High Grade Ni-Cu-Co-PGE Massive Sulphides Confirmed
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ASX ANNOUNCEMENT 21 September 2023
High Grade Ni-Cu-Co-PGE Massive Sulphides Confirmed at Mangaroon (Earn-in)
HIGHLIGHTS
•
•
A 10-hole (1,074m) RC drill program was recently completed at the Bookathanna North and
High Range prospects along the 45km Money Intrusion, part of the Mangaroon Ni-Cu-PGE
Project. Visual Ni-Cu sulphide mineralisation was intersected over 400m strike, open in all
directions, at Bookathanna North which is located ~2.5kms north of Bookathanna where
mineralisation was intersected in 2022 (ASX 10 Nov 2022).
The first hole at Bookathanna North (REYRC013, for 153m) targeted a 37,000S conductor
plate, intersected 23m of Ni-Cu-Co-PGE sulphide mineralisation including 2m of massive
sulphides with results including (ASX 31 Aug 2023):
REYRC013: 23m @ 0.50% Ni
0.51% Cu
0.02% Co
0.49g/t 3PGE from 36m including:
2m @ 3.32% Ni
2.88% Cu
0.12% Co
1.46g/t 3PGE from 45m
•
Results from REYRC019, a 200m step out hole from REYRC013, which intersected 27m of NiCu sulphide mineralisation including 2m of semi-massive sulphides with no previously defined
geophysical signature are due in October 2023.
•
Given the tenor, style and thickness of mineralisation, the entire Money Intrusion will be
reassessed. One workstream is to complete induced polarisation (“IP”) surveys to search for
large-scale, net-textured and semi-massive sulphides which would not have been identified
with previous EM surveys. A further workstream is to complete down-hole EM (“DHEM”)
surveys to identify off-hole massive sulphides particularly at REYRC013 and REYRC019.
Understanding the “blind” signature at REYRC019 is also important.
Dreadnought Resources Limited (“Dreadnought”) is pleased to announce that rushed assay
results from REYRC013 have been received from RC drilling at Bookathanna North along
the 45km long Money Intrusion part of the Mangaroon Ni-Cu-PGE Project, located in the
Gascoyne Region of Western Australia.
Dreadnought’s Managing Director, Dean Tuck, commented: “For
the past two years, the work programs at the Money Intrusion have
focused on confirming the fertility, high tenor and potential to form
sulphide accumulations. This program has been a major leap forward
confirming massive and semi-massive sulphides within thick halos of
disseminated and net textured sulphides at a trap site within the Money
Intrusion. These assay results have now confirmed observations and
interpretations to date, further underscoring the potential of the Money
Intrusion to host significant Ni-Cu-Co-PGE sulphide mineralisation.
There are two key outcomes from this program. Firstly, that the Money
Intrusion can form high tenor massive sulphides and that the search for
additional trap sites is an imperative. Secondly, given the high tenor of
mineralisation, massive sulphides are not required for high-grade
mineralisation and geophysical techniques used to date need to be
broadened. We look forward to re-assessing the entire Money Intrusion,
including follow up geophysics and drilling at Bookathanna North later
in 2023.”
Figure 1: Nick Chapman (L) and Chris Manners (R) with semimassive sulphide RC chips from a step out drill hole at Bookathanna
North.
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SNAPSHOT – MANGAROON Ni-Cu-PGE
Major Miner, First Quantum Minerals, Earning-in
•
The potential of the Money Intrusion is underscored by an Earn-In with First Quantum Minerals Ltd (TSE:FM), a
~$20B TSX listed company (ASX 7 Apr 2021, ASX 30 Aug 2022).
•
First Quantum Minerals can earn an initial 51% interest by funding $12M of expenditure by 1 March 2026. First
Quantum Minerals may withdraw at any time during the earn-in phase with 0% interest.
•
Upon satisfying the earn-in requirements, a Joint Venture will be formed where First Quantum Minerals may elect
to increase its interest to 70% by sole funding expenditure up until a Decision to Mine.
•
Once a Decision to Mine has been made, Dreadnought can elect to either:
• Maintain its 30% by co-contributing.
• Dilute to 20% and be loan carried by First Quantum Minerals, repaid through revenue.
• Divest its 30% interest to First Quantum Minerals at fair market value.
•
Dreadnought retains gold rights across the earn-in tenements.
Fertile Ni-Cu-PGE System Confirmed
•
Fertile Ni-Cu-PGE sulphide systems are rare and the Money Intrusion has already been proven to contain high
tenor magmatic Ni-Cu-PGE mineralisation.
•
The Money Intrusion is confirmed to be ~800Ma, a fertile time for Ni-Cu-PGE systems globally. Highly prospective
keel geometries which are suitable for forming trap sites for magmatic sulphide accumulations have been identified.
•
First pass drilling in 2022 at the Bookathanna and High Range prospects intersected magmatic sulphide
mineralisation (ASX 10 Nov 2022). To date, the Ni and Cu have been in ~50:50 proportions.
•
Notwithstanding the early-stage drilling, a significant success rate has already been achieved. Out of the 22 RC
holes (2,906m) drilled to date, 15 holes have either assayed or shown visual/pXRF evidence of Ni-Cu-PGE
sulphides.
No Modern Exploration
•
Outcropping Ni sulphides were identified by Alan McDonald, the Pastoralist at Mangaroon in the early 1960s.
However, no detailed geophysical, geochemical or mapping programs were ever undertaken.
•
The first-ever detailed airborne magnetics, surface geochemical, ground EM and mapping surveys have now
confirmed the potential of the 45km long Money Intrusion.
Genuine Camp Scale Potential
•
Outcropping blebby sulphides have been confirmed over significant portions of the ~45km long Money Intrusion.
•
Multiple plumbing centres have been interpreted, each with the potential for trap sites within the magma pathways.
•
Mineralisation has already been confirmed by drilling at three prospects within the Money Intrusion: Bookathanna,
Bookathanna North and High Range.
Nickel and Copper are Critical to the Low Carbon Energy Transition
•
Nickel is essential to clean energy technologies including being a major cathode material in lithium-ion batteries.
Furthermore, nickel sulphide deposits have a much lower carbon footprint when being converted to Class 1 nickel
for battery grade applications.
•
Copper is essential for electricity-related technologies with renewable energy systems requiring up to 12x more
copper compared to traditional energy systems.
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Figure 2: Plan view image showing the location of recently completed drill holes (red dots) in relation to previous drilling
over a magnetics (RTP 1VD) and ortho image. The Money Intrusion is outlined in green.
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Technical Discussion of Ni-Cu-PGE RC Drilling (REYRC013-22)
The drill program was originally designed as 5 RC holes
with DHEM to test 5 EM conductors within the Money
Intrusion (2 at Bookathanna North and 3 at High
Range). Following the intersection of massive sulphides
in the first hole (REYRC013), an additional 5 holes were
drilled at Bookathanna North infilling and then stepping
out north and south along strike. A total of 10 holes
have been drilled (1,074m) with 7 holes at Bookathanna
North and 3 at High Range.
Drilling generally collared into the shallow and weakly
weathered gabbroic core of the Money Intrusion before
passing into the footwall olivine dolerite and finishing in
gneissic to granitic country rock. Significantly, the
furthest north hole (REYRC017) intersected a thick
gabbroic core and did not reach the mineralised
footwall olivine dolerite or country rock. REYRC017
highlights the variable geometry of the Money Intrusion
and potential to form trap sites for sulphide
accumulation.
Importantly, 6 of the 7 holes at Bookathanna North
intersected thick (10-50m) disseminated and net
textured Ni-Cu sulphides within the footwall olivine
Figure 3: Photo of massive sulphide RC chips from
dolerite. Of these, REYRC013 and REYRC019 each
REYRC013 45-46m comprised of 40-50% pentlandite and
intersected 2m of semi-massive to massive sulphides
chalcopyrite.
within the mineralised envelope. All sulphide
mineralisation consists of pentlandite (Fe,Ni)9S8, chalcopyrite (CuFeS2) and pyrrhotite (Fe(1-x)S) with pentlandite and
chalcopyrite making up ~40-50% of the sulphide mix with the remainder being pyrrhotite.
Assay results have been received for REYRC013 with significant results including:
REYRC013: 23m @ 0.50% Ni
0.51% Cu
0.02% Co
0.49g/t 3PGE from 36m including:
2m @ 3.32% Ni
2.88% Cu
0.12% Co
1.46g/t 3PGE from 45m
The assay results have confirmed the high tenor mineralisation which importantly include significant palladium,
platinum, gold (“3PGE”) and cobalt credits. The 3PGE credits are made up of ~70% palladium, ~20% platinum and
~10% gold.
A mass balance of the mineralisation indicates that the logged massive sulphide interval was a mix of massive and
semi-massive sulphides leaving open the potential for even higher grades should a significant massive sulphide body
be located in further drilling. This observation further enhances the significance of REYRC019 which was a blind step
out hole not targeting a conductive anomaly. REYRC019 intersected semi-massive sulphides emphasising the need
for the entire Money Intrusion to be reassessed given the results to date.
At High Range, 3 holes were drilled (REYRC020-22, 255m) targeting three conductive plates ranging from 450-900S.
These holes intersected sheared metasediments within the Edmund Group explaining the EM conductors. These
results will be incorporated into the overall reassessment of the entire Money Intrusion.
DHEM surveys of the holes drilled is currently underway and an IP survey is expected to commence in October
2023.
Further assay and DHEM results are expected in October 2023.
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Discussion of Ni-Cu-PGE Exploration (E08/3274, E8/3178, E09/2384, E09/2433, E09/2473: First Quantum Minerals Earn-in)
The confirmation of a fertile magmatic Ni-Cu-PGE system within the 45km long Money Intrusion highlights the
potential for multiple deposits and/or deposit styles as outlined below.
-
Jinchuan Ni-Cu-PGE: The Money Intrusion has been dated to ~800Ma, similar in age and tectonic setting
to the Jinchuan Ni-Cu-PGE deposit in China (>500 Mt @ 1.2% Ni, 0.7% Cu, ~0.4 g/t PGE, Lightfoot 2007).
Jinchuan contains three main deposits over ~6.5kms of strike, each situated within a sub-chamber of the
overall intrusion. Only one of the deposits outcrops at surface. Mineralisation is dominated by net-textured
and disseminated sulphides with minor massive sulphide accumulations. The disseminated sulphides form an
envelope around the higher-grade, net-textured and massive sulphides.
-
Eagle and Eagle East: To date, 15 out of 22 RC holes intersected mineralisation along significant strike
showing increasing width and intensity near subtle changes in the walls and base of the intrusion, including
the formation of massive and semi-massive mineralisation. These results highlight the potential for massive
sulphide mineralisation to concentrate and form at trap sites. This is similar to Eagle and Eagle East (~5Mt
@ 3.5% Ni, 2.9% Cu, 1.6g/t PGE, 0.1% Co, Lundin 2013) located in North America.
Drill targeting to date has been dominated by FLEM surveys designed to identify near-surface, massive sulphides along
the southwestern edge of the Money Intrusion. Drilling has confirmed high tenor massive, semi-massive sulphides
within a halo of net-texture and disseminated sulphides with mineralisation intensifying in trap sites along the edges
and base of the intrusion. Drilling at Bookathanna North has confirmed that thick mineralisation occurs over a
significant strike length and that net-textured and semi-massive sulphide accumulations have not been identified by
the FLEM surveys.
Given the high tenor of the Ni-Cu
sulphide system, net-textured and
semi-massive
sulphides
are
attractive targets in their own right.
Additionally, deeper trap sites with
the potential to form significant
massive sulphide accumulations
have not been targeted or assessed.
Targeting going forward will focus
on identifying and understanding:
- large scale, net textured and
heavily
disseminated
sulphide
mineralisation using IP surveys; and
- deep trap sites for massive
sulphides
using
geophysical
inversions, DHEM and more
powerful EM surveys; and
- blind mineralisation as seen at
REYRC019.
A reassessment of the Money
Intrusion and the targeting
completed to date is underway
with further drill targets expected
in the December 2023 quarter.
Figure 4: Plan view image showing
the location of recently completed
drill holes at Bookathanna North in
relation to FLEM plates over an
orthoimage and interpreted Money
Intrusion.
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Background on Mangaroon (E08/3274, E8/3178, E09/2384, E09/2433, E09/2473: First Quantum Minerals Earn-in) (E08/3275,
E08/3439, E09/2290, E09/2359, E09/2370, E09/2405, E09/2448, E09/2449, E09/2450, E09/2467, E09/2478, E09/2531, E09/2535, E09/2616,
M09/91, M09/146, M09/147, M09/174, M09/175: 100%)
Mangaroon (Figure 5) covers >5,200sq kms of the Mangaroon Zone in the Gascoyne Region of Western Australia
and is comprised of:
-
the ~45km long Money Intrusion (First Quantum Minerals earn-in) which contains high tenor magmatic NiCu-PGE mineralisation;
-
the >10km long Mangaroon Au Shear Zone (100%) where fractured, small scale ownership has limited
previous gold exploration with only ~200m of the >10km having been drilled notwithstanding the high-grade,
camp scale potential;
-
the ~43km long Yin REE Ironstone Complex (100%) which already contains: an independent total Resource
of 20.06Mt @ 1.03% TREO (ASX 5 Jul 2023) over only ~4km of the ~43km of ironstones including an initial
Indicated Resource of 5.52Mt @ 1.23% TREO over only ~250m of strike (ASX 5 Jul 2023); and an Exploration
Target of 50-100Mt at 0.9-1.3% TREO (ASX 13 Feb 2023) over 40 kms of strike.
-
the ~9km long REE-Nb-Ti-P-Sc C1-C5 carbonatites which contain an initial independent Inferred Resource
of 10.84Mt @ 1.00% TREO at C3 (ASX 28 Aug 2023).
Figure 5: Plan view map of Mangaroon showing the location of the First Quantum Minerals Earn-in and 100% Dreadnought
ground (Mangaroon Au Shear Zone, Yin REE Ironstone Complex and REE-Nb-Ti-P-Sc C1-C5 carbonatites).
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For further information please refer to previous ASX announcements:
•
•
•
•
•
•
•
•
•
•
25 November 2020
7 April 2021
14 February 2022
10 June 2022
30 August 2022
10 November 2022
24 March 2023
30 August 2023
31 August 2023
12 September 2023
Mangaroon Ni-Cu-PGE & Au Project
Option/JV Agreement Signed with Global Base Metal Miner
Conductors Defined Along the Money Intrusion
Drilling Successfully Completed at Mangaroon Ni-Cu-PGE
Mangaroon Ni-Cu-PGE Project advances to $15M Earn-In
Exploration Update Mangaroon Ni-Cu-PGE (FQM Earn-In)
Five Strong EM Conductors at Mangaroon Ni-Cu-PGE Project
Drilling Commenced at Money Intrusion Ni-Cu-PGE
Massive and Disseminated Ni-Cu Sulphides Intersected
Thick Ni-Cu Mineralisation over 400m, Open in all Directions
UPCOMING NEWSFLOW
August-December: Ongoing drilling results from completed drilling at Mangaroon REE (100%)
September: Results of geophysical surveys at Mangaroon (100%)
September: Commencement of drilling at Tarraji-Yampi (80% and 100%)
September: Results of geophysical and geochemical surveys at Central Yilgarn (100%)
October: DHEM and Further Assay Results from Money Intrusion (Earn-in)
October/November: Results from target generation and definition work at Bresnahan (100%)
October/November: Further RC drilling at Mangaroon Ni (Earn-in) and Au, REEs (100%)
October: Quarterly Activities and Cashflow Report
23 November: Annual General Meeting
December 2023 quarter: REE Resource upgrade (Mangaroon 100%)
~Ends~
For further information please contact:
Dean Tuck
Managing Director
Dreadnought Resources Limited
E: dtuck@dreres.com.au
Jessamyn Lyons
Company Secretary
Dreadnought Resources Limited
E: jlyons@dreres.com.au
This announcement is authorised for release to the ASX by the Board of Dreadnought.
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Cautionary Statement
This announcement and information, opinions or conclusions expressed in the course of this announcement contains forecasts and
forward-looking information. Such forecasts, projections and information are not a guarantee of future performance, involve unknown
risks and uncertainties. Actual results and developments will almost certainly differ materially from those expressed or implied. There
are a number of risks, both specific to Dreadnought, and of a general nature which may affect the future operating and financial
performance of Dreadnought, and the value of an investment in Dreadnought including and not limited to title risk, renewal risk,
economic conditions, stock market fluctuations, commodity demand and price movements, timing of access to infrastructure, timing of
environmental approvals, regulatory risks, operational risks, reliance on key personnel, reserve estimations, native title risks, cultural
heritage risks, foreign currency fluctuations, and mining development, construction and commissioning risk.
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.
Competent Person’s Statement – Exploration Results
The information in this announcement that relates to geology, exploration results and planning, and exploration targets was compiled
by Mr. Dean Tuck, who is a Member of the AIG, Managing Director, and shareholder of the Company. Mr. Tuck has sufficient
experience which 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. Tuck consents to the inclusion in the announcement of the matters based on the 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 forma and context in which the Competent Person’s findings are presented have not been materially modified from the
original reports.
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INVESTMENT HIGHLIGHTS
Kimberley Ni-Cu-Au Project (80/100%)
The project is located only 85kms from Derby in the
West Kimberley region of WA and was locked up as a
Defence Reserve since 1978.
The project has outcropping mineralisation and historic
workings which have seen no modern exploration.
Results to date indicate that there may be a related,
large scale, Proterozoic Cu-Au-Ag-Bi-Sb-Co system at
Tarraji-Yampi, similar to Cloncurry/Mt Isa and Tennant
Creek.
Mangaroon Ni-Cu-PGE JV & Au/REE 100%
Project
Mangaroon covers ~5,200 kms and is located 250kms
south-east of Exmouth in the Gascoyne Region of WA.
At the Money Ni-Cu-PGE has been identified and is
subject to an earn-in by First Quantum Minerals (up to
70%). Dreadnought also has areas of outcropping highgrade gold including the historic Star of Mangaroon and
Diamonds gold mines. In addition, Mangaroon has
emerged as a globally significant, rapidly growing,
potential source of critical minerals. Highlights include:
-
An Exploration Target of 50-100Mt at 0.9-1.3%
TREO estimated for the top 150m of the ~43km
long Yin REE Ironstone Complex (ASX 13 Feb 2023).
-
An independent Resource for Yin Ironstones Complex of 20.06Mt @ 1.03% TREO over only ~4kms – including
an Indicated Resource of 5.52Mt @ 1.23% TREO over just 250m strike (ASX 5 Jul 2023).
-
Regional source of rare earths at the C1-C5 carbonatites totaling ~9kms x ~1km (ASX 7 Aug 2023).
-
A large, independent initial Resource of 10.84Mt @ 1.00% TREO at C3, containing a range of critical minerals
including rare earths, niobium, phosphate, titanium and scandium (ASX 28 Aug 2023).
Bresnahan HREE and Au Project (100%)
Bresnahan is located ~125km southwest of Newman in the Ashburton Basin. The project comprises ~3,700 sq kms
covering over 200kms strike along the Bresnahan Basin / Wyloo Group unconformity. Bresnahan is prospective for
unconformity related heavy rare earth (“HREE”) deposits similar to Browns Range HREE deposits and mesothermal
lode gold similar to Paulsen’s Au-Ag-Sb deposits along strike.
Prior to consolidation by Dreadnought, the Bresnahan Basin had only been explored for unconformity uranium with
limited exploration for mesothermal gold. Bresnahan is a first mover opportunity to explore for unconformity HREE.
Central Yilgarn Gold, Base Metals, Critical Minerals & Iron Ore Project (100%)
Central Yilgarn is located ~190km northwest of Kalgoorlie in the Yilgarn Craton. The project comprises ~1,600 sq
kms covering ~150km of strike along the majority of the Illaara, Yerilgee and Evanston greenstone belts. Central
Yilgarn is prospective for typical Archean mesothermal lode gold deposits, VMS base metals, komatiite hosted nickel
sulphides and critical metals including Lithium-Caesium-Tantalum.
Prior to consolidation by Dreadnought, the Central Yilgarn was predominantly held by iron ore explorers and
remains highly prospective for iron ore.
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Table 1: Significant Sulphide Intervals – Visual Estimates
REYRC014
REYRC015
REYRC016
From
(m)
37
45
47
35
28
41
To
(m)
45
47
51
61
57
73
Interval
(m)
8
2
4
26
29
32
REYRC018
5
58
53
REYRC019
59
78
80
78
80
86
19
2
6
Hole ID
REYRC013
Mineralisation
Style
Disseminated
Massive
Net Textured
Disseminated
Disseminated
Disseminated
Disseminated /
Net Textured
Disseminated
Semi-Massive
Disseminated
Sulphide Type
Sulphide %
Prospect
1-5
80-100
5-10
1-10
1-5
1-5
Bookathanna North
Pyrrhotite,
Pentlandite,
Chalcopyrite
1-20
1-5
30-40
1-10
Table 2: Drill Collar Data (GDA94 MGAz50)
Hole ID
REYRC013
REYRC014
REYRC015
REYRC016
REYRC017
REYRC018
REYRC019
REYRC020
REYRC021
REYRC022
Easting
364221
364222
364192
364245
364279
364150
364136
360783
360759
360725
Northing
7384666
7384657
7384670
7384710
7384805
7384574
7384456
7376739
7376696
7376672
RL
286
288
285
288
288
288
286
334
333
333
Dip
-70
-70
-85
-75
-70
-60
-80
-60
-60
-60
Azimuth
045
40
215
15
20
30
215
290
270
260
EOH
153
141
81
87
177
69
111
57
81
117
Type
RC
RC
RC
RC
RC
RC
RC
RC
RC
RC
Prospect
Bookathanna North
High Range
JORC Code, 2012 Edition – Table 1 report template
Section 1 Sampling Techniques and Data
(Criteria in this section apply to all succeeding sections.)
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
RC Drilling
Reverse Circulation (RC) drilling was undertaken to produce
samples for assaying.
Two sampling techniques were utilised for this program, 1m
metre splits directly from the rig sampling system each
metre and 2m composite sampling from spoil piles. Samples
submitted to the laboratory were determined by the site
geologist.
1m Splits
Every metre drilled a 2-3kg sample (split) was sub-sampled
into a calico bag via a Metzke cone splitter from each metre
of drilling.
2m Composites
All remaining spoil from the sampling system was collected
in buckets 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 2m
composite sample in a calico.
For gold and PGEs, all samples are submitted to the
laboratory and pulverised to produce a 50g charge for Fire
Assay (ALS Code PGM-ICP24).
Base Metal and lithological samples are analysed for 48 multielements via 4 acid digestion with MS/ICP finish (ALS Code
ME-MS61)
Drilling techniques
•
Drill type (e.g. core, reverse circulation, open-hole hammer,
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Criteria
JORC Code explanation
Commentary
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.
RC Drilling
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.
RC Drilling
RC chips were logged under the supervision of a qualified
geologist with sufficient experience in this geological terrane
and relevant styles of mineralisation using an industry
standard logging system which could eventually be utilised
within a Mineral Resource Estimation.
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.).
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Logging
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Ausdrill undertook the program utilising a Drill Rigs
Australia truck mounted Schramm T685WS drill rig with
additional air from an auxiliary compressor and booster. Bit
size was 5¾”.
Drilling was undertaken using a ‘best practice’ approach to
achieve maximum sample recovery and quality through the
mineralised zones.
Best practice sampling procedure included: suitable usage of
dust suppression, suitable shroud, lifting off bottom between
each metre, cleaning of sampling equipment, ensuring a dry
sample and suitable supervision by the supervising geologist
to ensure good sample quality.
Lithology, mineralisation, alteration, veining, weathering and
texture were all recorded digitally.
Chips were washed each metre and stored in chip trays for
preservation and future reference.
RC pulp material is also analysed on the rig by pXRF and
magnetic susceptibility meter to assist with logging and the
identification of mineralisation.
Logging is qualitative, quantitative or semi-quantitative in
nature.
Sub-sampling
techniques and sample
preparation
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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.
Preliminary pXRF analysis
pXRF analysis of pulverised and partially homogenised reject
RC sample piles is fit for purpose as a preliminary
exploration technique.
pXRF is a spot reading on raw (unprocessed) RC sample
piles with variable grain sizes and states of homogenisation.
High grade results were repeated at multiple locations to
confirm repeatability. The competent person considers this
acceptable within the context of reporting preliminary
exploration results.
RC Drilling
From every metre drilled, a 2-3kg sample (split) was subsampled into a calico bag via a Metzke cone splitter or taken
as a grab sample from the bulk reject in more clay-rich
material.
QAQC in the form of duplicates and CRM’s (OREAS
Standards) were inserted through t
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