Exploration Update - Central Yilgarn and Laverton Projects
Released
Released
Announcement PDF
ASX Announcement
25 June 2025
Exploration Update of the Central
Yilgarn and Laverton Projects
Highlights
• Within the Central Yilgarn Project an initial RC drilling program is planned to
commence in 2H 2025.
• Seven exciting walk up drill targets have shown proven mineralisation containing
several high-grade intercepts not followed up.
• Several robust, high tenor gold in soil anomalies can be enhanced with additional
sampling.
• At Laverton, a significant zone of gold mineralisation was identified from aircore
drilling along the interpreted position of the regionally significant and mineralised
Barnicoat Shear Zone.
• Also, at Laverton a high-grade REE intersection is particularly significant with a 4m
zone over 10,000ppm TREO (1%).
Catalina Resources Ltd (ASX: CTN) (‘Catalina’ or the ‘Company’) acquired the Yerilgee and Evanston greenstone belts in
January 2025 from the wholly owned subsidiary of Dreadnought Resources Limited (DRE), Dreadnought Exploration Pty
Ltd (“Dreadnought”)1. These Projects (Figure 1) are located within an underexplored region of the world-renowned Yilgarn
Craton, approximately 190 km to the northwest of Kalgoorlie and 160 kms southwest of Leonora. The project area covers
an area of over 650 km2, and over approximately 65 km of strike, along the Yerilgee and Evanston greenstone belts.
The tenements present a rare exploration play over multiple greenstone belts with proven mineralisation potential for
gold, iron ore, lithium, nickel and Cu-Zn-Ag massive sulphides. With several high-grade gold targets identified and
minimal follow-up to date, the exploration potential is considered by CTN to be significant.
Following a technical review of the voluminous database drill targets have been generated in the Yerilgee and Evanston
greenstone belts with an RC drill program planned to commence in 2H, 2025.
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Figure 1 – Regional locations of the Yerilgee and Evanston Projects
Yerilgee Project
The exposed Yerilgee Greenstone Belt, which has been subjected to multistage deformation and shearing, is composed
of typical greenstone lithologies comprising basalts, ultramafic volcanics, sediments, banded iron formations and
granites. It hosts three primary camp-scale gold targets: T6, T8, and T11, illustrated in Figure 2.
T6 Gold Camp (Figure 2). Defined by anomalous gold and pathfinder soil geochemical anomalies over an area of 5,000m
x 3,000m, illustrated in Figure 3. Within the T6 Gold camp, Chicken Little is a ~1,500m x ~300m Au-As-Sb-Pb-Zn-Ag soil
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anomaly along an intrusive contact of BIFs-ultramafic and lamprophyre intrusions into a sediment package with felsic
porphyries. Multi-element geochemistry at T6 suggests a fractionated intrusion-related hydrothermal system with the
pathfinder geochemical gradient transitioning from Mo-W, associated with a major felsic intrusion, to Bi-Te and As-Sb.
Figure 2 – Regional geological interpretation of the Yerilgee Greenstone Belt. It hosts three primary
camp-scale gold targets: T6, T8, and T11. The T6 Gold Camp contains the Chicken Little, Snowflake
and Megatron drill targets
In 2018, gold was identified at surface by DRE during soil sampling and subsequent drilling produced significant gold
intercepts at Chicken Little including:
•
•
BARAC0477: 24m @ 1.6 g/t Au from 0m and 9m @ 3.3g/t Au from 12m ².
BARRC025: 45m @ 0.4g/t Au from 6m, including 8m @ 0.9 g/t Au and 52.8 g/t Ag from 10m ².
In 2024 follow up drilling by DRE (2 RC holes, 270m) intersected a ~40m wide strongly sulphidised and variably oxidized
banded iron formation (“BIF”) horizon with an internal felsic schist that is interpreted to be either highly altered
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sedimentary rock or a small felsic porphyry. This horizon appears to be a key structural component to the mineralisation
at Chicken Little (see Figure 4). In addition, variable weak to moderate quartz veining with associated sulphides was
observed. Both holes intersected significant Au-Ag mineralisation including:
• CYRC012: 17m @ 4.1 g/t Au and 28.0 g/t Ag from 53m, including: 4m @ 14.9 g/t Au and 72.2 g/t Ag from 54m ³.
• CYRC013: 7m @ 0.2 g/t Au, 56 g/t Ag from 82m ³.
RC drilling at Chicken Little will focus upon the down dip and potential plunge of the identified mineralisation.
Figure 3 – T6 Gold Camp: Prospects are defined by very anomalous gold and pathfinder soil geochemistry
Also, within the T6 prospect, are the Snowflake and Megatron targets, illustrated in Figure 2. Both have clearly defined
robust anomalous gold in soil geochemistry, illustrated in Figure 3.
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Megatron is identified by an intense ~600m x 400m gold in soil anomaly associated with major cross cutting structures
and multiple phases of felsic and mafic intrusions. Gold mineralisation appears to be associated with a strong carbonate
and sulphide altered felsic porphyry. RC drilling by DRE in 2024 reported
•
•
9m @ 2.6 g/t Au from 23m, including 3m @ 7.1 g/t Au ⁴.
11m @ 0.34 g/t Au from 21m, including 3m @ 1.2 g/t Au⁴.
Figure 4 – Drilling section for RC hole CYRC012 at Chicken Little North
Snowflake was identified by a ~800m x 200m gold and bismuth in soil anomaly associated with a secondary N-S trending
structure, a significant 180m long quartz blow and felsic intrusions. High grade gold mineralisation from aircore drilling
in 2024 (16m @ 1.9 g/t Au from 0m, including 4m @ 8.5 g/t Au from STKAC0118) was hosted within a near surface 1-2m
quartz vein within an intensely sericite carbonate altered felsic porphyry ⁴.
These results are highly encouraging and will result in a strong focus on the T6 Gold camp.
T8 Gold Camp: The T8 Gold Camp (located in Figure 2) is focussed upon a significant domal structure clearly indicated
in magnetic and gravity geophysics. (see Figure 9). It was defined by a 1.7km x 400m gold-in-soil anomaly associated
with As-Sb-Bi-Mo-W pathfinders. Drilling in 2018 identified an anticlinal closure of a banded iron formation (BIF) which
had been replaced by pyrite, arsenopyrite and quartz in three holes, and had been intruded by a felsic porphyry along a
major regional lineament. RC drilling by DRE returned significantly wide intercepts including:
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•
•
17m @ 0.7 g/t Au from 22m, including 8m @ 1.2 g/t Au from 27m and 14m @ 0.3 g/t Au from 60m in BARRC015
².
10m @ 0.8 g/t Au, including 1m @ 6 g/t Au, from 11m and 27m @ 0.4 g/t Au from 40m in BARRC014 ².
A supergene gold blanket present in holes BARAC012, BARAC013, BARAC014, averaging 0.5g/t Au, overlies the target
zone illustrated in Figure 5.
Figure 5. T8 Gold Prospect drill section
Evanston Project
The northeasterly trending Evanston Greenstone Belt (see Figure 1 for location), is a strongly faulted and deformed belt,
contained within the Evanston Shear Zone. Quartz veins are common and intrude all exposed rock types. Large quartz
veins, up to 40 m thick, are parallel to the regional fabric of the shear zone and traceable over several hundred metres.
Lithologies include basalts, ultramafics, banded iron formation, sediments and felsic intrusions.
The Evanston Greenstone Belt currently contains two main camp-scale gold targets: T1 and T2, (see Figure 6) with proven
mineralisation and significant high-grade intercepts that have yet to be followed up.
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Figure 6 – Regional geological interpretation of the Evanston Greenstone Belt. Showing two
primary camp-scale gold targets T1 and T2
T1 Gold Camp, Viper Prospect, located in Figure 6. Sequence of high magnesium basalts, ultramafic rocks and banded
iron formation, with minor sediments situated along the regional scale Evanston Shear Zone which has been intruded by
felsic to intermediate intrusions. Significant gold-in-soil anomalies and historical gold working situated along the main
banded iron formation horizon and immediately surrounding rocks. Significant 1,500m x 800m in soil Au-As-Sb anomaly
and historical gold workings (Rainy Rocks, Liberty) are situated along the main banded iron formation horizon. Figure 7
illustrates a summary of the exploration completed at the Viper drill target.
Key drill intersections include ⁵.
•
•
15m @ 1.5 g/t Au from 12m, including 3m @ 6.7 g/t Au in aircore hole BARC0136.
33m @ 0.3 g/t Au, incl. 3m @ 0.9 g/t Au in aircore hole BARAC0945.
Only 3 RC holes have been drilled at Viper. Significant intercepts remain open and represent exciting walk up drill targets
for CTN.
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Figure 7 – Exploration summary diagram of the Viper Prospect. Underlaying image is the regional
aeromagnetic image.
T2 Gold Camp, Figure 6: It is dominated by a large regional north-plunging syncline and contains minor felsic intrusions
and pegmatites. At Leghorn, mapping by the GSWA in 2001 (Greenfield, 2001) identified extensive vein networks and
significant rutile, sphene, and perovskite in outcropping calc-silicate lithologies. These minerals can contain major
amounts of Nb, Ta, Ce, Ti and Rare Earth elements (REEs).
This camp includes significant gold-in-soil anomalies and historical gold workings along major structural trends. Within
the calc silicate outcrops at Leghorn soil sampling, RC and aircore drilling have been completed⁵. Notable intercepts at
Leghorn include:
•
•
•
48m @ 0.6 g/t Au from 27m, including 21m @ 1.3 g/t Au in hole BARRC07 ⁸.
34m @ 0.5 g/t Au from 32m, including 1m @ 2.88 g/t Au in BARRDD02 ⁸.
7m @ 0.79% Cu, including 2m of 2.1% Cu, 535 ppb Au, 4 ppm Mo and 17.4 g/t Ag in RC hole BARRC01⁸
An exploration summary of the work conducted within the Leghorn project is illustrated in Figure 8. A structural trend
containing several mineralised drill holes including BARRC001, BARAC0856 and BARRC07 is supported by anomalous
Au, Ag, Mo and Cu soil geochemistry.
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At Erk, located 2 kms east of Leghorn in Figure 8, a 3km-long North-trending gold-in-soil anomaly overlays a sheared
granite and calc-silicate package. Drilled as a first-pass small AC program in 2023, with all drill lines intersecting gold
mineralisation, it remains open to the west, north and south. Numerous nugget patches exist at Erk and more are found
every year by local prospectors.
The geochemical attributes and gravity features occurring within calc silicate lithologies suggest a bulk tonnage Au-Cu
mineralisation model including potentially lucrative skarn style mineralisation may be applicable at Leghorn. Gold in
quartz vein hosted shear zones are applicable at Erk.
Figure 8 – Exploration summary of the Leghorn Prospect
A 2 km long structural trend of anomalous Cu and Au soil and drilling geochemistry
Soil Geochemistry
Whilst previous drilling has provided abundant follow-up drill targets, the acquired database containing over 20,000
soil samples and 700 rock chip samples will provide a steady pipeline of new drill targets. As the terrain is amenable
to soil geochemistry, with minor amounts of transported cover masking the underlying weathered bedrock, soil
sampling is an extremely cost-effective target generation tool.
The T8 Gold camp (discussed above) is located on the margin of a significant combined gravity and aerial magnetic
dome (T8 Dome) illustrated in Figure 9. The domal feature may be due to a deeply buried granitic intrusve. In addition
to the T8 soil anomaly, which identified the T8 prospect and is discussed above, two additional high tenor gold in soil
anomalies have been identified in locations around the dome margins. These soil anomalies remain open along strike
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and further extensional and in-fill soil sampling is warranted to refine and extend these anomalies. They are highly
anticipated future drill targets for Catalina Resources.
Figure 9 – The T8 Gold Prospect is located on the margins of a significant gravity and aerial magnetic
dome structure (T8 Dome). Two additional significant gold in soil anomalies have been identified in
locations around the dome margins and are not drilled. The background image is regional
aeromagnetic image.
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Laverton Gold Project
Aircore drilling by CTN was completed at the Laverton Project (E38/3697) in September 2024 (Figure 10). The Laveton
Project is located within the Laverton Gold Province, an exceptionally mineralised terrain in the Eastern Goldfields. The
region hosts several world class deposits of gold, nickel and rare earth elements (REEs) including Sunrise Dam, Wallaby,
Granny Smith and the Mt Weld REE deposit, one of the highest grade REE deposits in the world.
Drilling focussed upon the Barnicoat Shear Zone and its interpreted position within E38/3697 illustrated in Figure 11. The
Barnicoat Shear Zone is a significantly mineralised structure with several moderate size gold deposits scattered along its
length, illustrated in Figure 11. It is interpreted to pass through E36/3697, where it has been the focus of exploratory
drilling by Catalina.
Figure 10 – Regional location diagram of the Laverton Gold Project
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A significant zone of gold mineralisation was identified in hole LVAC049, near the interpreted position of the Barnicoat
Shear Zone, see Figure 11 and 12. Best assay results from analysis of the 1m splits using a Fire Assay method are as
follows ⁷:
•
LVAC049: 28m @ 1.09g/t Au from 57, Including 1m @ 9.69g/t Au from 57m.
This broad intersection of supergene gold mineralization with a high-grade zone of 1m @ 9.69g/t Au occurs within lower
saprolitic clay but is interpreted to be located directly above the bedrock source of the gold mineralization. The gold
intersection in LVAC049 is considered significant because it supports the visual observations of veining and alteration
logged in bottom of hole samples. Importantly, hole LVAC012 located 50m to the east intersected altered and veined
sediments at bottom of hole indicative of a hydrothermal system. The drilling cross section is illustrated in Figure 13.
Figure 11 – The north south orientated Barnicoat Shear Zone is a significantly mineralised
structure with several significant gold deposits scattered along its length
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Figure 12 – Drilling containing anomalous gold intersections outlined in the area marked in red,
including LVAC049: (28m @ 1.09g/t Au from 57m)
Figure 13 – The drilling cross section for aircore hole LVAC049
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Laverton REE Project
Anomalous REE intersections were returned from drilling in the gold target area illustrated in Figure 12. The high-grade
intersection in hole LVAC037 on the southernmost aircore traverse is particularly significant with a 4m zone with over
10,000ppm TREO (1%), illustrated in Figure 14.
•
9m @ 7,565ppm TREO from 47m in LVAC037 Including: 4m @ 13,406ppm (1.34%) TREO from 49m ₆
The REE assays in LVAC037 contain up to 0.3% NdPr (neodymium and praseodymium), a very high NdPr to total rare
earth oxides (“NdPr:TREO”) ratio. These ratios are similar to those encountered in the nearby Mt Weld carbonatite hosted
REE deposit which contains a resource of 54.7 Mt @ 5.3% TREO, (Duncan R. K. et al, 1990.). The neodymium magnets
made from praseodymium alloy is one of the most powerful and widely used rare earth magnets in electrical motor
manufacture, medical science, renewable energy, and high technology equipment (Constable, 2024).
Figure 14 – The high-grade intersection in hole LVAC037 is particularly significant with a 4m zone
intersecting over 10,000ppm TREO (1%)
The source of the REE mineralization is not known as the basement rocks are deeply weathered. However, the drilling
was 100m spaced so intrusive dykes related to the Mt. Weld carbonatite may be present.
Next Steps
The Company is highly encouraged by both the drill targets at the Central Yilgarn Project and the assay results from the
follow-up aircore drilling program completed at Laverton. The gold intersection in LVAC049 of 28m @ 1.09g/t Au from 57
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includes 1m @ 9.69g/t Au from 57m and is considered very significant as it supports the visual observations of veining
and alteration logged in bottom of hole samples.
Very significant REE intersections above 1% TREO were also intersected at Laverton.
RC drilling is planned to test the LVAC049 intersection at depth as well as the REE mineralization.
RC drilling and soil sampling is also planned for the targets discussed at the Central Yilgarn Project.
The release of this document to the market has been authorised by the Board of Catalina Resources Ltd.
Contacts
Investors / Shareholders
Ross Cotton
Executive Director
T: +61 (0)8 6165 8858
Competent Person Statement
The review of historical exploration activities and results contained in this report is based on information compiled by
Michael Busbridge, a Member of the Australian Institute of Geoscientists (AIG). He is a consultant to Catalina Resources
Ltd. He has sufficient experience which is relevant to the style of mineralisation and types of deposits under
consideration and to the activity which he is undertaking to qualify as a Competent Person as defined in the 2012 edition
of the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves (the JORC Code).
Michael Busbridge has consented to the inclusion in the report of the matters based on his information in the form and
context in which it appears.
The Company confirms that it is not aware of any new information or data that materially affects the information in the
original reports, and that the form and context in which the Competent Person’s findings are presented have not been
materially modified from the original reports.
Where the Company refers to the Mineral Resources in this report (referencing previous releases made to the ASX), it
confirms that it is not aware of any new information or data that materially affects the information included in that
announcement and all material assumptions and technical parameters underpinning the Mineral Resource estimate
with that announcement continue to apply and have not materially changed.
References (ASX):
This Report contains information extracted from ASX market announcements reported in accordance with the 2012
edition of the “Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves” (“2012
JORC Code”). Further details (including 2012 JORC Code reporting tables where applicable) of exploration results
referred to in this Quarterly Activities Report can be found in the following announcements lodged on the ASX:
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¹ 9/1/2025
2
14/6/2018
3
23/5/2024
⁴ 8/2/2024
5 5/4/2024
6
3/6/2024
⁷1/11/2024
Completion of Acquisition of Yerilgee & Evanston (ASX:CTN).
(ASX: AMD).
Shallow High-Grade gold and silver at Chicken Little. (ASX:DRE).
Seven Camp Scale Gold Prospects at Central Yilgarn (100%)
Drilling of 4 compelling gold targets commenced - Central Yilgarn.
Resampling Upgrades Gold and REE Targets at Laverton (ASX:CTN)
Catalina intersects 44m @ 1.01 g/t gold at Laverton.
These announcements are available for viewing on the Company’s website. The Company confirms that it is not aware
of any new information or data that materially affects the information included in any original ASX announcement.
Forward-Looking Statements
This announcement contains forward-looking statements that are subject to a range of risks and uncertainties. These
statements relate to the Company’s expectations, intentions, or strategies regarding the future. While the Company
believes these statements to be reasonable at the time of release, actual events or results may differ materially from
those anticipated. Readers are cautioned not to place undue reliance on forward-looking statements and should
consider all relevant assumptions and risk factors as disclosed by the Company.
References.
Constable, T., Australian rare earths and lithium projects set to transform the industry. Media Release. Minerals Council
Australia. March 2024.
Duncan R K, Willett G C. 1990. Mt Weld Carbonatite. In Hughes F E (ed). 1990. Geology of the Mineral Deposits of
Australia and Papua New Guinea. The Aus IMM. Monograph 14 v1 pp591-597.
Greenfield, J. E., 2001, Geology of the Lake Giles 1:100 000 sheet: Western Australia Geological Survey, 1:100 000
Geological Series Explanatory Notes, 19p.
ABOUT CATALINA RESOURCES LIMITED
Catalina Resources Limited is an Australian diversified mineral exploration and mine development company whose
vision is to create shareholder value through the successful exploration of prospective gold, base metal, lithium and
iron ore projects and the development of these projects into production.
Catalina Resources Limited
ACN 130 618 683
ASX: CTN
T: 61 8 6165 8858
E: info@catalinaresources.com.au
A : 2/7 Havelock Street
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JORC Code, 2012 Edition – Table 1 Report Template
SECTION 1 SAMPLING TECHNIQUES AND DATA
Criteria
Sampling
techniques
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.
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.
Commentary
DRE (Central Yilgarn Project) and CTN Laverton Project)
conducted aircore and reverse circulation drilling to obtain
1m samples which were placed on the ground from which
a scoop was used to composite 3m samples weighing
approximately 2‐3kgs being made up equally from each
sample pile.
RC Drilling (DRE)
Two sampling techniques were utilised for the RC
program, 1m metre splits directly from the rig sampling
system for each metre and 3m composite sampling from
spoil piles. Samples submitted to the laboratory were
determined by the site geologist.
From every metre drilled a 2-3kg sample (split) was subsampled into a calico bag via a Metzke cone splitter from
each metre of drilling or taken as a grab sample from the
bulk reject in more clay-rich material.
All remaining spoil from the sampling system was
collected in buckets or green plastic mining bags if wet
from the sampling system and neatly deposited in rows
adjacent to the rig. An aluminium scoop was used to then
sub-sample each spoil pile to create a 2-3kg 3m
composite sample in a calico bag.
QAQC samples consisting of duplicates, blanks, and
CRM’s (OREAS Standards) will be inserted through the
program at a rate of 1:50 samples.
All samples are submitted to ALS Laboratories in Perth for
determination of gold by fire-assay (ALS Method AuICP22). selected samples were also submitted for 48
multi-elements via 4 acid digestion with MS/ICP finish
(ALS Code ME-MS61) to assist with lithological
interpretation.
AC Drilling (DRE)
Aircore (AC) chips were collected at 1m intervals. 3m
composites were collected by a scoop sample from 1m
sample piles.
AC samples were collected via a static cone splitter
mounted beneath a cyclone return system attached to the
drill rig.
The static cone splitter produces up to two samples in
calico bags and a bulk reject sample, which was collected
in a bucket and placed in rows on the pad in 1m intervals.
1m sample splits were collected from the static cone
splitter and placed on the sample piles for later analysis.
2‐3 kg samples were collected from the sample piles.
Field duplicates were collected on a 1:50 ratio to ensure
repeatability of sampling method.
CRM standards were inserted on a 1:50 ratio to test the
calibration of lab equipment.
Sample weights have been recorded and reported by the
lab.
These samples will be dispatched to ALS Laboratories in
Perth for sample preparation and analysis.
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Criteria
JORC Code explanation
Commentary
3 kg samples were pulverised to 85% passing 75 micron
for an aqua regia digest of an 50g aliquot followed by ICP‐
MS for gold (ALS Code Au‐TL44).
If the samples returned values greater than 0.5ppm Au,
then a 50g aliquot was fused by fire assay and finished by
AAS.
AC Drilling (CTN).
The drilling contractor was Gyro Drilling from Kalgoorlie.
Gyro uses 3m drill rods. Holes were drilled to blade refusal
unless excess water was intersected.Hole diameter was
85mm / 3.5”.
Aircore drilling uses a three-bladed steel or tungsten drill
bit to penetrate the weathered layer of loose soil and rock
fragments. The drill rods are hollow and feature an inner
tube with an outer barrel (like RC drilling).
Aircore drilling uses small compressors (750 cfm/250 psi)
to drill holes into the weathered layer of loose soil and
fragments of rock. Compressed air is injected into the
space between the inner tube and the drill rods inside
wall, which flushes the cuttings up and out of the drill hole
through the rod’s inner tube, causing less chance of crosscontamination.
Gyro used an Air 750 CFM / 250 PSI Sullair Compressor
with additional Air Booster Support 750 CFM / 250PSI.
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.).
RC Drilling (DRE)
Challenge Drilling undertook the program utilising a KWL
380 drill rig with additional air from an auxiliary
compressor and booster. Reverse Circulation drilling
comprised a 90mm face sampling bit.
AC Drilling (DRE)
Aircore drilling comprised of a 90mm aircore sampling bit.
A smaller drill rig allows for better manoeuvrability in
remote drilling areas and lower drilling expenses.
AC Drilling (CTN).
Gyro used an Air 750 CFM / 250 PSI Sullair Compressor
with additional Air Booster Support 750 CFM / 250PSI.
Aircore drilling uses small compressors (750 cfm/250 psi)
to drill holes into the weathered layer of loose soil and
fragments of rock. Compressed air is injected into the
space between the inner tube and the drill rods inside
wall, which flushes the cuttings up and out of the drill hole
through the rod’s inner tube, causing less chance of crosscontamination.
Drill sample
recovery
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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.
RC Drilling (DRE)
Drilling was undertaken using a ‘best practice’ approach to
achieve maximum sample recovery and quality through
the minera
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