New High-grade Lithium Drill Results within 20km of Grants
Released
Released
Announcement PDF
Level 9, 2 Mill Street
Perth WA 6000
T 61 8 8317 1700
E info@corelithium.com.au
ABN 80 146 287 809
ASX CXO
6 November 2024
ASX: CXO Announcement
New high-grade Lithium drill results within
20km of the Grants processing facility
Highlights
•
Excellent new lithium drilling results at the Blackbeard prospect, including:
o
63m @ 1.67% Li2O from 166m, including 20m @ 2.09% Li2O from 208m (NRC269)
•
Builds on strong previously reported Blackbeard results of 41m @ 1.63% Li2O from 137m
(SRC117) and 59m @ 1.54% Li2O from 158m (SRC118).1
•
Lithium mineralisation now confirmed over 600m of strike when combined with the
adjacent Centurion prospect.
•
The Blackbeard mineralisation is clearly defined and entirely contained within Core
Lithium’s 100%-owned Mining Lease. This lease is strategically located within 20km of
the Grants processing facility.
Core Lithium Ltd (ASX:CXO) (Core or Company) is pleased to provide an update on the exploration drilling
program being undertaken at the 100% owned Finniss Lithium Project (Finniss Project). Initial assays have been
received from RC (reverse circulation) drilling with wide zones of spodumene mineralisation intersected at the
Blackbeard prospect (Figure 1). These results, together with those previously reported for the nearby Centurion
prospect, demonstrate mineralised pegmatites exist along a clearly defined strike length within the Company’s
existing mining lease.
The exploration focus for the 2024 field season at Finniss has been on testing large scale pegmatite targets which
can potentially sustain lower cost production. Results are presented here for 27 drill holes that represent 4,880m
of drilling across a range of prospects that are all within 20km of the Grants Processing Facility.
1 See ASX announcement “Significant Increase to Finniss Mineral Resources” on 18 April 2023
corelithium.com.au
1
Commenting on the Blackbeard drilling results, Core CEO Paul Brown said:
“The results from Blackbeard are highly encouraging and indicate we have discovered a large, highly mineralised
pegmatite within a short distance of our processing infrastructure, consistent with the key objective of our 2024
field season. Blackbeard is up to 45 metres wide and open at depth. Further drilling will be completed to determine
the ultimate scale of the system. This will support a future Mineral Resource Estimate and have potential to be
incorporated into our ongoing restart studies.”
Figure 1: Location of Blackbeard prospect and Grants processing facility
Blackbeard
Excellent results were received from seven drill holes infilling and testing depth extensions at the Blackbeard
prospect (Table 1 and Figure 2). Results from the current RC drill program included:
•
63m @ 1.67% Li2O from 166m, including 20m @ 2.09% Li2O from 208m (NRC269)
•
24m @ 0.70% Li2O from 188m (NRC270)
•
22m @ 0.68% Li2O from 135m, including 6m @ 1.25% Li2O from 208m (FRC488)
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Previous intersections at Blackbeard include 41m @ 1.63% Li2O (SRC117) and 59m @ 1.54% Li2O (SRC118)1.
Drilling to date has demonstrated that the primary mineralised pegmatite body is steeply dipping within the mining
lease, up to 45m in true thickness and remains open at depth (Figure 3). With the largest and highest-grade
intersection in NRC269 currently also the deepest. Furthermore, the drilling has identified a smaller subparallel
pegmatite body to the north of the main pegmatite (Figure 3) with current indications that it is also mineralised. While
many of the drill holes intersected this secondary body, it was often intersected at shallow depths in the weathering
zone where lithium is typically depleted.
Several holes did intersect fresh pegmatite however, including:
•
10m @ 0.91% Li2O from 108m (NRC269)
Blackbeard is located directly northeast of the nearby Centurion prospect (Figure 2) where previous drilling resulted
in mineralised intersections including 22m @ 0.74% Li2O (CRC001) and 18m @ 0.85% Li2O (FRC391)2.
The drill results at the Blackbeard and Centurion prospects (Figure 2) define a mineralised trend with a strike
extent of over 600m. This makes Blackbeard-Centurion one of the larger pegmatite trends discovered to date
within the Finniss Project area.
The two pegmatites appear to be closed off to the northeast and southwest but remain open at depth. They are
located entirely within Core’s granted Mining Lease (MLN1148) and this may enable a quicker path to
development.
A number of other prospects within the immediate vicinity such as Northern Reward, Kristies and Frilled Lizard
(Figure 2) also warrant further drill testing and exploration.
Regional Results - Drilling
First pass drilling at other prospects, including at Kristies, Zola East, Rocky Ridge West and Archer (Table 1) did
not intersect any significant lithium mineralisation despite many of these holes intersecting pegmatite. An
evaluation of the results will be undertaken to determine if any follow-up drilling is warranted.
Next Steps
Drilling is continuing at a number of high priority pegmatite targets across the Finniss Project including further
drilling of targets adjacent to Blackbeard. All targets are within trucking distance of the Grants processing facility
and results are expected next month.
Given these excellent results, it is anticipated that further drilling will be undertaken at Blackbeard as soon as
practicable after the end of the wet season in early CY25. Drilling would target depth extensions to the
mineralisation as well as potentially collecting geotechnical information and samples for preliminary metallurgical
test work. If drilling is successful, it would provide the data necessary to include Blackbeard (alongside deposits
such as BP33, Carlton and Lees) in any re-start strategy and longer-term mine plan discussions.
2 See ASX announcement “Finniss Lithium Project Exploration Update” on 13 December 2021
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Figure 2: Blackbeard drill plan
Figure 3: Blackbeard Cross Section
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This announcement has been approved for release by the Board of Core Lithium Ltd.
For further information, please contact:
Investor Enquiries
Media enquiries
Paul Brown
Michael Vaughan
CEO
Executive Director
Core Lithium Ltd
Fivemark Partners
+61 8 8317 1700
+61 422 602 720
info@corelithium.com.au
michael.vaughan@fivemark.com.au
About Core
Core Lithium Ltd (ASX: CXO) (Core or Company) is an Australian hard-rock lithium company that owns the
Finniss Lithium Operation on the Cox Peninsula, south-west and 88km by sealed road from the Darwin Port,
Northern Territory. Core's vision is to generate sustained value for shareholders from critical minerals exploration
and mining projects underpinned by strong environmental, safety and social standards.
For further information about Core and its projects, visit www.corelithium.com.au
Important Information
This announcement may reference forecasts, estimates, assumptions and other forward-looking statements.
Although the Company believes that its expectations, estimates and forecast outcomes are based on reasonable
assumptions, it cannot assure that they will be achieved. They may be affected by various variables and changes in
underlying assumptions subject to risk factors associated with the nature of the business, which could cause results
to differ materially from those expressed in this announcement. The Company cautions against reliance on any
forward-looking statements in this announcement.
Competent Person Statement
The information in this release that relates to Exploration Results has been compiled by Dr Graeme McDonald. Dr
McDonald is the Resource Manager for Core Lithium Ltd. Dr McDonald is a member of the Australasian Institute of
Mining and Metallurgy and the Australian Institute of Geoscientists. He has sufficient experience with the style of
mineralisation, deposit type under consideration and to the activities 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” (The JORC Code). Dr McDonald consents to the inclusion in this report of the contained technical
information relating to the Exploration Results in the form and context in which it appears.
The Company confirms it is not aware of any new information or data that materially affects the information cross
referenced in this announcement. The Company confirms that the form and context in which the Competent Person’s
findings are presented have not been materially modified from the original announcements.
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Table 1. Summary of drill hole data and received assay results from exploration activities at the Finniss Project
Hole ID
Prospect
Type
NRC268
NRC269
Blackbeard
Blackbeard
RC
RC
GDA94 Grid
East
687221
687118
GDA94 Grid
North
8585243
8585203
Dip (°)
-69.9
-71.8
Azimuth (°)
145.92
148.41
Depth (m)
From (m)
216
254
and
incl
NRC270
Blackbeard
RC
686981
8585143
-68.3
148.14
240
and
incl
and
NRC271
FRC488
Blackbeard
Blackbeard
RC
RC
686899
686984
8585108
8585082
-67.9
-63.0
144.64
145.92
252
174
FRC489
FRC490
NRC272
NRC273
NRC274
FRC492
FRC493
FRC494
FRC491
FRC495
FRC496
FRC497
FRC498
FRC499
FRC500
FRC501
FRC502
FRC503
FRC504
FRC505
FRC506
FRC507
Blackbeard
Blackbeard
Kristies
Kristies
Kristies
Kristies
Kristies
Kristies
Northern Reward
Frilled Lizard
Zola East
Zola East
Zola East
Zola East
Rocky Ridge West
Rocky Ridge West
Rocky Ridge West
Rocky Ridge West
Archer
Archer
Archer
Archer
RC
RC
RC
RC
RC
RC
RC
RC
RC
RC
RC
RC
RC
RC
RC
RC
RC
RC
RC
RC
RC
RC
686929
687234
686498
686603
686469
686512
686497
686528
687251
686477
691137
691129
690957
690953
692329
692377
692429
692473
692380
692428
692473
692496
8585073
8585190
8585019
8585114
8584783
8584871
8584878
8584751
8584878
8584431
8591457
8591557
8591386
8591490
8589120
8589166
8589247
8589312
8589468
8589519
8589590
8589643
-60.5
-63.4
-67.8
-70.6
-70.2
-62.7
-63.4
-65.8
-72.7
-64.9
-64.9
-64.7
-60.2
-60.3
-60.7
-65.6
-63.3
-63.3
-65.1
-65.4
-65.1
-65.3
142.99
144.85
118.98
117.22
114.6
113.79
107.82
112.89
294.55
113
266.04
268.76
91.65
89.66
298.15
297.13
299.66
300.78
304.81
310.78
306.21
307.52
174
102
300
246
222
120
174
180
210
204
180
162
180
180
126
84
126
132
150
168
150
174
To (m)
No Significant Intercept
108.0
118.0
166.0
229.0
208.0
228.0
166.0
167.0
188.0
212.0
197.0
198.0
215.0
219.0
No Significant Intercept
109
112
135
157
144
150
No Significant Intercept
60
74
No Significant Intercept
No Significant Intercept
No Significant Intercept
No Significant Intercept
No Significant Intercept
No Significant Intercept
No Significant Intercept
No Significant Intercept
No Significant Intercept
No Significant Intercept
No Significant Intercept
No Significant Intercept
No Significant Intercept
No Significant Intercept
No Significant Intercept
No Significant Intercept
No Significant Intercept
No Significant Intercept
No Significant Intercept
No Significant Intercept
Interval
(m)
Grade
(Li2O %)
10.0
63.0
20.0
1.0
24.0
1.0
4.0
0.91
1.67
2.09
0.88
0.70
1.70
0.76
3
22
6
0.65
0.68
1.25
14
0.90
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6
JORC Code, 2012 Edition – Table 1 Report
Section 1 Sampling Techniques and Data
(Criteria in this section apply to all succeeding sections)
Criteria
JORC Code Explanation
Commentary
Sampling
techniques
•
•
•
•
•
Drilling
techniques
•
Drill sample
recovery
•
•
•
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.
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).
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.
•
•
Reverse circulation (RC) drill techniques have been employed for the Core
Lithium Ltd (“Core” or “CXO”) drilling. A list of the hole IDs and positions
for drilling discussed in the release has been included.
RC drill spoils over all programs were collected into two sub-samples:
-1 metre split sample, homogenized and cone split at the cyclone into
12x18 inch calico bags. Weighing 2-5 kg, or 15% of the original sample.
-20-40 kg primary sample, which for CXO’s drilling was collected in
600x900mm green plastic bags and retained until assays had been
returned and deemed reliable for reporting purposes.
RC sampling of pegmatite for CXO’s assays was done on a 1 metre basis.
1m sampling continued into the barren wall-zone adjacent to the
pegmatite.
•
RC Drilling was carried out with 5 inch face-sampling bit.
•
RC drill recoveries were visually estimated from volume of sample
recovered. The majority of sample recoveries reported were above 90% of
expected.
RC samples were visually checked for recovery, moisture and
contamination and notes made in the logs.
The rigs splitter was emptied between 1m samples. A gate mechanism on
the cyclone was used to prevent inter-mingling between metre intervals.
The cyclone and splitter were also regularly cleaned by opening the doors,
visually checking, and if build-up of material was noted, the equipment
cleaned with either compressed air or high-pressure water.
Drill collars are sealed to prevent sample loss and holes are normally
drilled dry to prevent poor recoveries and contamination caused by water
ingress. Wet intervals are noted in case of unusual results.
•
•
•
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Criteria
JORC Code Explanation
Commentary
•
Logging
•
•
•
Sub-sampling
techniques
and sample
preparation
•
•
•
•
•
•
Quality of
assay data
and laboratory
tests
•
•
•
Verification of
sampling and
assaying
•
•
•
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.
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/secondhalf sampling.
Whether sample sizes are appropriate to the grain size
of the material being sampled.
The nature, quality and appropriateness of the
assaying and laboratory procedures used and whether
the technique is considered partial or total.
For geophysical tools, spectrometers, handheld XRF
instruments, etc, the parameters used in determining
the analysis including instrument make and model,
reading times, calibrations factors applied and their
derivation, etc.
Nature of quality control procedures adopted (e.g.
standards, blanks, duplicates, external laboratory
checks) and whether acceptable levels of accuracy (i.e.
lack of bias) and precision have been established.
The verification of significant intersections by either
independent or alternative company personnel.
The use of twinned holes.
Documentation of primary data, data entry procedures,
data verification, data storage (physical and electronic)
protocols.
•
•
•
•
•
•
•
•
•
•
•
•
•
•
•
•
•
•
•
•
•
•
Previous studies of the lithium mineralisation have shown that there is no
sample bias due to preferential loss/gain of the fine or coarse material.
Detailed geological logging was carried out on all RC drill holes.
Logging recorded lithology, mineralogy, mineralisation, weathering, colour,
and other sample features.
RC chips are stored in plastic RC chip trays.
All holes were logged in full.
Pegmatite sections are also checked under a single-beam UV light for
spodumene identification on an ad hoc basis. These only provide
indicative qualitative information.
RC chip trays are photographed and stored on the CXO server.
The majority of the mineralised samples were collected dry, as noted in
the drill logs and database.
RC samples were collected from the cone splitter on the drill rig into a
calico bag for dispatch to the laboratory.
The sample sizes are considered more than adequate to ensure that there
are no particle size effects relating to the grain size of the mineralisation.
A field duplicate sample regime is used to monitor sampling methodology
and homogeneity of RC drilling. The typical procedure was to collect
duplicates via a split directly from the cone splitter.
Sample prep for drilling occurs at Intertek Laboratories, Darwin, NT.
RC samples do not require any crushing, as they are largely pulp already.
RC Samples are then split and prepared by pulverising to 95% passing 100 um.
Field and lab standards together with blanks were used routinely.
For drilling, lithium sample analysis occurs at Intertek, Darwin, NT.
All samples are crushed and pulverized.
For lithium samples, a sub-sample of the pulp is digested via a sodium
peroxide fusion in a Ni crucible and analysed via ICP-MS and ICP-OES
methods for the following elements: Li, Al, B, Ba, Be, Ca, Cs, Fe, K, Mg,
Mn, Nb, P, Rb, S, Sn, Sr, Ta, W and As.
Intertek utilise standard internal quality control measures including the use
of Certified Lithium Standards and duplicates/repeats.
CXO implemented quality control procedures include appropriate certified
Lithium ore standards, duplicates for RC drilling and blanks.
There were no significant issues identified with any of the QAQC data.
Senior technical personnel have visually inspected and verified the
significant drill intersections.
All field data is entered into specialised Ocris logging software (supported
by look-up tables) at site and subsequently validated as it is imported into
the centralized CXO Access database.
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Criteria
JORC Code Explanation
Commentary
•
•
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
Orientation of
data in
relation to
geological
structure
•
•
•
•
•
Sample
security
•
Audits or
reviews
•
Data spacing for reporting of Exploration Results.
Whether the data spacing and distribution is sufficient
to establish the degree of geological and grade
continuity appropriate for the Mineral Resource and
Ore Reserve estimation procedure(s) and
classifications applied.
Whether sample compositing has been applied.
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.
•
The results of any audits or reviews of sampling
techniques and data.
•
•
•
•
•
•
Hard copies of survey and sampling data are stored in the local office and
electronic data is stored on the CXO server.
Metallic Lithium percent was multiplied by a conversion factor of
2.1527/10000 to report Li ppm as Li2O%.
Differential GPS has been used to determine the majority of collar
locations, including RL. Some of the 2024 drilling remains to be surveyed
and hand-held GPS coordinates were used. Collar position audits are
undertaken, and no issues have arisen.
The grid system is MGA_GDA94, zone 52 for easting, northing and RL.
All RC hole traces were surveyed by north seeking gyro tool operated by
the drillers.
The local topographic surface is used to generate the RL of collars when
coordinates are obtained via handheld GPS.
The lithium mineralisation and geology show good continuity from hole to
hole at the more heavily drilled prospects and will be sufficient to support
the definition of a Mineral Resource and the classifications contained in
the JORC Code (2012 Edition).
Most mineralised intervals reported are based on a one metre sample
interval.
Drilling traverses were planned to be oriented approximately perpendicular
to the interpreted strike of mineralization (pegmatite body) as mapped.
Because of the dip of the hole, drill intersections are apparent thickness
and overall geological context is needed to estimate true thickness.
Estimates of true thickness are between 50-90%.
No sampling bias is believed to have been introduced.
Sample security was managed by the CXO. After preparation in the field
or CXO’s warehouse, samples were packed into polyweave bags and
transported by a freight transport company directly to the assay laboratory.
The assay laboratory audits the samples on arrival and reports any
discrepancies back to the Company. No such discrepancies occurred.
No audits or reviews of the techniques or data associated with the drilling
reported have occurred.
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Section 2 Reporting of Exploration Results
(Criteria listed in the preceding section also apply to this section.)
Criteria
JORC Code explanation
Commentary
Mineral
tenement
and land
tenure status
•
Type, reference name/number, location and ownership
including agreements or material issues with third
parties such as joint ventures, partnerships, overriding
royalties, native title interests, historical sites,
wilderness or national park and environmental settings.
The security of the tenure held at the time of reporting
along with any known impediments to obtaining a
licence to operate in the area.
•
Acknowledgment and appraisal of exploration by other
parties.
•
•
Exploration
done by
other parties
•
•
•
•
•
•
•
•
•
•
•
•
•
•
•
Drilling took place on EL29698, EL31126, EL30012 and MLN1148 which
are 100% owned by CXO.
There are no registered native title interests covering the areas being
drilled.
Across the tenure there are known Aboriginal sacred sites as well as
archaeological and heritage sites. Disturbance of these are avoided.
The tenements are in good standing with the NT DIPR Titles Division.
The areas being drilled comprises predominantly Vacant Crown land and
to a lesser extent Crown Leases (perpetual and term) as well as minor
Freehold private land.
The history of mining in the Bynoe area dates back to 1886 when tin was
discovered by Mr. C Clark.
By 1890 the Leviathan Mine and the Annie Mine were discovered and
worked discontinuously until 1902.
In 1903 the Hang Gong Wheel of Fortune was found, and 109 tons of tin
concentrates were produced in 1905. In 1906, the mine produced 80 tons
of concentrates.
By 1909 activity was limited to Leviathan and Bells Mona mines in the
area with little activity in the period 1907 to 1909.
The records of production for many mines are not complete, and in
numerous cases changes have been made to the names of the mines and
prospects which tend to confuse the records still further. In many cases
the published names of mines cannot be linked to field occurrences.
In the early 1980s the Bynoe Pegmatite field was reactivated during a
period of high tantalum prices by Greenbushes Tin which owned and
operated the Greenbushes Tin and Tantalite (and later spodumene) Mine
in WA. Greenbushes Tin Ltd entered into a JV named the Bynoe Joint
Venture with Barbara Mining Corporation, a subsidiary of Bayer AG of
Germany.
Greenex (the exploration arm of Greenbushes Tin Ltd) explored the Bynoe
pegmatite field between 1980 and 1990 and produced tin and tantalite
from its Observation Hill Treatment Plant between 1986 and 1988.
They then tributed the project out to a company named Fieldcorp Pty Ltd
who operated it between 1991 and 1995.
In 1996, Julia Corp drilled RC holes into representative pegmatites in the
field, but like all their predecessors, did not assay for Li.
Since 1996 the field has been defunct until recently when exploration has
begun ascertaining the lithium prospectivity of the Bynoe pegmatites.
The NT geological Survey undertook a regional appraisal of the field,
which was published in 2004 (NTGS Report 16, Frater 2004).
10
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Criteria
JORC Code explanation
Commentary
•
•
•
Geology
•
Deposit type, geological setting and style of
mineralisation.
•
•
•
Drill hole
Information
•
•
Data
aggregation
methods
•
•
A summary of all information material to the
understanding of the exploration results including a
tabulation of the following information for all Material
drill holes:
o easting and northing of the drill hole collar
o elevation or RL (Reduced Level – elevation
above sea level in metres) of the drill hole
collar
o dip and azimuth of the hole
o down hole length and interception depth
o hole length.
If the exclusion of this information is justified on the
basis that the information is not Material and this
exclusion does not detract from the understanding of
the report, the Competent Person should clearly
explain why 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.
Where aggregate intercepts incorporate short lengths
of high-grade results and longer lengths of low-grade
results, the procedure used for such aggregation
•
•
•
•
•
LTR drilled the first deep RC holes at BP33, Hang Gong and Booths in
2016, targeting surface workings dating back to the 1980s. The operators
at that time were seeking Tin and Tantalum.
CXO subsequently drilled BP33, Grants, Far West, Central, Ah Hoy and
several other prospects in 2016.
After purchase of the Liontown tenements in 2017, CXO drilled Lees,
Booths, Carlton and Hang Gong.
The CXO tenure covers a complex zoned rare element pegmatite field,
which comprises the 55km long by 10km wide West Arm – Mt Finniss
pegmatite belt (Bynoe Pegmatite Field; NTGS Report 16).
The Finniss pegmatites have intruded early Proterozoic shales, siltstones
and schists of the Burrell Creek Formation which lies on the northwest
margin of the Pine Creek Geosyncline. To the south and west are the
granitoid plutons and pegmatitic granite stocks of the Litchfield Complex.
The source of the fluids that have formed the intruding pegmatites is
generally accepted as being the Two Sisters Granite to the west of the
belt, and which probably underlies the entire area at depths of 5-10 km.
Lithium mineralisation has been identified historically as occurring at
Bilatos (Picketts) and Saffums 1 but more recently LTR and CXO have
identified spodumene at numerous other prospects, including Grants,
BP33, Booths, Lees, Hang Gong, Ah Hoy, Far West Central and Sandras.
A summary of material information for all drill holes discussed in this
release is contained within the body of the report. This includes all collar
locations, hole depths, dip and azimuth as well as current assay or
intercept information.
Only drill holes with assays returned are discussed and presented here.
Any sample compositing reported here is calculated via length weighted
averages of the 1 m assays. Length weighted averages are acceptable
method because the density of the rock (pegmatite) is constant.
0.3% Li2O was used as lower cut off grades for compositing and reporting
intersections with allowance for including up to 3m of consecutive drill
material of below cut-off grade (internal dilution).
No metal equivalent values have been used or reported.
11
corelithium.com.au
Criteria
JORC Code explanation
•
Relationship
between
mineralisatio
n widths and
intercept
lengths
•
Diagrams
•
Balanced
reporting
•
Other
substantive
exploration
data
•
Further work
•
•
•
•
should be stated and some typical examples of such
aggregations should be shown in detail.
The assumptions used for any reporting of metal
equivalent values should be clearly stated.
These relationships are particularly important in the
reporting of Exploration Results.
If the geometry of the mineralisation with respect to the
drill hole angle is known, its nature should be reported.
If it is not known and only the down hole lengths are
reported, there should be a clear statement to this
effect (e.g. ‘down hole length, true width not known’).
Appropriate maps and sections (with scales) and
tabulations of intercepts should be included for any
significa
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