Narryer Project - 54 m of graphite mineralisation at Ranger
Released
Released
Announcement PDF
ASX Release
29th August 2024
Narryer Project: 54 m of graphite mineralisation at Ranger
•
NY001RC intersects 54 m of graphitic mineralisation 198 m – 252 m (eoh)
o includes 20 m > 10% visually estimated graphite from 232 m
•
Hole abandoned in high-grade graphite due to excess water
•
Assay results expected mid-October
•
>7 km trend at Oculus is now highly prospective for similar mineralisation
Buxton Resources Ltd (‘Buxton’; ASX:BUX) is pleased update shareholders in relation
to activities at the 100% owned Narryer Project, in the Murchison region of WA.
NY001RC, the maiden Buxton drill hole at the Narryer Project aimed to test a ground
EM target at the Ranger Prospect (Figure 1). Graphite mineralisation was intersected
at depth as predicted by the EM model (Figure 2).
Visual estimates by Buxton geologists indicate that NY001RC intersected continuous
graphite mineralisation from 198 metres depth to the end-of hole (Figure 3, Table
1). Continuous high-grade graphite (visually estimated > 10% TGC) was observed
from 232 metres to 252 metres depth, at which depth excessive water caused the
hole to be abandoned.
The rig has now been released, and Buxton will prioritise assaying the mineralised
interval for Total Graphitic Carbon (TGC) with results expected by mid-October.
Figure 1: Reverse Circulation drilling at the Ranger Prospect, August 2024.
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While the drilling program has downgraded the nickel potential of the Ranger target,
the thickness, apparent high-grade and visual evidence of a coarse flake component
within the graphitic interval in NY001RC provides significant encouragement for
further graphite exploration in the Project area.
Significantly, the ground EM conductors modelled at the nearby Oculus prospect are
now most likely to be related to similar graphitic mineralisation. These conductors
have been confirmed to be legitimate bedrock conductors by modelling of Buxton’s
recent ground EM survey data (see ASX Announcement 22 May 2024). The related
airborne EM conductivity trends extend over >7 linear / strike kilometres around the
Oculus Prospect (Figure 4) and define a relatively simple fold structure.
Buxton has commenced modelling “early time” ground EM data to determine the
potential for up-dip / shallower extensions to the drill-confirmed graphite
mineralisation at Ranger and the EM models at Oculus will be similarly revisited. The
current models are based solely on mid-late time EM channels (standard practice for
targeting sulphide mineralisation).
Planning works for Loupe EM and Heritage surveys at Oculus are also underway.
Buxton has successfully utilised the Loupe EM surveying method to target recent RC
drilling at Graphite Bull (see ASX Announcement 23 October 2023).
Figure 2: Narryer Project - Ranger Prospect cross section looking east-northeast. Modelling of early
time EM channels will assess potential for the graphite mineralisation to extend closer to surface than
the current model (based on late time channels) indicates.
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Figure 3: High grade graphite NY001RC at 252m depth (end of hole) – the “smear test” and “float
test” assist grade & flake size estimates during visual logging of reverse circulation samples.
Figure 4: Ranger & Oculus Prospects. HeliTEM2 AEM conductivity depth image at 100 m below
ground level. Heavy dashed line (7,260 m long) = graphite exploration target at Oculus.
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Table 1: Visual estimates of graphite mineralisation in NY001RC. True thickness is estimated to be
97.5% of the drilled interval.
Hole ID
NY001RC
Total
From
(m)
198
203
206
218
219
227
228
232
To
(m)
203
206
218
219
227
228
232
252
Interval
(m)
Estimated True
Thickness (m)
54
52.5
5
3
12
1
8
1
4
20
4.9
2.9
11.7
1.0
7.8
1.0
3.9
19.4
Visual TGC
Estimate (%)
0.5 - 5%
5 - 10%
0.5 - 5%
5 - 10%
0.5 - 5%
>10%
5 - 10%
>10%
Lithology
graphitic schist
Cautionary Statement: 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.
Table 2: Collar location details for August 2024 RC hole at the Ranger Prospect
Hole ID
Easting (m)
Northing (m)
RL (m)
Azimuth (grid)
Incl.
Total Depth (m)
NY001RC
402100
7081045
314.7
290
-75
252
---ooo--This announcement is authorised by the Board of Buxton Resources Ltd. For further
information, please contact:
Martin Moloney
Sam Wright
Chief Executive Officer
Company Secretary
marty@buxtonresources.com.au
sam@buxtonresources.com.au
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About the Narryer Project
The Narryer Project is comprised of four Exploration Licenses covering 452 km2 located within the
Narryer Terrane which forms part of the Archean Yilgarn Craton margin that hosts the recently
discovered, world-class Julimar Ni-Cu-PGE Project. This discovery by Chalice Mining Ltd and the
presence of numerous Ni-Cu-PGE occurrences along a >1,000km strike length defines the West
Yilgarn Ni-Cu-PGE Province. In addition to Ni-Cu-PGE prospectivity, Buxton has also now identified
that the Narryer Project has potential for graphite and carbonatite-related Rare Earth Element (REE)
style deposits and regolith-hosted REE within both Proterozoic and Archean successions.
During 2021 & 2022, Buxton completed ground reconnaissance, a regionally extensive 1-km spaced
ground gravity survey and a highly targeted 2566.6-line km Airborne EM survey. Interpretation of the
AEM data has identified multiple high priority anomalies, three of which warranted immediate followup by moving loop EM, which was completed at Bandito, Prodigy and Ranger Prospects in early 2023.
Additional soil sampling was conducted over AEM targets in late 2003 which provided
encouragement to extend the Ranger ground EM coverage to the nearby Oculus Prospect, which
hosts a large eye-shaped conductivity feature. The recent RC drilling at Ranger indicates that the
high-conductance ground EM target at Ranger is caused by thick graphite mineralisation with visually
estimated high-grades (>10% TGC). Future exploration will test if the extensive conductors at the
nearby Oculus Prospect are also related to similarly thick, high-grade graphite mineralisation.
Figure 5: Buxton’s Graphite Bull & Narryer Projects are located within the Gascoyne / Murchison
Region of Western Australia and are readily accessible year-round.
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Competent Persons – Narryer Project
The information in this report that relates to Exploration Results is based on information compiled by
Mr Martin Moloney, Member of the Australian Institute of Geoscientists and Society of Economic
Geologist. Mr Moloney is a full-time employee of Buxton Resources Ltd. Mr Moloney has sufficient
experience which is relevant to the activity being undertaken to qualify as a “Competent Person” as
defined in the 2012 edition of the Joint Ore Reserves Committee (JORC) Australasian Code for
Reporting of Exploration Results, Mineral Resources and Ore Reserves. Mr Moloney consent to the
inclusion in this report of the matters based on the information in the form and context in which it
appears.
The information presented herein that relates to Exploration Results from analysis of the Ground
Electromagnetic survey results is based on information compiled and reviewed by the Russell
Mortimer, a Competent Person who is a Member of The Australian Institute of Geoscientists and fairly
represents this information. Mr Mortimer has sufficient experience relevant to the style of
mineralisation and type of deposit under consideration, and to the activities undertaken, to qualify as
a Competent Person as defined in the 2012 Edition of the Joint Ore Reserves Committee (JORC)
Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves. Mr
Mortimer is an independent Consultant Geophysicist at Southern Geoscience Consultants Pty Ltd and
consents to the inclusion in the report of the matters based on his information in the form and context
in which it appears.
Previously Reported Information – Narryer Project
There is information in this announcement relating to exploration results previously announced on:
1.
2.
3.
4.
5.
6.
13th October 2022 - High priority AEM anomalies detected at Narryer Project
30th January 2023 - Exploration Update - Narryer Project
2nd August 2023 - Highly Anomalous REE in Rock Chip at Prodigy Prospect
24th August 2023 - Narryer Soil Sampling Program Complete (clarification)
22nd May 2024 - High Conductance Ground EM Plates Modelled at Ranger & Oculus Prospects
27th August 2024 - Graphite Bull & Narryer Update
Validity of Referenced Results
Buxton confirms that it is not aware of any new information or data that materially affects the
information from previous ASX announcements which has been referenced in this announcement.
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Cautionary Note Regarding Forward-Looking Information
This Announcement contains forward-looking statements and forward-looking information within the
meaning of applicable Australian securities laws, which are based on expectations, estimates and
projections as of the date of publication. This forward-looking information includes, or may be based
upon, without limitation, estimates, forecasts and statements as to management’s expectations with
respect to, among other things, the timing required to execute the Company’s programs, and the
length of time required to obtain permits, certifications and approvals.
Wherever possible, words such as “anticipate”, “believe”, “expect”, “intend”, "should", "intend",
“may” and similar expressions have been used to identify such forward-looking information. Forwardlooking information is based on the opinions and estimates of management at the date the
information is given, and on information available to management at such time. Forward-looking
information involves significant risks, uncertainties, assumptions, and other factors that could cause
actual results, performance or achievements to differ materially from the results discussed or implied
in the forward-looking information. These factors, including, but not limited to, fluctuations in
currency markets, fluctuations in commodity prices, the ability of the Company to access sufficient
capital on favourable terms or at all, changes in national and local government legislation, taxation,
controls, regulations, political or economic developments in Australia or other countries in which the
Company does business or may carry on business in the future, operational or technical difficulties in
connection with exploration or development activities, employee relations, the speculative nature of
mineral exploration and development, obtaining necessary licenses and permits, contests over title
to properties, especially title to undeveloped properties, the inherent risks involved in the exploration
and development of mineral properties, the uncertainties involved in interpreting drill results and
other geological data, environmental hazards, industrial accidents, limitations of insurance coverage
and the possibility of project cost overruns or unanticipated costs and expenses, and should be
considered carefully.
Many of these uncertainties and contingencies can affect the Company’s actual results and could
cause actual results to differ materially from those expressed or implied in any forward-looking
statements made by, or on behalf of, the Company. Prospective investors should not place undue
reliance on any forward-looking information. Although the forward-looking information contained on
in this Announcement is based upon what management believes, or believed at the time, to be
reasonable assumptions, the Company cannot assure prospective purchasers that actual results will
be consistent with such forward-looking information, as there may be other factors that cause results
not to be as anticipated, estimated or intended, and neither the Company nor any other person
assumes responsibility for the accuracy and completeness of any such forward-looking information.
The Company does not undertake, and assumes no obligation, to update or revise any such forwardlooking statements or forward-looking information contained herein to reflect new events or
circumstances, except as may be required by law. No stock exchange, regulation services provider,
securities commission or other regulatory authority has approved or disapproved the information
contained in this Announcement.
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JORC Table: 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 (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.
Reverse Circulation drilling was completed using
standard industry best practice.
Drilling techniques
Drill type (e.g., 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).
Reverse Circulation (RC) drilling was undertaken by by
Topdrill PL using a Schroamm T685 truck mounted rig
(RC).
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.
RC recoveries were considered good with available air
for drill sample recovery being deemed adequate for the
ground conditions and depth of sampling undertaken.
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.
Reverse Circulation drilling produced samples that were
collected at one-metre intervals. A one metre ‘split’
sample was collected in pre-numbered calico bags at the
time of drilling using a cone splitter integrated into the
drill cyclone to produce an approximate 1.5kg sample,
which is considered representative of the full drill metre.
The residual material from each metre interval was
collected in 600mm x 900mm biodegradable bags
preserved at the drill sites whilst laboratory analysis is
ongoing.
Drill samples selected for analysis were limited to those
containing visible graphite (using the one metre split
samples) alongside composites containing either a two,
three or four-metre buffer either side of the visible
intervals.
Analyses will be undertaken by ALS Geochemistry in
Perth and include Total Graphitic Carbon with other
parameters as necessary.
Appropriate measures have been undertaken to
maximise sample recovery and ensure the
representative nature of samples, including:
-
Terminating RC holes when recovery amounts
are reduced at depth
Terminating RC holes when excess water is
encountered
No apparent relationship has been defined between
sample recovery and grade based on the various drilling
programs to date at Graphite Bull.
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.
Chip trays were collected from each one metre interval
this was used to log lithology, oxidation and visual
graphite content estimate a streak test was used to
assist with visual estimates alongside historical samples.
Visual estimates for TGC were based on comparison with
historic samples from Buxton’s Graphite Bull Project,
YBRC0018 and YBRC0019 which constituted 276 metres
of previously assayed material with grades from 0.1% to
30.9% TGC. This included 52 samples greater than 10%
TGC. 19 samples from 5-10% and 87 samples from 0-5%.
Samples were noted if they were wet or where recovery
was significantly impacted.
Photographs of all RC chip trays will be taken at BUX’s
core processing facility at the Project, and in Perth and
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retained on file with the original chip trays stored at
BUX’s storage facility in Peth.
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.
Logging is considered to be semi-quantitative.
All RC one-metre sub-samples from drill holes were
collected from a cone splitter respectively, to produce an
~15% routine split sample for analysis.
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.
Quality of assay data
and laboratory tests
Verification of
sampling and
assaying
The nature, quality and appropriateness of the assaying
and laboratory procedures used and whether the
technique is considered partial or total.
Not applicable, the release does not include laboratory
assay results.
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.
See ASX announcement 13th October 2022 for details
relating to the airborne EM and ASX announcement 22nd
May 2024 for details relating to the ground Moving Loop
EM.
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.
In addition to duplicate samples (detailed above),
Quality Control and Quality Assurance (QA/QC)
procedures included insertion of standards (three
different standards each certified for TGC at three
different abundance levels appropriate for the expected
abundances of mineralisation intersected in the drill
program) and blanks which were inserted every 20
samples.
The verification of significant intersections by either
independent or alternative company personnel.
Senior company geological personnel onsite for the
entirety of the drilling and logging process.
The release does not include data from other
geophysical or handheld XRF tools.
Once the core is processed at BUX’s core processing
facility in Perth. The logging will be validated by a BUX
on-site geologist and compiled onto the BUX MX Deposit
drill hole database
Assay data will be imported directly from digital assay
files from contract analytical company ALS (Perth) and
merged in the Company MX Deposit drill hole database.
Data is backed up regularly in off-site secure servers.
The use of twinned holes.
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No new geophysical results are used in exploration
results reported.
No historic holes were twinned as part of this program.
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Documentation of primary data, data entry procedures,
data verification, data storage (physical and electronic)
protocols.
Discuss any adjustment to assay data.
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.
Data spacing and
distribution
Data spacing for reporting of Exploration Results.
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 measures taken to ensure sample security.
Sample security
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.
Logging and sampling were recorded directly into a
digital database.
Not applicable, the release does not include laboratory
assay results.
The surface hole collar location was surveyed using a
handheld Garmin GPS unit with an expected accuracy of
±6m for easting and northing with elevation also
recorded.
Drill path gyroscopic surveys were at 0m and at
subsequent 30m downhole intervals to final hole depth
using an Axis Gyro tool.
All surface surveying was completed using a handheld
GPS to MGA94 / Zone 50 South grid system.
Topographic control was provided by a Digital Elevation
Model (DEM) derived from the SRTM dataset which
provided a DEM with a +/- 3.5m vertical accuracy
(Elsonbaty et al 2023).
This is deemed adequate for first-pass exploration
drilling, particularly given that topographic relief is
extremely low.
See drill tables for drill hole location.
Only a single hole has been drilled at the Ranger
prospect, and so this spacing and distribution is not
considered suitable for mineral resource estimation.
The orientation of the drilling is not expected to
introduce sampling bias. All drill holes have intersected
the mineralisation at a sufficient angle to the strike and
dip of the mineralised units.
The chain-of-sample custody is managed by the BUX
staff from collection at the rig to the submission of the
samples to ALS Limited – Perth for analysis.
Samples are being stored at the drillsite before being
transported and processed at BUX’s secure sample
processing and storage facility in Perth.
The diamond drill core will be wet cut using a diamond
blade and sampled at BUX’s core processing facility in
Perth by BUX staff and contractors.
Diamond drill core samples will be placed in prenumbered calico bags and further secured in green
plastic sample bags with cable ties. The samples are
further secured in a bulk bag and delivered to the ALS Perth by contractor freight service.
Sample reconciliation advice is sent by ALS-Perth to
BUX’s Geological Database Administrator on receipt of
the samples.
Any inconsistences between the despatch paperwork
and samples received is resolved with BUX before
sample preparation commences.
Sample preparation and analysis is completed at one of
the ALS laboratories in Perth.
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Audits or reviews
The results of any audits or reviews of sampling
techniques and data.
The risk of deliberate or accidental loss or contamination
of samples is considered very low.
Sampling procedures are identical to those followed by
Buxton in 2013/14 which have previously been reviewed
and found to be adequate by an independent resource
geologist.
JORC Table: 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.
BUX have a 100% interest in exploration license
E09/2027, E09/2028, E09/2029 and E09/2722 which
cover 452 km2.
No royalties encumber these tenements.
Native Title is held by the Wajarri Yamatji native title
determination and claim covers approximately 100,701
square kilometres of land in the Yamatji region. Horizon
Heritage Management (Horizon Heritage) was engaged
by Heritage Link to facilitate and undertake an AHA Work
Program Clearance Aboriginal heritage survey with
Wajarri Yamatji (Simpson) Traditional Owners for the
Narryer – Ranger Prospect survey area. A review of the
Department of Planning, Lands and Heritage (DPLH)
online ACHIS identified no Aboriginal sites or places
within the Narryer – Ranger Prospect survey area.
Exploration done by
other parties
Geology
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.
Acknowledgment and appraisal of exploration by other
parties.
Deposit type, geological setting and style of
mineralisation.
The eastern portion of the Narryer Project lies within the
Radio Quiet Zone of the Inyarrimanha Ilgari Bundara, the
CSIRO Murchison Radio-astronomy Observatory. The
RQZ does not cover the Ranger or Oculus Prospects.
The tenement is in good standing with DMIRS and there
are no known impediments for exploration on this
tenement.
Numerous exploration parties have held portions of the
area covered by BUX tenure previously. No substantive
historical exploration for graphite has been undertaken.
No other parties were involved in the exploration
program that generated data that was used in this
release.
The Narryer Project area is located on the north western
margin of the Yilgarn Craton.
The surface geology of the Narryer Project is dominated
by tertiary lateritic weathering profiles and TertiaryQuaternary drainage basin sediments that largely
obscure the basement geology.
Basement geology consists of Archean rocks of the
Narryer Gneiss Terrane and, in the far northwest, the late
Mesoproterozoic - Neoproterozoic Badgeradda Group.
These two distinct geological terranes are juxtaposed
along the Meeberie fault.
The Narryer Gneiss Terrane is composed of a tectonically
interleaved and poly deformed mixture of granite, mafic
intrusions and metasedimentary rocks in excess of 3.3
billion years old, with the majority in excess of 3.6 billion
years old.
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The rocks have experienced multiple metamorphic
events at amphibolite or granulite conditions, resulting in
often complete destruction of original igneous or
sedimentary (protolith) textures.
The Narryer Gneiss Terrane is divided into four major
rock sequences (Myers 1990); the Dugel Gneiss,
Meeberrie Gneiss, Manfred Complex, and unassigned
polydeformed leucocratic gneisses and metasediments.
Graphite mineralisation is hosted by quartz-felspathic
and hornblende gneisses and chloritic schists that are
most likely from the Mount Narryer gneissic complex.
The hornblende gneiss gradually included slivers of
graphite which in turn became massive.
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
See the body of the release for drillhole data as compiled
by Buxton.
o elevation or RL (Reduced Level –
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