Significant Exploration Programs Underway at Bauloora
Released
Released
Announcement PDF
ASX ANNOUNCEMENT
1 February 2024
Significant Exploration Programs Underway at Bauloora
Foundational geochemical and geophysical surveys underway
Audio Frequency Magnetotelluric Survey
Large scale audio frequency magnetotelluric (AMT) survey underway for 83 line-km’s across
10km2 of the Primary Bauloora Epithermal Vein Field (Primary Vein Field).
Ground Gravity Survey
•
• Significant ground gravity survey is underway of 100m x 100m spaced stations over 10km2.
Geochemical Surveys
Tenement wide Bulk Leached Extractable Gold (BLEG) stream sediment sampling underway
across 330km2.
Geological Mapping
•
•
Detailed geological mapping underway across 10km2 of the Primary Vein Field.
Follows on from substantial activities completed in 2023
Diamond drilling at the Breccia Sinter Prospect
•
1,792.7m completed to date with assay results pending.
The drilling successfully intercepted the target zone with mineralogy and low sulphidation
epithermal quartz vein textures in the drill core consistent with the upper “boiling zone”.
Tenement-wide Airborne Aeromagnetic and Radiometric survey
•
• 7,000 line-km survey completed across 330km2 at 50m line-spacing.
Additional Epithermal Pathfinder Element analysis underway
•
Assay results are pending from the Laboratory for 3,004 soil samples.
Strong platform for drill targeting in 2024
•
The completion of these exploration activities will provide a world-class dataset which the
Company intends to use to drill test epithermal gold mineralisation targets in 2024.
Figure 1: Drill hole BX003 drill testing beneath sinter outcrop and anomalous soil samples.
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Legacy Minerals Holdings Limited (ASX: LGM, “Legacy Minerals” or “the Company”) is pleased to
announce the exploration results and upcoming programs of work the Bauloora Project (EL8995 and
EL9464) in the Lachlan Fold Belt, NSW.
Management comment - Legacy Minerals CEO & Managing Director, Christopher Byrne said:
“After the completion of diamond drilling at the Breccia Sinter in December 2023, we are
recommencing our systematic exploration programs at Bauloora with purpose.
This multi-faceted geochemical, geophysical, and geological data acquisition will further enhance the
outstanding geological information that we have collected at the Bauloora Project. This detailed
dataset will be worldclass and is important in defining major epithermal Au targets to be drilled under
our JV partnership with Newmont.
With the upcoming news including the release of assays from the diamond drilling campaigns at the
Breccia Sinter Prospect and at diamond drilling at Fontenoy, the Company also intends to provide
updates soon on its Black Range Project, including planned drilling and results of ASTER analysis
completed last year.”
Audio Frequency Magnetotellurics
The Company is completing the second phase of the large-scale, 80 line-km AMT survey over the
Bauloora Vein Field. Geophysical contractors Quantec and AGS are now onsite completing this work.
The survey will cover approximately 10km2 at 200m spaced lines with the objective of to identify and
target large strike extensive resistivity anomalies that may represent zones of silicification associated
with epithermal veining. It is expected that the survey will provide quality resistivity datasets to depths
greater than 1,000m.
MT surveys such as AMT have proven success globally in the delineation of subsurface zones of
silicification manifest as zones of elevated resistivity, even beneath areas of high-level silica which can
be expected in the upper portions of a completely preserved low sulphidation epithermal system such
as that interpreted at Bauloora.
Figure 2: AGS and Quantec AMT field crew setting up a survey station on the Bauloora Project.
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The AMT survey will expand upon the knowledge gained from the Company’s Gradient Array Induced
Polarisation survey 1,i which demonstrated that linear resistive trends at Bauloora are commonly
associated with mapped quartz veins and silicic alteration on surface. The AMT survey will provide a
depth and dip parameter to previously identified resistive trends and add further clarity to these and
mapped zones of silicification.
Figure 3: Planned and completed AMT survey area of mapped vein field ii
1
See ‘Endnotes’ on Page 19 for references.
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The survey is being completed in two phases. The first phase completed over the Breccia Sinter
Prospect to assist with the interpretation of results from returned from drilling completed last year
that resulted in the discovery of new epithermal veins. The second phase covers the broader Bauloora
vein field and includes the Mee Mar Prospect vein trend where wide and strike extensive epithermal
veins were intercepted in diamond drilling early last year, and a new discovery at the Bluecap Prospect
which returned 13m at 1.66g/t Au, 6.68g/t Ag, 0.14% Cu and 4.23% Pb+Zn incl. 6m at 3.56g/t Au,
10.95g/t Ag, 0.22% Cu and 6.47% Pb+Znvi.
About AMT
AMT is a passive geophysical method which uses natural time variations of the earth's magnetic and
electric fields to measure the electrical resistivity of the sub-surface rocks. Electrical resistivity of
rocks and minerals is an important physical property to measure as part of attempts to understand
geological structure, alteration, veining and lithology. It varies by many orders of magnitude which
allows for the differentiation of very resistive zones of silicification and quartz veins development
rom more conductive sedimentary rocks or saline clay gouge faults. The resistivity data collected
from the audio magnetotelluric survey, is the manifestation of the bulk property of a volume of
earth material and is associated with factors such as rock composition, porosity and permeability as
well as rock fluid composition and temperature.
- Extract from Geoscience Australia, Australian Commonwealth Governmentiv
Aero-magnetic and Radiometric Survey
The Company has completed a tenement-wide (EL8994 and EL9464) fixed-wing magnetic and
radiometric survey. Flight lines were flown at 50m line spacing at a height of ~60m and provided high
quality magnetic and radiometric survey data across the Project. This has greatly improved upon the
previously available low resolution 200m and 250m line spaced surveys over the tenements.
These datasets are currently under review with interpretations being developed as new information
from ongoing field mapping is returned. Initial observations show several previously unrecognised
magnetic features interpreted to be I-type intrusions and felsic to intermediate dykes. Furthermore
clear structural features are highlighted over the known vein field and across the tenement with
interpretations being undertaken. Several zones which exhibit low magnetic intensity have been
identified and may be the result of demagnetisation due to magnetite-destructive alteration of the
host volcanic rocks. These features and others will be visited during field mapping and reconnaissance.
Encouragingly elevated K:Th, which may represent illite-adularia alteration, has highlighted areas of
known low-sulphidation epithermal vein mineralisation and identified large areas to be explored for
epithermal Au-Ag mineralisation across the Project.
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Figure 4: Aero-magnetic survey across the Bauloora Project showing magnetic RTP image (50m spaced lines).
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Ground Gravity
The Company is completing an initial, ground gravity survey over the Primary Vein Field area. The
survey will cover approximately 10km2 and will be surveyed at 100m x 100m spaced stations for a total
of approximately 1,550 stations. Geophysical contractors Fender Geophysics have now been engaged
to complete this work. The objective of the survey is to help detect the location and orientation of
potential growth faults buried beneath the surface lithologies, including the strike extension of the
Deep Gully Creek conglomerate unit. Conglomerate basin fill, developed in half-graben basins, occurs
associated with growth faults proximal to large globally recognised low-sulphidation epithermal
gold-silver deposits. The gravity survey, in conjunction with ongoing geological mapping, will increase
the understanding of the litho-structural controls to mineralisation in the Project and provide
potential vectors towards additional low-sulphidation epithermal gold-silver mineralisation.
Figure 5. Fender Geophysics field crew setting up a survey station on the Bauloora Project.
BLEG stream sediment
The known low sulphidation epithermal vein field is only a small portion of the 330km2 Bauloora
Project. The Company is commencing a project wide BLEG stream sediment sampling survey which is
a proven method of screening large areas for any hydrothermal systems that may be exposed on the
surface. There are several known regional mineral occurrences within the Bauloora Project that are
present and Global Ore Discovery’s review of the ASTER data delineated instances of advanced argillic
alteration including alunite elsewhere on the Project that may represent alteration related to
epithermal systems.
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Principal terms of the joint venture with Newmont
Phase 1 - $5M earn-in for 51%
• Subject to satisfying the minimum commitments, Newmont may acquire a 51% farm-in
interest in the Bauloora tenements by spending a total of A$5 million within 48 months.
• Undertaking 4,000m of drilling within 48 months.
• Legacy Minerals will act as operator during the initial earn in period.
Phase 2 - $10M earn-in for 75%
• Subject to completion of Phase 1, Newmont may earn a further 24% farm-in interest in the
tenements by spending an additional A$10 million.
• Undertaking a further 8,000m of drilling within 48 months.
Newmont financing facility and Mining Joint Venture
• A Mining Joint Venture may be formed between the Company’s upon the decision to mine.
• At the discretion of Legacy Minerals, LGM may enter an agreement to be loan carried
through to production through a Newmont financing facility, allowing Newmont to earn-in
up to 80%.
• The loan would be re-paid from Legacy Minerals’ 20% share of any future mining proceeds.
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About the Bauloora Project
Legacy Minerals’ Bauloora Project is located in the Lachlan Fold Belt of New South Wales which is host
to world-class copper-gold orebodies including the Cadia-Ridgeway, Northparkes, and Cowal mines.
In 2023, Newmont Exploration Pty Ltd entered into a Farm-In and Joint Venture on the Project iii. It
covers a large hydrothermal alteration zone 27km2 in size, within which is an anomalous gold zone
currently mapped to 15km2. Rock chip and soil samples collected by the Company from the Project
area have highlighted several priority areas of anomalous precious metal values with highly
anomalous values of epithermal pathfinders iv. The drilling of the first of these targets resulted in the
discovery of the Bluecap Prospect returning 13m at 1.66g/t Au, 6.68g/t Ag, 0.14% Cu and 4.23% Pb+Zn
from 57miv.
Extensive epithermal alteration exists on the Project, including widespread zones of high-level
chalcedonic veins, clay alteration and local sinter formations. The Project has seen very limited
exploration drilling, and the Company believes the results from work to date strongly support the
assessment that there is significant potential for the discovery of a major low-sulphidation epithermalstyle gold-silver deposit at the Bauloora Project.
Figure 6: Regional setting of the Bauloora Project v,vi,vii,viii,ix
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Approved by the Board of Legacy Minerals Holdings Limited.
For more information:
Investors:
Chris Byrne
CEO & Managing Director
chris.byrne@legacyminerals.com.au
+61 (0) 499 527 547
Media:
Nicholas Read / Kate Bell
Read Corporate
info@readcorporate.com.au
+ 61 (0) 419 929 046
DISCLAIMER AND PREVIOUSLY REPORTED INFORMATION
Information in this announcement is extracted from reports lodged as market announcements referred to above
and available on the Company’s website https://legacyminerals.com.au/. The Company confirms that it is not
aware of any new information that materially affects the information included in the original market
announcement and that all material assumptions and technical parameters underpinning the estimates in the
relevant market announcement continue to apply and have not materially changed.
This announcement contains certain forward-looking statements. Forward looking statements are only
predictions and are subject to risks, uncertainties and assumptions which are outside of the control of Legacy
Minerals Holdings Limited (LGM). These risks, uncertainties and assumptions include commodity prices,
currency fluctuations, economic and financial market conditions, environmental risks and legislative, fiscal or
regulatory developments, political risks, project delay, approvals and cost estimates. Actual values, results or
events may be materially different to those contained in this announcement. Given these uncertainties, readers
are cautioned not to place reliance on forward-looking statements. Any forward-looking statements in this
announcement reflect the views of LGM only at the date of this announcement. Subject to any continuing
obligations under applicable laws and ASX Listing Rules, LGM does not undertake any obligation to update or
revise any information or any of the forward-looking statements in this announcement to reflect changes in
events, conditions or circumstances on which any forward-looking statements is based.
COMPETENT PERSON’S STATEMENT
The information in this Report that relates to Exploration Targets, Exploration Results, Mineral Resources or Ore
Reserves is based on information compiled by Thomas Wall, a Competent Person who is a Member of the
Australian Institute of Geoscientists. Mr Wall is the Technical Director and a full-time employee of Legacy
Minerals Pty Limited, the Company’s wholly-owned subsidiary, and a shareholder of the Company. Mr Wall has
sufficient experience that is relevant to the style of mineralisation and type of deposit 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 Wall consents
to the inclusion of the matters based on this information in the form and context in which it appears in this
announcement.
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About Legacy Minerals
Legacy Minerals is an ASX listed public company that has been involved in the acquisition and
exploration of gold, copper, and base-metal projects in the Lachlan Fold Belt since 2017. The Company
has eight projects that present significant discovery opportunities for shareholders.
Au-Cu (Pb-Zn) Cobar (EL9511)
Au Harden (EL9257, ELA6694)
Undrilled targets next door to the Peak Gold Mines.
Several priority geophysical anomalies and gold in
lag up to 1.55g/t Au.
Large historical high-grade quartz-vein gold
mineralisation. Drilling includes 3.6m at 21.7g/t Au
116m and 2m at 17.17g/t Au from 111m.
Au-Ag Bauloora (EL8994, EL9464) Newmont JV
Au-Cu Fontenoy (EL8995) Earth AI Alliance
One of NSW’s largest low-sulphidation, epithermal
systems with a 27km2 epithermal vein field.
An 8km long zone of Au and Cu anomalism defined
in soil sampling and drilling. Significant drill
intercepts include 79m at 0.27% Cu from 1.5m.
Cu-Au Rockley (EL8296)
Au-Ag Black Range (EL9466, EL9589)
Prospective for porphyry Cu-Au and situated in the
Macquarie Arc Ordovician host rocks with historic
high-grade copper mines that graded up to 23% Cu.
Extensive low-sulphidation, epithermal system with
limited historical exploration. Epithermal
occurrences across 30km of strike.
Cu-Au Glenlogan (EL9614) S2 Resources JV
Cu-Au Drake (EL6273, EL9616)
Large, undrilled magnetic anomaly underneath
Silurian cover located 55kms from Cadia Valley.
Large caldera (~150km2) with similar geological
characteristics to other major pacific rim deposits.
Figure 7: Regional setting of Legacy Minerals Projects vi,vii,viii,ix,x
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Appendix 1 – JORC Code, 2021 Edition Table 1
Section 1 Sampling Techniques and Data
Criteria
JORC Code Explanation
Nature and quality of sampling (e.g., cut channels,
random chips, or specific specialised industry
standard measurement tools appropriate to the
minerals under investigation, such as down hole
gamma sondes, or handheld XRF instruments, etc).
These examples should not be taken as limiting the
broad meaning of sampling.
Sampling
Techniques
Drilling
techniques
Drill sample
recovery
Commentary
No assays are being reported in this release.
References in this announcement to visual
results are from HQ3/NQ diamond drill core.
Mineralised sections in drill core will be cut,
and half-core sampled for assaying. Assay
results are expected in February 2024.
Include reference to measures taken to ensure
sample representivity and the appropriate
calibration of any measurement tools or systems
used.
No sampling completed.
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 1m 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.
No assays are being reported in this release.
Drill type (e.g., core, reverse circulation, open‐hole
hammer, rotary air blast, auger, Bangka, sonic, etc)
and details (e.g. core diametre, 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).
Diamond drilling is completed using HQ3 drill
core. Core orientation completed using a
REFLEX tool.
Method of recording and assessing core and chip
sample recoveries and results assessed.
Core recovery is captured in the core logging.
No assays are being reported in this release.
Measures taken to maximise sample recovery and
ensure representative nature of the samples.
No assays are being reported in this release.
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.
To date, minimal sample recovery issues have
been identified that would impact on
potential sample bias in the competent fresh
rocks that host the mineralised sulphide
intervals.
Systematic geological and geotechnical
logging was undertaken. Data collection
where appropriate includes:
• Nature and extent of lithologies.
• Relationship between lithologies.
• Amount and mode of occurrence of ore
minerals.
• Location, extent and nature of structures
such as bedding, cleavage, veins, faults etc.
Structural data (alpha & beta) are recorded
for orientated core.
• Geotechnical data is collected as required
such as recovery, RQD, fracture frequency,
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qualitative IRS, microfractures, veinlets and
number of defect sets. For some geotechnical
holes the orientation, nature of defects and
defect fill may be recorded.
• Bulk density by Archimedes principle at
regular intervals may be taken.
• Magnetic susceptibility recorded at 1m
intervals for some holes as an orientation and
alteration characterisation tool.
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.
Logging
Sub‐sampling
techniques and
sample
preparation
Whether logging is qualitative or quantitative in
nature. Core (or costean, channel, etc)
photography.
Logging of records lithology, mineralogy,
mineralisation, structures, weathering, colour
and other noticeable features. This is
generally qualitative except for % of sulphides
and vein mineral content. Core trays are
photographed in wet form.
The total length and percentage of the relevant
intersections logged.
All drill holes are geologically logged in full.
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.
No assays are being reported in this release.
For all sample types, the nature, quality and
appropriateness of the sample preparation
technique.
No sampling completed.
Quality control procedures adopted for all
subsampling 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.
Quality of
assay data and
laboratory
tests
Geological logging is carried out on all drill
hole chips with lithology, alteration,
mineralisation, structure and veining recorded
where possible.
No assays are being reported in this release.
No sampling completed.
No sampling completed.
Whether sample sizes are appropriate to the grain
size of the material being sampled.
No sampling completed.
The nature, quality and appropriateness of the
assaying and laboratory procedures used and
whether the technique is considered partial or total.
No assays are being reported in this release.
For geophysical tools, spectrometres, handheld XRF
instruments, etc, the parametres used in
determining the analysis including instrument make
and model, reading times, calibrations factors
applied and their derivation, etc.
No assays are being reported in this release.
Nature of quality control procedures adopted (e.g.
standards, blanks, duplicates, external laboratory
checks) and whether acceptable levels of accuracy
(i.e. lack of bias) and precision have been
established.
No assays are being reported in this release.
The verification of significant intersections by either
independent or alternative company personnel.
No assays are being reported in this release.
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Verification of
sampling and
assaying
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.
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 for reporting of Exploration Results.
Data spacing
and
distribution
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.
Whether sample compositing 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.
No twinned holes have been planned for the
current drill programme.
Primary data is captured onto a laptop
through excel and using Datashed software
and includes geological logging, sample data
and QA/QC information. This data, together
with the assay data, is stored both locally and
entered into the LGM central online database.
No adjustments or calibrations will be made
to any primary assay data collected for the
purpose of reporting assay grades and
mineralised intervals. For the geological
analysis, standards and recognised factors
may be used to calculate the oxide form
assayed elements, or to calculate volatile free
mineral levels in rocks.
A handheld Garmin GPSmap 65 was used to
pick up collars with an averaged accuracy of
1m.
Downhole surveys are conducted using a
downhole Gyro during drilling to record and
monitor deviations of the hole from the
planned dip and azimuth.
The grid system used is GDA94, MGA Zone 55.
Using government data topography and 2017
DTM data. A topographic surface has been
created using this elevation data.
The spacing and distribution of holes is not
relevant to the drilling programs which are at
the exploration stage rather than definition
drilling. Drill holes were preferentially located
at those areas considered most prospective.
No sampling completed.
No compositing has been applied to the
exploration results.
The drill holes are orientated to intersect the
dipping mineralised trends at as near
perpendicular orientation possible (unless
otherwise stated).
The orientation of key structures may be
locally variable and any relationship to
mineralisation has yet to be identified.
The orientation of drilling relative to key
mineralised structures is not considered likely
to introduce sampling bias.
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.
Orientation of the mineralisation and
structural trends is constrained by previous
drilling and outcrop.
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The orientation of sampling is considered
appropriate for the current geological
interpretation of the mineral style.
No sample bias due to drilling orientation is
known.
Sample
security
The measures taken to ensure sample security.
Audits or
reviews
The results of any audits or reviews of sampling
techniques and data.
Chain of Custody is managed by the Company
until samples pass to a certified assay
laboratory for subsampling and assaying. The
core trays are stored on secure sites and
delivered to the assay laboratory by the
Company or a competent agent. When not in
transit, they are kept in locked premises.
Where appropriate transport logs have been
set up to track the progress of samples.
Sampling techniques and procedures are
regularly reviewed internally, as is data. To
date, no audits of sampling techniques and
data have been completed on the drilling
programme.
Section 2 Reporting of Exploration Results
(Criteria in this section apply to all succeeding section)
Criteria
JORC Code Explanation
Commentary
Mineral
Tenement and
Land Status
Type, name/reference number, location and
ownership including agreements or
material issues with third parties including
joint ventures, partnerships, overriding
royalties, native title interests, historical
sites, wilderness or national park and
environmental settings.
The Bauloora Project is comprised of EL8994 and
EL9464. The license is owned 100% by Legacy
Minerals Pty Ltd (a fully owned subsidiary of Legacy
Minerals Holdings Limited). There are no royalties or
encumbrances over the tenement areas.
The security of the tenure held at the time
of reporting along with any known
impediments to obtaining a licence to
operate in the area.
The land is primarily freehold land. There are no
native title interests in the license area.
Exploration
Done by Other
Parties
Acknowledgment and appraisal of
exploration by other parties.
Geology
Deposit type, geological setting and style of
mineralisation
Drill hole
Information
A summary of all information material to
the understanding of the exploration results
including tabulation of the following
information for all Material drill holes:
Teck Exploration - conducted mapping, IP geophysics,
rock chip sampling, diamond and RC drilling. BP
Minerals/MM&S - conducted detailed mapping,
geochemical sampling and AC drilling. Billiton
Australia - conducted mapping, IP geophysics, rock
chip sampling. North Limited – rock chip sampling,
soil sampling, drilled AC and RC holes. Robust
Resources – soil sampling diamond and RC drilling.
Bushman Resources – Rock chip sampling.
Known mineralisation at the Bauloora Project sits
within the Silurian Frampton Volcanics, and
Devonian Bethungra Formation, Cowcumbala
Rhyolite and Deep Gully Creek Conglomerate. The
Project is considered prospective for lowsulphidation epithermal style gold-silver and basemetal mineralisation.
See Table 1 in the body of the article.
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• Easting and northing of the drill hole
collar
•Elevation or RL (Reduced Level – elevation
above sea level in metres) of the drill hole
collar
• Dip and azimuth of the hole
• Down hole length and interception depth
• 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 this is the case.
In reporting Exploration Results, weighting
averaging techniques, maximum and/or
minimum grade truncations (e.g. cutting of
high grades) and cut‐off grades are usually
Material and should be stated.
Data
aggregation
methods
Where aggregated intercepts incorporate
short lengt
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