kiet Lithium Project

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About Pan Asia Metals Limited (ASX:PAM)

Pan Asia Metals Limited (ASX:PAM) is a battery and critical metals explorer and developer focused on the identification and development of projects in Asia that have the potential to position Pan Asia Metals to produce metal compounds and other value-added products that are in high demand in the region.

Pan Asia Metals currently owns three lithium projects and two tungsten projects. Four of the five projects are located in Thailand fitting Pan Asia Metal’s strategy of developing downstream value-add opportunities situated in low-cost environments proximal to end market users.

Complementing Pan Asia Metal’s existing project portfolio is a target generation program which identifies desirable assets in the region. Through the program, Pan Asia Metals has a pipeline of target opportunities which are at various stages of consideration. In the years ahead, Pan Asia Metals plans to develop its existing projects while also expanding its portfolio via targeted and value-accretive acquisitions.

To learn more, please visit: www.panasiametals.com

Stay up to date with the latest news by connecting with PAM on LinkedIn and Twitter.

Investor and Media Enquiries

Paul Lock Anthony Thompson Pan Asia Metals Limited Viriathus Capital Pty Ltd Managing Director 1300 509 924 [email protected] [email protected]

Stay up to date and be informed by scanning this QR Code, we will deliver the latest news and updates directly to you.

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Competent Persons Statement

The information in this Public Report that relates to Exploration Targets, Exploration Results, Mineral Resources or Ore Reserves is based on information compiled by Mr David Hobby, who is a Member of the Australasian Institute of Mining and Metallurgy. Mr Hobby is an employee, Director and Shareholder of Pan Asia Metals Limited. Mr Hobby has sufficient experience that is relevant to the style of mineralization and type of deposit under consideration and to the activity that 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. Mr Hobby consents to the inclusion in the report of the matters based on his information in the form and context in which it appears.

Forward Looking Statements

Various statements in this document constitute statements relating to intentions, future acts and events which are generally classified as “forward looking statements”. These forward looking statements are not guarantees or predictions of future performance and involve known and unknown risks, uncertainties and other important factors (many of which are beyond the Company’s control) that could cause those future acts, events and circumstances to differ materially from what is presented or implicitly portrayed in this document. For example, future reserves or resources or exploration targets described in this document may be based, in part, on market prices that may vary significantly from current levels. These variations may materially affect the timing or feasibility of particular developments. Words such as “anticipates”, “expects”, “intends”, “plans”, “believes”, “seeks”, “estimates”, “potential” and similar expressions are intended to identify forward-looking statements. Pan Asia Metals cautions security holders and prospective security holders to not place undue reliance on these forward-looking statements, which reflect the view of Pan Asia Metals only as of the date of this document. The forwardlooking statements made in this document relate only to events as of the date on which the statements are made. Except as required by applicable regulations or by law, Pan Asia Metals does not undertake any obligation to publicly update or review any forward-looking statements, whether as a result of new information or future events. Past performance cannot be relied on as a guide to future performance.

Important

To the extent permitted by law, PAM and its officers, employees, related bodies corporate and agents (Agents) disclaim all liability, direct, indirect or consequential (and whether or not arising out of the negligence, default or lack of care of PAM and/or any of its Agents) for any loss or damage suffered by a Recipient or other persons arising out of, or in connection with, any use or reliance on this document or information.

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APPENDIX 1

Table 1 - Reung Kiet Drill hole collars

Hole ID East North mASL Dip Azimuth Tot.Depth
(m)
(mag)
RKDD027 433362 918288 31.4 -55 310 125.5
RKDD028 433381 918388 12.7 -55 308 78
RKDD029 433498 918576 13.0 -60 307 85
RKDD030 433543 918658 8.5 -65 310 95
RKDD035 433486 918300 16.7 -55.0 310.2 250.1
RKDD036 433435 918217 24.9 -53.6 311.8 230.5
RKDD037 433395 918250 25.3 -54.3 310.2 167.9

Table 2 – RK Drilling Assay Results

Hole ID from
to

interval
(m)
Li2O
Sn

Ta2O5
Cs
Rb

K
(m) (m) (%) (ppm) (ppm) (ppm) (%) (%)
RKDD027 1.30
3.00 4.30 0.39 172 78 165 0.15 1.03
RKDD027 5.00
6.90 11.90 0.86 445 136 367 0.31 1.86
RKDD027 3.00
6.90 8.90 1.38 355 142 378 0.31 1.81
RKDD027 0.40
25.50 25.90 1.01 489 255 576 0.42 2.74
RKDD027 10.60
28.30 38.90 1.24 540 144 400 0.43 3.21
RKDD027 3.95
43.85 47.80 0.27 187 90 380 0.10 2.76
RKDD027 6.40
55.80 64.20 0.51 406 263 821 0.39 2.90
RKDD027 2.30
59.60 61.90 1.07 468 468 1583 0.92 3.13
RKDD027 1.85
69.30 71.15 0.33 217 70 326 0.15 2.88
RKDD027 0.60
84.20 84.80 0.63 583 88 222 0.27 2.74
RKDD027 2.25
115.25 117.50 0.34 683 103 128 0.20 2.70
RKDD028 0.95
33.40 34.35 0.51 683 131 184 0.24 2.77
RKDD028 2.80
48.00 50.80 0.001 630 145 18 0.05 2.77
RKDD028 0.60
59.10 59.70 0.68 550 96 172 0.26 2.52
RKDD028 2.00
66.00 68.00 0.51 667 70 122 0.22 2.61

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Hole ID from
to

interval
(m)
Li2O
(%)

Sn
(ppm)

Ta2O5
(ppm)
Cs
(ppm)

Rb

K
(m) (m) (%) (%)
RKDD029 11.05 0.07 960 113 45
49.95 61.00 0.14 3.33
RKDD029 12.20 0.66 970 117 209
61.00 73.20 0.31 3.03
RKDD030 5.30 0.60 382 84 220
11.00 16.30 0.24 1.86
RKDD030 0.90 1.32 496 256 489
15.40 16.30 0.54 3.59
RKDD030 20.70 0.69 1149 128 216
46.20 66.90 0.35 2.66
RKDD030 6.00 0.89 1072 164 285
59.00 65.00 0.40 2.55
RKDD030 8.25 0.52 981 98 186
72.00 80.25 0.28 2.76
RKDD030 1.30 1.13 782 242 419
82.50 83.80 0.45 2.16

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APPENDIX 2 - JORC Code, 2012 Edition – Table 1

PAM Lithium Projects. Drilling

Section 1 Sampling Techniques and Data

Criteria JORC Code explanation Commentary
Sampling Nature and quality of sampling (eg cut channels, Cut drillcore samples were selected in order to
techniques random chips, downhole gamma sondes, handheld ascertain the degree of lithium enrichment. The
XRF instruments, etc). samples
are
representative
of
the
lithium
Include reference to measures taken to ensure sample
representivity and the appropriate calibration of any
measurement tools or systems used.
mineralisation within the samples collected.
Drillcore is subjected to spot analysis by hand held
XRF at intervals of around 0.3-0.5m within and
adjacent to pegmatite dykes. The quality of this
Aspects of determination of mineralisation that are sampling is not representative of the core as a whole
Material to the Report (eg ‘RC drilling used to obtain and so the results are viewed as preliminary
1m samples from which 3kg was pulverised to produce indications of the grade of target elements.
a 30g charge for fire assay’; or where there is coarse
gold that has inherent sampling problems).
Certified Reference Material is routinely analysed to
ensure the XRF is operating accurately and/or
precisely.
The
mineralisation
is
contained
within
alpo-
pegmatites. Half HQ3 or NQ3 samples were used with
sample weights of 2.5kg-3.5kg and average sample
interval is 0.99m. The whole sample was fine crushed,
and then split to obtain a 0.5-1kg sub-sample all of
which is pulverised to provide the assay pulp.
Drilling Drill type (eg core, reverse circulation, etc) and details All holes are diamond core from surface. HQ and NQ
techniques (eg core diameter, triple tube, depth of diamond tails, triple tube diameters were employed. The core was
face-sampling bit, whether core is oriented; if so, by oriented using the spear method, as directed by the rig
what method, etc). geologist.
Drill Method of recording and assessing core and chip Drill core recovery is recorded for every drill run by
sample sample recoveries and results assessed. measuring recovered solid core length over the actual
recovery Measures taken to maximise sample recovery, drilled length for that run.
ensuring representative nature of samples. Triple tube drill methods were used to assist with
Is sample recovery and grade related; has sample bias
occurred due to preferential loss/gain of fine/coarse
maximising sample recovery especially in the
weathered zone.
material? Sample recovery through the mineralised zones
averages 96%, so little bias would be anticipated.
Logging Have
core/chip
samples
been
.
geologically/geotechnically logged to a level of detail The drill core was geologically logged at sufficient
to support appropriate resource estimation, mining detail. Geotechnical logging was limited to contact
studies and metallurgical studies. zones and major structures.
Is logging qualitative or quantitative in nature. Core (or The logging is mostly qualitative in nature, with some
costean, channel, etc) photography. quantitative data recorded. Photographs of each core
The total length and percentage of the relevant
intersections logged.
tray wet and dry, and of wet cut core were taken. The
total length of core logged..
Sub- If core, cut or sawn and whether quarter, half or all core All core for sampling was cut in half with a diamond
sampling taken. saw. Some samples were cut as ¼ core from the
techniques
and
sample

If non-core, riffled, tube sampled etc and sampled wet
or dry?
original half core, for QA/QC.
The sample preparation technique is industry
standard, fine crush to 70% less than 2mm. A sub-
For
all
sample
types,
nature,
quality
and
appropriateness of sample preparation technique.
sample of 0.5-1kg or 100% of sample weight if less
than 1kg is obtained via rotary splitting. This sample is
pulverised to 85% passing 75 microns. The laboratory
QAQC procedures for all sub-sampling stages to reports QA/QC particle size analysis for crushed and
maximise representivity of samples. pulverised samples. The laboratory also reports

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Criteria JORC Code explanation Commentary
Measures taken to ensure sampling is representative
results for internal standards, duplicates, prep
of the material collected, e.g. results for field duplicates and blanks. Pan Asia has collected ¼ core
duplicate/second-half sampling. pairs. Comparison of results indicate excellent
Whether sample sizes are appropriate to the grain size agreement between Li2O grades from each ¼ pair.
of the material being sampled. The sample weights average 2.8kg. This is considered
appropriate for the material being sampled.
Quality of Nature, quality and appropriateness of the assaying Analysis in by ALS Method ME-MS89L, which uses a
assay data and laboratory procedures used; whether the sodium peroxide digestion with ICP finish, all by ALS
and technique is considered partial or total. Chemex in Vancouver or Perth. The method is
laboratory
tests
For geophysical tools, spectrometers, handheld XRF
instruments etc, parameters used in determining the
analysis including instrument make and model,
considered a total technique. Multielement analysis is
done by sodium peroxide digestion with ICP-MS finish
with 49 elements reported.
reading times, calibrations factors applied, their
derivation, etc.
The laboratory reports results for internal standards,
duplicates, prep duplicates and blanks. PAM has
Nature of QAQC procedures adopted (eg standards, conducted ¼ sampling and re-analysis of sample
blanks, duplicates, external laboratory checks); pulps utilising different digestion and assay methods,
whether acceptable accuracy levels (ie lack of bias) / Pan Asia inserts its own internal Li “standards” as
precision established. pulps and blanks as 0.5kg. Both the lab QA/QC and
additional PAM data indicate acceptable levels of
accuracy and precision for Li assays, PAM has only
utilised internal ALS QA/QC for the multielement data.
For spot hhXRF analysis, an Olympus Vanta+ X-Ray
Flourescence analyser in Geochem3_extra mode,
with analysis for 30 seconds. Li cannot be analysed by
hhXRF. However, Rb, Cs, Mn, show good correlation
with lab reported Li results. Other elements of interest
such as Sn. Ta and Nb are also recorded by hhXRF
as well as many others. Certified standards are
routinely analysed.
Verification Verification of significant intersections by independent Sample results have been checked by company
of
sampling
and
assaying
/ alternative company personnel.
The use of twinned holes.
Documentation
of
primary
data,
data
entry
Chief
Geologist
and
Senior
Geologist.
Li
mineralisation is associated with visual zones of
distinctively coloured lepidolite.
procedures, data verification, data storage (physical Assays reported as Excel xls files and secure pdf files.
and electronic) protocols.
Discuss any adjustment to assay data. Data entry carried out both manually and digitally by
Geologists. To minimize transcription errors field
documentation procedures and database validation
are conducted to ensure that field and assay data are
merged accurately.
The adjustments applied to assay data for reporting
purposes:
Li x 2.153 to convert to Li to Li2O. Ta is converted to
Ta2O5,by multiplying Ta by 1.221.
Location of Accuracy and quality of surveys used to locate drill Drill hole locations up to RKDD038 are derived from
data points holes (collar and down-hole surveys), trenches, mine DGPS_,_with_a_pproximately 10cm accuracy. RKDD039
workings etc used in estimation. and onwards are sited by handheld GPS with accuracy
Specification of grid system used. of 2-5m in XY. The Z value is derived from topographic
model with 1m accuracy.
Quality and adequacy of topographic control. All locations reported are UTM WGS84 Zone 47N.

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Criteria JORC Code explanation Commentary
Data Data spacing for reporting of Exploration Results. The drilling was conducted on variably spaced
spacing
and
distribution
Is data spacing and distribution sufficient to establish
degree of geological and grade continuity appropriate
for Resource / Reserve estimation procedure(s) and
sections with holes 50-100m apart on section, with two
holes on many sections giving down-dip separations
of about 50-100m between holes.
classifications applied? Resources or reserves are not being reported.
Whether sample compositing has been applied.
Sample compositing relates to reporting total
aggregate pegmatite thickness, over a drilled interval.
Grades are then reported byweighted average.
Orientation Does the orientation of sampling achieve unbiased The sampling of half core and ¼ core supports the
of data in sampling of possible structures; extent to which this is unbiased nature of the sampling.
relation to known/understood.
geological
structure
If relationship between drilling orientation and
orientation of mineralised structures has introduced a
The drill holes reported are drilled normal or very near
normal to the strike of the mineralised zone.
sampling bias, this should be assessed and reported
if material.
Sample The measures taken to ensure sample security. Samples are securely packaged and transported by by
security company personnel or reputable carrier to the Thai-
Laos border, where ALS laboratory personnel take
delivery or the samples are on forwarded to ALS Laos.
Pulp samples for analysis are then air freighted to
Vancouver or Perth in accordance with laboratory
protocols.
Audits or The results of any audits or reviews of sampling No formal audits conducted at this stage of the
reviews techniques and data. exploration program.

Section 2 Reporting of Exploration Results

Criteria Criteria JORC Code explanation Commentary
Mineral Type,
reference
name/number,
location
and
Three contiguous Special Prospecting Licences
tenement and ownership including agreements or material issues (JSPL1, 2 and 3) covering an area of 48sq km are
land tenure with third parties such as joint ventures, partnerships, registered to Thai company Siam Industrial Metals
status overriding royalties, native title interests, historical Co. Ltd. (SIM). Pan Asia Metals holds 100% of SIM
sites, wilderness or national park and environmental located 60km north of Phuket in southern Thailand.
settings. The tenure is secure and there are no known
The security of the tenure held at the time of
reporting along with any known impediments to

impediments to obtaining a licence to operate, aside
from normal considerations.
obtaining a licence to operate in the area.
Exploration Acknowledgment and appraisal of exploration by The Institute of Geological Sciences, a precursor of
done by other other parties. the British Geological Survey (BGS) in the late
parties 1960’s conducted geological mapping, documenting
old workings, surface geochemical sampling, mill
concentrates and tailings sampling and metallurgical
test work on the pegmatite then being mined at
Reung Kiet. This work appears to be of high quality
and is in general agreement with Pan Asia’s work.
In 2014 ECR Minerals reported Li results for rock
samples collected in Reung Kiet project area. The
locations and other details of the samples were not
reported. But the samples showed elevated Li
contents.
Geology Deposit type, geological setting and style of The project is located in the Western Province of the
mineralisation. South-East Asia Tin Tungsten Belt. The Reung
project area sits adjacent and sub-parallel to the
regionally extensive NE trending Phangnga fault.
The Cretaceous age Khao Po granite intrudes into
Palaeozoic agePhuket Group sediments along the

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Criteria JORC Code explanation Commentary
fault zone, Tertiary aged LCT pegmatite dyke
swarms intrude parallel to the fault zone.
Drillhole A
summary
of
information
material
to
the
Drillhole information and intersections are reported in
Information understanding of the exploration results including a tabulated from within the public report.
tabulation for all Material drill holes of:

easting and northing of the drill hole collar

elevation or RL (Reduced Level – elevation above
sea level in meters) of the drill hole collar

dip and azimuth of the hole

downhole length and interception depth

hole length.
If exclusion of this information is not Material, the
Competent Person should clearly explain why this is
the case.
Data Weighting
averaging
techniques,
maximum/
Intersections are reported at > 0.2% Li2O, and may
aggregation minimum grade cutting and cut-off grades are rarely, allow for internal dilution of < 0.2% Li2O. No
methods Material and should be stated. top cut has been applied.
Where compositing short lengths of high grade
results and longer lengths of low grade results,
compositing
procedure
to
be
stated;
typical
Higher grade zones within the bulk lower grade
zones are reported, where material.
examples of such aggregations to be shown in detail.
Assumptions for metal equivalent values to be clearly
stated.
Relationship These relationships are particularly important in the Intercept lengths are reported as downhole length.
between reporting of Exploration Results.
mineralisation
widths
and
intercept
If mineralisation geometry with respect to the drillhole
angle is known, its nature should be reported.
The mineralised zones dip around 65-55 degrees
southeast. Holes were drilled at -55 to -65 degrees
lengths If it is not known and only down hole lengths are
reported, a clear statement to this effect is required
(eg ‘down hole length, true width not known’).
towards the northwest (normal to strike). The true
width of the mineralisation reported is around 75-
90% of the reported downhole width.
Diagrams Appropriate maps and sections (with scales) and Appropriate plans and sections are provided in the
tabulations of intercepts to be included for any public report.
significant discovery. These to include (not be limited
to) plan view of collar locations and appropriate
sectional views.
Balanced Where comprehensive reporting of all Exploration Results are reported for every drillhole, that are
reporting Results is not practicable, representative reporting of above cut-off grade. Some results below Li2O cut-off
both low and high grades and/or widths should be grade are reported to assist interpretation.
practiced to avoid misleading reporting of Exploration
Results.
Other Other exploration data, if meaningful and material, The drilling results reported are from holes targeting
substantive should be reported including (but not limited to): mineralisation beneath and along strike from an old
exploration geological observations; geophysical survey results; open cut. Soil, rock-chip and trench sampling by Pan
data geochemical survey results; bulk samples – size and Asia indicate additional mineralisation is present
method of treatment; metallurgical test results; bulk along trend to the south, where drillholes are also
density,
groundwater,
geotechnical
and
rock
reported Weaker surface Li anomalism is also
characteristics;
potential
deleterious
or
present immediately north of the pit. The whole
contaminating substances. mineralised trend at RK are potentially 1km or more.
Garson et al 1969 conducted work on concentrates,
tailings and met test-work on a sample taken from the
mine. This work was positive, no deleterious
substanceshave been identified to date.
Further work The nature and scale of planned further work (eg Planned further work will include drilling especially
tests for lateral extensions or depth extensions or along strike to the south. Infill drilling is also planned
large-scale step-out drilling). around existing holes that have intersected higher
grademineralisation. Thismaylater lead to

21

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Criteria JORC Code explanation Commentary
Diagrams clearly highlighting the areas of possible
deeper/step out drilling should geological controls on
extensions,
including
the
main
geological

higher grade zones be identified.
interpretations and future drilling areas (if not
commercially sensitive).
Criteria JORC Code explanation Commentary
Sampling Nature and quality of sampling (eg cut channels, Cut drillcore samples were selected in order to
techniques random chips, downhole gamma sondes, handheld ascertain the degree of lithium enrichment and The
XRF instruments, etc). samples
are
representative
of
the
lithium
Include reference to measures taken to ensure sample mineralisation within the samples collected.
representivity and the appropriate calibration of any
measurement tools or systems used. The
mineralisation
is
contained
within
alpo-
Aspects of determination of mineralisation that are
Material to the Report (eg ‘RC drilling used to obtain
1m samples from which 3kg was pulverised to produce
a 30g charge for fire assay’; or where there is coarse
gold that has inherent sampling problems).
pegmatites. Half HQ3 or NQ3 samples were used
average sample weight of 2.5kg-3.5kg and average
sample interval was 0.99m. The whole sample was
fine crushed, and then split to obtain a 0.5-1kg sub-
sample all of which is pulverised to provide the assay
pulp.
Drilling Drill type (eg core, reverse circulation, etc) and details All holes are diamond core from surface. HQ and NQ
techniques (eg core diameter, triple tube, depth of diamond tails, triple tube diameters were employed. The core was
face-sampling bit, whether core is oriented; if so, by oriented using the spear method, as directed by the rig
what method, etc). geologist.
Drill Method of recording and assessing core and chip Drill core recovery is recorded for every drill run by
sample sample recoveries and results assessed. measuring recovered solid core length over the actual
recovery Measures taken to maximise sample recovery, drilled length for that run.
ensuring representative nature of samples. Triple tube drill methods were used to assist with
Is sample recovery and grade related; has sample bias
occurred due to preferential loss/gain of fine/coarse
maximising sample recovery especially in the
weathered zone.
material? Sample recovery through the mineralised zones
averages 97%, so little bias would be anticipated.
Logging Have
core/chip
samples
been
.
geologically/geotechnically logged to a level of detail The drill core was geologically logged at sufficient
to support appropriate resource estimation, mining detail. Geotechnical logging was limited to contact
studies and metallurgical studies. zones and major structures.
Is logging qualitative or quantitative in nature. Core (or The logging is mostly qualitative in nature, with some
costean, channel, etc) photography. quantitative data recorded. Photographs of each core
The total length and percentage of the relevant
intersections logged.
tray wet and dry, and of wet cut core were taken. The
total length of core logged..
Sub- If core, cut or sawn and whether quarter, half or all core All core for sampling was cut in half with a diamond
sampling taken. saw. Some samples were cut as ¼ core from the
techniques
and
sample

If non-core, riffled, tube sampled etc and sampled wet
or dry?
original half core, for QA/QC.
The sample preparation technique is industry
standard, fine crush to 70% less than 2mm. A sub-
For
all
sample
types,
nature,
quality
and
appropriateness of sample preparation technique.
sample of 0.5-1kg or 100% of sample weight if less
than 1kg is obtained via rotary splitting. This sample is
pulverised to 85% passing 75 microns. The laboratory
QAQC procedures for all sub-sampling stages to reports QA/QC particle size analysis for crushed and
maximise representivity of samples. pulverised samples. The laboratory also reports
Measures taken to ensure sampling is representative
of the material collected, e.g. results for field
duplicate/second-half sampling.

results for internal standards, duplicates, prep
duplicates and blanks. Pan Asia has collected ¼ core
pairs. Comparison of results indicate excellent
agreement between Li2O grades from each ¼ pair.
Whether sample sizes are appropriate to the grain size
of the material being sampled.

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Criteria JORC Code explanation Commentary
The sample weights average 2.6kg. This is considered
appropriate for the material being sampled.
Quality of Nature, quality and appropriateness of the assaying Assaying is performed by ALS Method ME-MS89L
assay data and laboratory procedures used; whether the which is a sodium peroxide digestion with ICP finish,
and technique is considered partial or total. all by ALS Chemex in Vancouver or Perth. The method
laboratory
tests
For geophysical tools, spectrometers, handheld XRF
instruments etc, parameters used in determining the
is considered a total technique. Multielement analysis
with 49 elements is also reported,
analysis including instrument make and model,
reading times, calibrations factors applied, their
derivation, etc.
The laboratory reports results for internal standards,
duplicates, prep duplicates and blanks. PAM has
conducted ¼ sampling and re-analysis of sample
Nature of QAQC procedures adopted (eg standards, pulps utilising different digestion and assay methods,
blanks, duplicates, external laboratory checks); Pan Asia inserts its own internal Li “standards” as
whether acceptable accuracy levels (ie lack of bias) / pulps and blanks as 0.5kg. Both the lab QA/QC and
precision established. additional PAM data indicate acceptable levels of
accuracy and precision for Li assays, PAM has only
utilised internal ALS QA/QC for the multielement data..
Verification Verification of significant intersections by independent Sample results have been checked by company
of
sampling
and
assaying
/ alternative company personnel.
The use of twinned holes.
Documentation
of
primary
data,
data
entry
Chief
Geologist
and
Senior
Geologist.
Li
mineralisation is associated with visual zones of
distinctively coloured lepidolite.
procedures, data verification, data storage (physical Assays reported as Excel xls files and secure pdf files.
and electronic) protocols.
Discuss any adjustment to assay data. Data entry carried out both manually and digitally by
Geologists. To minimize transcription errors field
documentation procedures and database validation
are conducted to ensure that field and assay data are
merged accurately.
The adjustments applied to assay data for reporting
purposes:
Li x 2.153 to convert to Li to Li2O and Ta x 1,221 to
convert Ta to Ta2O5.
Location of Accuracy and quality of surveys used to locate drill Drill hole locations are derived from hand held GPS_,_
data points holes (collar and down-hole surveys), trenches, mine with_a_pproximately 2-5m accuracy, sufficient for this
workings etc used in estimation. type of reconnaissance drilling.
Specification of grid system used. All locations reported are UTM WGS84 Zone 47N.
Quality and adequacy of topographic control. Topographic locations interpreted from Thai base
topographyin conjunction with GPS results.
Data Data spacing for reporting of Exploration Results. The drilling was conducted on variably spaced
spacing
and
distribution
Is data spacing and distribution sufficient to establish
degree of geological and grade continuity appropriate
for Resource / Reserve estimation procedure(s) and
sections with holes 50-100m apart on section, with two
holes on many sections giving down-dip separations
of about 70-100m between holes.
classifications applied? Resources or reserves are not being reported.
Whether sample compositing has been applied.
Sample compositingwas not applied
Orientation Does the orientation of sampling achieve unbiased The sampling of half core and ¼ core supports the
of data in sampling of possible structures; extent to which this is unbiased nature of the sampling.
relation to known/understood.
geological
structure
If relationship between drilling orientation and
orientation of mineralised structures has introduced a
The drill holes reported are drilled normal or near
normal to the strike of the mineralised zone.
sampling bias, this should be assessed and reported
if material.
Sample The measures taken to ensure sample security. Samples are securely packaged and transported by by
security company personnel or reputable carrier to the Thai-
Laos border,where ALS laboratory personnel took

23

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Criteria JORC Code explanation Commentary
delivery or the samples are on forwarded to ALS Laos.
Pulp samples for analysis are then air freighted to
Vancouver or Perth in accordance with laboratory
protocols.
Audits or The results of any audits or reviews of sampling No formal audits conducted at this stage of the
reviews techniques and data. exploration program.

24