DTM Walwa Rock Chip and Site Visit
Released
Released
Announcement PDF
Dart Mining NL
ABN: 84 119 904 880
Level 6, 412 Collins Street
Melbourne VIC 3000
Contact: James Chirnside
Email: jchirnside@dartmining.com.au
Mobile: +61 447 447 613
Webpage: www.dartmining.com.au
LinkedIn: Dart Mining NL
Twitter: @DartMining
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ASX Release
25th June 2026
WALWA TIN-TUNGSTEN PROJECT SITE VISIT AND OBSERVATIONS
Dart Mining NL (ASX:DTM) (Dart Mining or the Company) is pleased to announce that Dart
Geologists have recently visited the historic Walwa Tin mine as part of its review of its Victorian tin-
tungsten projects (the Project) in Northeast Victoria. Strong metal prices have prompted further
examination of tin-tungsten prospectivity on these tenements given their long history of tin and
tungsten mining. Walwa has the highest recorded primary tin production in Victoria, principally
from the Walwa tin mine with limited production from the Mt Alwa and Bounce tin mines within
EL007426 at Walwa1.
HIGHLIGHTS
The Project area has substantial recorded tin and tungsten production. Inspection of the historic
Walwa tin mine area and available data revealed:
• Abundant sub-horizontal aplite-pegmatite dykes were observed at Mt Alwa South. The
upper dyke at the Walwa tin mine was also sampled from the SW wall of the historic open
pit last worked in the 1970s;
• Extensive historic diamond and RC drilling at Walwa are currently being digitally compiled
for further assessment. Approximately 20 diamond and 100 RC percussion drill holes have
been drilled at Walwa since the late 1960s;
• Assays from samples are due to be received in 3-4 weeks;
• Further field inspections are also planned for other key prospects within the tenement
package;
• There is an extensive access track network suitable for drilling at Mount Alwa South, Mt
Alwa, Walwa tin mine as well as at the Bounce tin mine. The access tracks to each prospect
are still in in good condition, and suitable for access by drill rigs and support equipment.
Dart Mining’s Chairman, James Chirnside, commented: “Field inspection of the Walwa tin mine
area was an important first reconnaissance step in our potential diamond drilling program –
scheduled for August / September - targeting the tin bearing aplite-pegmatite dykes at Victoria’s
largest hardrock tin production mine. The team is excited around the interpretation of the geology
of the area and keen to explore the tenement further.”
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Dart holds 100% owned granted tenements at Walwa (EL007426 – 499sq.km), Cudgewa (EL006866
– 508sq.km) and Berringama (EL007170 – 27sq.km) which are shown in Figure 1. Dart Mining’s early
interpretation is that the apical zone of the stacked, dome forming, sub-horizontal aplite-pegmatite-
greisen dykes at the Walwa tin mine is an obvious target for a deeper drill hole seeking a possible
tin rich greisen at the topmost part of an underlying causative intrusion.
Figure 1 – Tenement location showing historic tin and tungsten mines and prospects
WALWA TIN MINE
The upper dyke at the Walwa tin mine was observed and sampled from the SW wall of the historic
open pit last worked in the 1970s. The in-situ grab sample was comprised of pegmatite with black
minerals interpreted to be coarse cassiterite. The pegmatite appears to represent a small fragment
of the mined ore left behind during open pit operations.
Float samples of pegmatite were taken from the floor of the historic pit at its southern extremity
and immediately outside its northern edge. Further interpreted tin bearing coarse cassiterite was
observed from all three locations. The four collected samples have been submitted to Intertek
Laboratory for analysis. A summary of the location and field description of the samples is provided
in Table 1. Photos of the rock chip samples is shown in Figure 2 and Figure 3.
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Table 1 - Samples taken from the Walwa tin mine area on EL007426
Sample ID Location Description
WAS001 Mt Alwa South
Grab sample of pegmatite from a sub-horizontal dyke with an observed thickness of 5m
to 8m.
WWP001 Walwa Pit 1
Float of greisenous pegmatite with black minerals interpreted to be coarse cassiterite
subject to assay confirmation. The boulder this sample was taken from was on the floor
of the southern end of the Walwa tin mine pit. The upper dyke was worked in this
location.
WWP002 Walwa Pit 2
In-situ grab sample of pegmatite with black minerals interpreted to be coarse cassiterite
subject to assay confirmation. The pegmatite formed the SW wall of the historic open pit
and appears to represent a small fragment of the mined ore left behind during open pit
operations.
WWP003 Walwa Pit 3
Float from the Upper dyke at the northern end of the Walwa tin mine pit. The pegmatite
rock was aplite with large potassium feldspars to 60mm across. Interpreted coarse
cassiterite was observed subject to assay confirmation.
Figure 2 – Sample WWP0011
showing interpreted black cassiterite in pegmatite boulder from the floor of the historic
Walwa open pit
1
Visual estimates of mineral abundance should never be considered a proxy or substitute for laboratory analyses
where concentrations or grades are the factor of principal economic interest. Visual estimates also potentially provide
no information regarding impurities or deleterious physical properties relevant to valuations
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Figure 3 – Sample WWP0021
with interpreted black cassiterite in pegmatite from the pit wall of the historic Walwa
open pit
GEOLOGY OF THE WALWA TIN ZONE
A number of shallow dipping tin-bearing greisenous aplite/pegmatite dykes are found in the Walwa-
Mt Alwa historic mine area and have been worked at various periods for a century with mining first
commencing around 1882 with large open pit workings developed in the 1970s when 97,000t was
excavated and processed. The sub-horizontal dykes cut across the vertical sedimentary country
rocks.
The country rocks are knotted schists, phyllites and quartzites found throughout the region. The
prominent foliation/ bedding strikes at 160° magnetic with vertical or subvertical dips. Joints are
irregularly developed with variable direction and dip.
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At the Walwa mine four major dykes can be recognised at surface and in addition two other dykes
were detected during previous drilling. These dykes are from 1 to 8 metres thick, with variable strike.
They generally dip at 20-30° to the north or north-east in the vicinity of the Walwa mine but form a
dome with dip becoming north westerly as one traverses west from the historic mine.
The dykes themselves are predominantly aplite with pegmatite and greisen phases, often containing
coarse cassiterite along their margins and large potassium feldspar crystals. Tantalum and Niobium
have been recorded in previous assays from the project area2.
Walwa is an early drill target for multiple sub-horizontal tin lodes to 8m thickness and a possible tin
rich greisen zone at the top of a causative intrusion. The existing open pit was last worked in the
1970's with the production and treatment of 97,000t of tin bearing ore. The Bounce lode is a sub-
horizontal pegmatite dyke with a vertical dyke interpreted as a vertical feeder structure.
Around 20 diamond drill holes and over 100 RC percussion drill holes have been drilled at Walwa
since the late 1960’s and developing a 3-D model is an important early step to understanding the
potential of the tin lodes present at the Walwa, Mt Alwa South and The Bounce historic mines. These
mines fall within a north south corridor over 2km long and 500-600m wide.
Figure 4 – Sample WWP0031
with interpreted black cassiterite in pegmatite from outside the northern pit wall of the
historic Walwa open pit.
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MT ALWA SOUTH
The Mt Alwa South prospect is located around 500m SSW of the Walwa tin mine and appears to
have been discovered and drilled after 1960 with no recorded historic production. Minor historic
alluvial tin workings were observed in the narrow gullies leading from the area.
Mt Alwa South has four existing bulldozed benches which served as drilling locations for previous
RC percussion drilling. These benches are cut into the mountain with switchback connections at
the bench end, each bench is 10m to 15m higher in elevation than the last.
Extensive sub-horizontal aplite-pegmatite dykes 5m to 8m thick were observed and one sample
taken for assay (see Figure 5 and Table 1).
Figure 5 – Sample WAS0011
from Mt Alwa South showing quartz-K-spar and mica with minor fine-grained
sulphide.
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Figure 6 – Mt Alwa South showing outcrop of pegmatite dyke and bulldozed bench previously used for drill
access.
THE BOUNCE
The Bounce lode is a sub-horizontal pegmatite dyke with a vertical dyke interpreted as a vertical
feeder structure from a causative intrusion. Workings were limited to a few shallow pits of small
extent with the largest being approximately 25m by 12m and around 3m deep. No samples were
taken. The pegmatite observed was rich is coarse white mica.
TUNGSTEN PROSPECTIVITY
Dart is currently collating and reviewing the large historic mining and exploration dataset on the
Project area to determine the next steps towards an assessment of tungsten prospectivity. Historic
tungsten mines and known tungsten occurrences are present in EL007426 and EL006866 with key
exploration prospects at McHargs and the Koetong field. Field inspection of these prospects is
scheduled for this year.
MCHARGS TUNGSTEN PROSPECT
Parallel scheelite mineralised lodes are known at the McHargs Tungsten Project, 5km southeast of
Walwa. McHargs was previously explored at a time of low tungsten prices and was deemed non-
economic at the time. Given the record high tungsten prices and increasing demand, McHargs
Tungsten Prospect is situated on private property and provides a strong priority exploration target.
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KOETONG TUNGSTEN
Koetong, in EL007426, is best known for tungsten deposits with historic mines at Keady's, Roper's,
Roper and O'Doughlin's, and Mclntyre's (Cochrane and Bowen, 1971). Quartz reefs occur, which
contain wolfram and/or scheelite and in addition some cassiterite and, occasionally, gold (Cochrane
and Bowen, 1971).
NEXT STEPS
• Compilation and assessment of the large historic mining and exploration data set across the
tenements is ongoing with over 100 detailed reports identified to date;
• Develop a 3D model of previous drilling and mineralisation style at Walwa to determine high priority
drill targets;
• Consider theoretical models for a tin-rich zone at the topmost part of a possible causative intrusion
below the parallel stacked sub-horizontal dykes at Walwa tin mine and determine optimum drilling
locations and depths; and
• Early field inspection of other key prospects to assess access for drilling and to undertake limited rock
chip sampling to confirm tin, tungsten, tantalum and niobium grades.
Approved for release by the Board of Directors.
For more information contact:
James Chirnside
Managing Director
Dart Mining NL
jchirnside@dartmining.com.au
+61 419 605 842
InvestorHub Link
Terry Bates
Director
Dart Mining NL
tbates@dartmining.com.au
REFERENCES
• Bowen (1970). Mt Alwa and The Bounce Tin Mines. Mining and Geological Journal, Victoria. Vol 6,
No 6.
• Cochrane and Bowen(1971). Tin Deposits of Victoria. Geological Survey of Victoria, Bulletin No 60.
• Greive (1938). Tungsten Ores in North-Eastern Victoria. Mining and Geological Journal, Victoria.
January 1938.
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About Dart Mining
The Triumph Gold Project is Dart’s first step into an advanced intrusion related gold system project in
Queensland. Dart will look to develop a regional presence in Queensland through advanced stage intrusion
related and epithermal gold projects. Dart is farming into the Coonambula Antimony-Gold Project in Central
Queensland. Dart Mining will continue to evaluate several historic Tin, Tungsten, and Gold prospects in
Central and Northeast Victoria including the Rushworth Gold, and Walwa Tin / Tungsten prospects.
Competent Person’s Statement
The information in this report has been prepared, compiled, and verified by Mr Andrew Dawes, who is a
Member of the Australasian Institute of Mining and Metallurgy and a Member of the Australian Institute of
Geoscientists. Mr Andrew Dawes is employed by AHD Resources and consults to Dart Mining NL. Mr Dawes
has sufficient experience that is relevant to the style of mineralisation and type of deposits under
consideration and to the activity being undertaken 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. Dawes takes responsibility for the exploration results, and 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 Statement
Certain statements contained in this document constitute forward-looking statements. Forward-looking
statements include, but are not limited to, Dart Mining’s current expectations, estimates and projections
about the industry in which Dart Mining operates, and beliefs and assumptions regarding Dart Mining’s future
performance. Such forward-looking statements are based on a number of estimates and assumptions made
by the Company and its consultants in light of experience, current conditions and expectations of future
developments which the Company believes are appropriate in the current circumstances. When used in this
document, words such as; “anticipate”, “could”, “intends”, “estimate”, “potential”, “plan”, “seeks”, “may”,
“should”, and similar expressions are forward-looking statements. Although Dart Mining believes that its
expectations presented in these forward-looking statements are reasonable, such statements are subject to
known and unknown risks, uncertainties and other factors, which may cause the actual results, achievements
and performance of the Company to be materially different from the future results and achievements
expressed or implied by such forward-looking statements. Investors are cautioned that forward-looking
information is no guarantee of future performance and accordingly, investors are cautioned not to place
undue reliance on these forward-looking statements.
No new information has been included in this release, all exploration results have been previously reported
and are available on the GSV website. Dart Mining is not aware of any new information or data that materially
affects the information included in the original announcements.
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APPENDIX 1: SUMMARY OF SAMPLES COLLECTED
Table 1: Sample Summary
Sample
ID
Easting Northing Sample Type Description
WAS001 563551 6020217 Outcrop
Grab sample of pegmatite from a sub-horizontal dyke with an
observed thickness of 5m to 8m.
WWP001 564026 6020942 Float
Float of greisenous pegmatite with black minerals interpreted
to be coarse cassiterite subject to assay confirmation. The
boulder this sample was taken from was on the floor of the
southern end of the Walwa tin mine pit. The upper dyke was
worked in this location.
WWP002 564016 6020944 Outcrop
In-situ grab sample of pegmatite with black minerals
interpreted to be coarse cassiterite subject to assay
confirmation. The pegmatite formed the SW wall of the historic
open pit and appears to represent a small fragment of the
mined ore left behind during open pit operations.
WWP003 563987 6021105 Outcrop
Float from the Upper dyke at the northern end of the Walwa tin
mine pit. The pegmatite rock was aplite with large potassium
feldspars to 60mm across. Interpreted coarse cassiterite was
observed subject to assay confirmation.
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APPENDIX 2: JORC CODE, 2012 EDITION – TABLE 1 REPORT
Section 1 Sampling Techniques and Data
Criteria JORC Code explanation Commentary
Sampling
techniques
• Nature and quality of sampling (eg cut channels,
random chips, or specific specialised industry standard
measurement tools appropriate to the minerals under
investigation, such as down hole gamma sondes, or
handheld XRF instruments, etc). These examples
should not be taken as limiting the broad meaning of
sampling.
• Include reference to measures taken to ensure sample
representivity and the appropriate calibration of any
measurement tools or systems used.
• 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 (eg ‘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 (eg submarine nodules) may
warrant disclosure of detailed information.
• Rockchip samples were collected
from identified outcrops using rock
hammers. The samples are between
0.5 and 2.0kg and were collected in
marked calico bags for assaying.
• Rockchip samples were collected by
hand and in several locations and in
some instances, multiple samples
were collected from a single outcrop
or float site to understand the
variability of the material.
• Measurements of the apparent
thickness of these outcrops are
reported in the announcement where
possible. These are apparent as the
true orientation of the outcrops are
not fully known yet. The visual
estimates here are of the thickness of
the outcrop only.
Drilling
techniques
• Drill type (eg core, reverse circulation, open-hole
hammer, rotary air blast, auger, Bangka, sonic, etc) and
details (eg 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).
• No drilling results are reported and is
not applicable.
Drill sample
recovery
• Method of recording and assessing core and chip
sample recoveries and results assessed.
• Measures taken to maximise sample recovery and
ensure representative nature of the samples.
• 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 drilling results are reported and is
not applicable.
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.
• Whether logging is qualitative or quantitative in nature.
Core (or costean, channel, etc) photography.
• The total length and percentage of the relevant
intersections logged.
• Basic descriptions of the outcrops
were made in the field by Dart Mining
personnel which include observations
of crystal/mineral habit, orientation of
the outcropping units, and mineral
identification where possible. These
logs are sufficient to support the
preliminary nature of assessing the
outcrops.
• Logging of the rockchip samples is
qualitative in nature.
Sub-
sampling
techniques
and sample
preparation
• If core, whether cut or sawn and whether quarter, half or
all core taken.
• If non-core, whether riffled, tube sampled, rotary split,
etc and whether sampled wet or dry.
• For all sample types, the nature, quality and
appropriateness of the sample preparation technique.
• Quality control procedures adopted for all sub-sampling
stages to maximise representivity of samples.
• 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.
• Whether sample sizes are appropriate to the grain size
of the material being sampled.
• No field sub sampling has been
undertaken on the samples. Whole
rocks were submitted to the
laboratory for standard crushing and
pulverizing with the laboratory taking
representative sub-samples as
required for analysis as per their
accredited protocols.
• The sampling technique is
appropriate for the sample type and
material sampled. The rocks will be
crushed to -2mm and then pulverized
to -75um for multi element acid digest
analysis and fusion analysis for Sn
and W.
• Sub-sampling QAQC is not
applicable to this announcement.
• Samples are selectively taken from
outcrops. The samples represent
rockchips that are of geological
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Criteria JORC Code explanation Commentary
interest for a variety of reasons
including crystal size, shape, colour
and alteration presented to the
sampler. The sampling is not
representative of the entire outcrops
intercepted in the field, but rather to
test if the outcrops have the potential
to be mineralised.
• Sample sizes are appropriate for the
analysis proposed and the master
pulp after pulverization and initial
analysis should be sufficient for
additional testing if required.
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.
• 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.
• Nature of quality control procedures adopted (eg
standards, blanks, duplicates, external laboratory
checks) and whether acceptable levels of accuracy (ie
lack of bias) and precision have been established.
• Samples have been submitted to the
laboratory, no results are available,
and the laboratory methods are not
reported or applicable to this
announcement.
• No geophysical tools were used.
• Laboratory test results are not
available yet but will be addressed
upon announcement of results.
Verification
of sampling
and
assaying
• The verification of significant intersections by either
independent or alternative company personnel.
• The use of twinned holes.
• Documentation of primary data, data entry procedures,
data verification, data storage (physical and electronic)
protocols.
• Discuss any adjustment to assay data.
• Samples have been submitted to the
laboratory and no results are
available yet and therefore cannot
address any results.
• Logging and photographs of the
samples were completed by
experienced Dart Mining personnel.
These photos were reviewed by the
Competent Person remotely prior to
being submitted to the laboratory.
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.
• Specification of the grid system used.
• Quality and adequacy of topographic control.
• The location of the samples was
recorded with a handheld GPS.
• The grid system used is GDA94 Zone
55.
• Topographic control is not applicable
given the samples were collected
from outcrop/float.
Data
spacing
and
distribution
• Data spacing for reporting of Exploration Results.
• 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.
• Whether sample compositing has been applied.
• The samples reported in this
announcement were collected
randomly from outcrop of float from
the historical open pits.
• No composited has been applied.
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.
• 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 rockchip samples were collected
at the discretion of Dart Mining
personnel and selective in nature.
• No drilling results are reported.
Sample
security
• The measures taken to ensure sample security. • Samples were kept in the custody of
Dart Mining personnel before delivery
to a freight company to courier to the
laboratory in Townsville.
Audits or
reviews
• The results of any audits or reviews of sampling
techniques and data.
• No audits of reviews have been
completed of sampling techniques.
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Section 2 Reporting of 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 security of the tenure held at the time of
reporting along with any known impediments
to obtaining a licence to operate in the area.
• Dart holds 100% owned granted tenements at
Walwa (EL007426 – 499sq.km), Cudgewa
(EL006866 – 508sq.km) and Berringama
(EL007170 – 27sq.km)
Exploration
done by other
parties
• Acknowledgment and appraisal of exploration
by other parties.
• A review and interpreted of previous
exploration across the mineral field is
underway. This includes digitisation of
exploration data from the previous drilling,
rock chip sampling, and soil sampling
programmes observed to have been
completed. Dart Mining will announce the
results of this review and interpretation in due
course.
Geology • Deposit type, geological setting and style of
mineralisation.
• The Walwa tin field is underlain by schists,
phyllites and quartzites, with foliation and
bedding striking approximately 160° magnetic
and dipping vertical to subvertical, and with
irregularly developed jointing.
• Within this sequence, shallow‑dipping
greisenous aplite–pegmatite sills occur and
have been historically mined for tin.
• Four major sills are exposed at surface and
two additional sills were identified in earlier
exploration, with individual sills ranging from 1
to 8 metres thick, striking 042° magnetic and
109° magnetic, and dipping 20–30° to the
north or northeast, forming a broad dome
where dips become northwesterly west of the
mine.
• The sills consist predominantly of aplite with
pegmatite and greisen phases and commonly
contain coarse cassiterite along their margins.
• The tin‑bearing sills occur within a 3 km long
and 500–600 m wide north–south corridor
that hosts the historic Walwa, Mt Alwa South
and The Bounce mines.
• The Bounce lode includes a sub‑horizontal
body associated with a vertical dyke
interpreted as a feeder structure.
• Walwa represents the largest primary
hard‑rock tin production field in Victoria, with
historic mining dating back to the 1880s and
an estimated 97,000 tonnes of ore treated
during the last phase of mining in the 1970s.
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:
o easting and northing of the drill hole collar
o elevation or RL (Reduced Level –
elevation above sea level in metres) of the
drill hole collar
o dip and azimuth of the hole
o down hole length and interception depth
o hole length.
• 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
• No drillhole information is reported in this
announcement.
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Criteria JORC Code explanation Commentary
this is the case.
Data
aggregation
methods
• In reporting Exploration Results, weighting
averaging techniques, maximum and/or
minimum grade truncations (eg cutting of high
grades) and cut-off grades are usually
Material and should be stated.
• 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.
• The assumptions used for any reporting of
metal equivalent values should be clearly
stated.
• No data aggregation methods have been
applied.
Relationship
between
mineralisation
widths and
intercept
lengths
• These relationships are particularly important
in the reporting of Exploration Results.
• If the geometry of the mineralisation with
respect to the drill hole angle is known, its
nature should be reported.
• If it is not known and only the down hole
lengths are reported, there should be a clear
statement to this effect (eg ‘down hole length,
true width not known’).
• No mineralisation widths are reported.
Apparent exposed thickness estimates of the
outcrops were made and are outlined in the
announcement (visual estimates). The
thicknesses reported are apparent as the true
orientation of the outcrop is not fully known.
No depth extents (or volumes) are outlined or
inferred in this assessment.
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.
• 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.
• The samples have been disclosed as
selective rockchip sampling. Samples were
collected on the basis of identified potential
mineralisation where tin mineralisation is
interpreted.
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, groundwat
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