Chairlift Kaolin Deposit Mineral Resource Estimate
Released
Released
Announcement PDF
16 November 2023
Andromeda Metals Limited ASX: ADN
ASX Announcement
10/431 King William Street
Adelaide, SA 5000
Tel:+61 8 7089 9800
admin@andromet.com.au
ABN
75 061 503 375
Chairlift Kaolin Deposit Mineral Resource Estimate
Andromeda Metals Limited (ASX: ADN) (Andromeda, the Company) is pleased to announce an
inaugural Mineral Resource Estimate (MRE) reported in accordance with the 2012 JORC Code
and Guidelines has been completed for the Chairlift kaolin deposit in South Australia. 1
Highlights
•
•
•
A combined Inferred Resource of 53.5 million tonnes (Mt) of kaolin comprised of:
o
27.0 Mt of Bright White, low titanium kaolinised granite (Chairlift CRM); and,
o
26.5 Mt of rheology modifier kaolin (Chairlift HRM).
The low titanium content of Chairlift CRM, with average TiO2 of 0.18%:
o
compliments that of the Great White Deposit’s kaolin;
o
is perfectly suited for the high-quality porcelain ceramics market2; and
o
is a potential additive and/or modifier for the high end coatings market.
Chairlift HRM has the same rheological properties as Great White HRM™, expanding the
potential market opportunities for the HRM product range.
•
The HRM “Rheology Index” methodology for determining the rheology modifying potential
of kaolin, is propriety to, and developed by, Andromeda.
•
Exploration upside potential, with mineralisation open in multiple directions.
Bob Katsiouleris, Andromeda’s CEO and Managing Director, said: “The Chairlift Deposit adds to
the number of high quality resources now surrounding The Great White Project, further cementing
the global significance of the region for high quality kaolin products.
“These resources significantly expand the potential market opportunities for Andromeda in the
high-end porcelain ceramics and low-carbon concrete markets, further supporting the long-term
benefits and future expansion opportunities of the planned development of The Great White
Project.
In addition, The Chairlift Deposit has the potential to further expand Andromeda’s participation
in the fast-growing, high-end market segments for white minerals, such as performance coatings
and pharmaceuticals.”
1
Chairlift is located on exploration license EL 6664 and is part of the Eyre Kaolin Project. Andromeda is currently sole funding
expenditure on the Eyre Kaolin Project to earn up to an 80% interest from Peninsula Exploration Pty Ltd. Refer ADN ASX
announcement dated 12 August 2021 titled Andromeda enters New Kaolin Joint Venture on the Eyre Peninsula, SA.
2
Subject to end-use customer validation and homologation test work.
Discussion
Andromeda Metals Limited is pleased to report the inaugural Chairlift Mineral Resource Estimate (MRE)
reported in accordance with the 2012 JORC Code and Guidelines.
The Chairlift Deposit is located on exploration license EL 6664 and lies 61 km to the southeast of the Great
White Deposit and 30 km southwest of Wudinna on the Eyre Peninsula of South Australia. Andromeda is
currently sole funding expenditure to earn up to an 80% interest in the Eyre Kaolin Project from Peninsula
Exploration Pty Ltd (Peninsula)3.
Figure 1: Great White Project and EKJV tenements
New 2012 JORC Mineral Resource Estimate Summary
An Inferred Mineral Resource Estimate for the Chairlift Deposit of 53.5Mt of kaolinised granite reported at
an ISO brightness (R457) cut-off of 75 in the <45 µm size fraction is shown in Table 1 below. The Resource
comprises of 27.0 Mt of Chairlift CRM, a low iron and low titanium kaolin suitable for use in high end
ceramics, and 26.5 Mt of Chairlift HRM, a rheology modifier targeted for use in cementitious construction
products and other industrial applications where solid matter needs to be suspended & stabilised.
Chemical analyses and brightness for Chairlift HRM are only reported for completeness. Properties normally
considered deleterious to kaolinite such as high iron and titanium, or low brightness have no effect on the
performance of Chairlift HRM.
For HRM (whether from Chairlift or Great White) the only number of
3
Refer ADN ASX announcement dated 12 August 2021 titled Andromeda enters New Kaolin Joint Venture on the Eyre
Peninsula, SA.
Andromeda Metals Limited | 2
significance is the “Rheology Index”, determined using a propriety Andromeda methodology, is a measure
of the rheology modifying potential of the kaolin.
Table 1 – Chairlift Kaolin Mineral Resource
PSD <45µm
%
Kaolinite
%
27.0
49.2
45
Chairlift HRM
26.5
51.6
47
Total
53.5
50.4
46
Product
Mt
Chairlift CRM
Note that all figures are rounded to reflect appropriate levels of confidence.
The MRE yields 26.9 Mt of kaolin product in the <45 µm recovered fraction, with the remaining approximate
49.6 % of material being largely residual quartz derived from the weathered granite. The MRE contains 13.3
Mt of <45 µm with an ISO B of 82.8 suitable for Chairlift CRM (refer Table 2), and an additional 13.7 Mt of
<45 µm suitable for Chairlift HRM.
Table 2 – Chairlift Kaolin Mineral Resource
Kaolinite
Product
Mt
Brightness
+
Al2O3
Fe2O3
TiO2
Rheology
<45µm
ISO B
Halloysite
%
%
%
RI
%
Chairlift CRM
13.3
82.8
91.0
36.6
0.50
0.18
-
Chairlift HRM
13.7
81.0
91.0
36.8
0.74
0.18
7.9
Total
26.9
81.9
91.0
36.7
0.62
0.18
-
Note that all figures are rounded to reflect appropriate levels of confidence.
The Chairlift MRE’s Chairlift CRM component compares favourably with and compliments the 2020 Great
White MRE4.
Table 3 – 2023 Chairlift kaolin MRE compared to 2020 Great White kaolin MRE
Kaolinite
Product
Mt
Brightness
+
Al2O3
Fe2O3
TiO2
<45µm
ISO B
Halloysite
%
%
%
%
Chairlift CRM
13.3
82.8
91.0
36.6
0.50
0.18
Great White
17.4
83.2
92.0
36.5
0.5
0.5
Note that all figures are rounded to reflect appropriate levels of confidence.
Eyre Kaolin Project Joint Venture Terms
The binding Heads of Agreement (HOA) with private entity Peninsula Exploration Pty Ltd (Peninsula) formed
the Eyre Kaolin Project Joint Venture 5. Peninsula holds title to four exploration licences that cover 2,799
4
Refer ADN ASX announcement dated 26 November 2020 Updated Mineral Resource for the Great White Kaolin JV Deposit.
Refer ADN ASX announcement dated 12 August 2021 titled Andromeda enters New Kaolin Joint Venture on the Eyre
Peninsula, SA.
5
Andromeda Metals Limited | 3
square kilometres located on the Eyre Peninsula of South Australia and which are adjacent to, or in close
proximity to, tenements that comprise The Great White Project (TGWP).
Andromeda can earn up to an 80% interest in the EKJV tenements through sole funding expenditure of
$2.75 million over 6 years from the commencement of the Joint Venture.
The principal terms of the Farm-in and Joint Venture Heads of Agreement are as follows:
•
Andromeda to make an initial payment to Peninsula of $20,000 upon execution of the HOA
•
A minimum expenditure requirement of $140,000 (exclusive of tenement rents) to be spent by
Andromeda on the Project tenements within 12 months of commencement of the EKJV
•
Stage 1 expenditure obligation by Andromeda of $750,000 (exclusive of tenement rents and which
is inclusive of the minimum expenditure requirement) within 3 years of commencement to earn a
51% interest in the EKJV (Stage 1 commitment)
•
Andromeda can elect to sole fund an additional $2 million over a further 3 years on meeting Stage
1 to earn an additional 29% interest, taking its overall interest in the EKJV to 80% (Stage 2
commitment)
•
If a JORC 2012 compliant Measured and Indicated Resource of at least 50Mt (with a minimum of
80 ISO Brightness and maximum total 1wt% Fe2O3 + TiO2 calculated from the -45um fraction) is
calculated over the EKJV tenements, Andromeda will issue Peninsula with $500,000 worth of ADN
shares, and
•
Peninsula has the option to convert its remaining interest of 20% into a 1.5% net profit royalty
following a Decision to Mine. If Peninsula elects not to convert its Participating Interest, or fails to
exercise its option within 10 business days, the parties are required to negotiate a good faith
production joint venture agreement and the production area relevant to the Decision to Mine will
be excised from the Joint Venture.
Mineral Resource Detail
The 2023 Chairlift Resource Estimate is based on exploration undertaken by Andromeda in 2022 and 2023.
The drilling and sampling procedures were the same used for the Great White Kaolin Deposit which were
reviewed by H&S Consultants and assessed as having no obvious issues.
All drillhole data used for the MRE is contained in an announcement lodged with ASX by Andromeda on
29 November 2022 and titled “Exploration Target Defined for Chairlift and Extensive High-Halloysite
intercepts at Halfpipe” and in Appendix 1 and Appendix 2 of this report.
Andromeda has completed 59 rotary air blast (RAB)/aircore (AC) drill holes (1,737.3 metres). All 59 drillholes
were drilled vertically to intersect the flat-lying mineralisation at right angles with most holes intersecting the
upper (hanging wall) and lower (footwall) contacts to the mineralisation.
The Company’s composited samples were wet sieved at Bureau Veritas S.A. (BV) in Adelaide to determine
percentage passing <45µm, with the recovered material then analysed by BV using their XRF 4B method
to determine elements that include Al2O3, Fe2O3, and TiO2.
Brightness on the <45 µm material was
determined by Andromeda staff at an enclosed laboratory room at the Streaky Bay pilot plant using a
Technidyne Colourtouch CT-PC Spectrophotometer in accordance with Tappi standard T534 om-15.
Additional spectrometry mineral analyses and rheology index (RI) measurements were undertaken inhouse using proprietary methods.
The MRE covers two areas separated by a palaeo channel that drains to the northwest. The western part
of the deposit covers an area of approximately 1.9 km E-W by 1.9 km N-S and remains open to the west
and to the south with a thickness ranging from 2 m to 12 m with an average thickness of 6.6 m and depth
Andromeda Metals Limited | 4
of 11.6 m. The eastern part of the deposit covers an area of approximately 1.1 km E-W by 3.9 km N-S and
is largely constrained by current drilling with a thickness ranging from 2 m to 23 m with an average thickness
of 7.9 m and depth of 12.3 m.
A plan view of the geological interpretation for the kaolin body is shown in Figures 2 and 3 and structure
contours of the top of the kaolin mineralisation showing the thickness of the kaolin is shown in Figure 3.
Overburden, which has an average thickness of 12.0 m consists of a thin soil layer which overlies a mixed
sequence of alluvial clays, sands and gravels. On occasions the top of the kaolin is silicified and the base
of silicification marks the top of the kaolin resource whilst the change in weathering intensity marks the base
of the kaolin resource.
Figure 2: Block model coloured by ISO B, drill collars and kaolin thickness contours (GDA 94 MGA 53)
Andromeda Metals Limited | 5
Figure 3: Block model coloured by RI, drill collars and cover depth contours (GDA 94 MGA 53)
The drilling and sampling procedures and analytical methods implemented by Andromeda were the same
used for the Great White Kaolin Deposit at Poochera which had been reviewed by H&S Consultants (2019)
and assessed as having no obvious issues with the sampling or analysis of the data. Composite intervals
were extracted from the drillhole database constrained by the kaolin wireframes. Grade interpolation of
the kaolinite was completed for the minus 45 micron recovered material, along with ISO B, Al 2O3, Fe2O3,
and TiO2 and RI, all obtained on the minus 45-micron fraction. Statistical analysis of the composite data
was undertaken and showed reasonably well-structured data with low coefficients of variation, all of which
resulted in no top cuts being applied.
Inverse distance squared (ID2) was chosen as the most appropriate method for the grade interpolation.
Maptek’s Vulcan software was used for modelling and the grade interpolation which used a two-pass
search domain of 500m by 500m by 5m followed by a 750 m by 750 m second pass. Parent block size was
100m by 100m by 2.5m (X, Y & Z), with 25m by 25m by 1.25 m sub-blocking. Three wireframes were used to
define the kaolinised granite (upper and lower saprolite) within the mineralised zone. These wireframes
were also used for the “Bend Unfolding Model”. Other wireframes were used to map out geological
boundaries above the mineralised zones, but these have no impact on the resource.
Resource classification of Inferred was based on internal blocks populated by a single interval within 200m
of a hole that intersected potentially economic mineralisation such that the Inferred classification extends
no further than 200m past the outer limit holes.
Andromeda Metals Limited | 6
Block model validation consisted of a visual comparison of block grades with drillhole assays and
composite values and a review of the summary statistics for the block grades and composite values.
No density measurements have been determined on the Chairlift kaolin. For the MRE a density of 1.46 t/m3
was used which is the average dry bulk density of kaolin from the Great White deposit.
The triangulations that define the mineralisation were based off the lithological units but upper and lower
extents of the saprolite were restricted to an ISO B of >75%. Blocks with <0.6 % Fe2O3 were assigned as
CRM, the details for the Chairlift CRM upper and lower saprolite, by domain, are reported below in Tables
4 and 5.
Table 4 – Chairlift CRM comparison by domain between Upper and Lower Saprolite
Chairlift CRM
Mt
<45 µm (%)
Kaolinite (%)
Upper saprolite - west
10.01
52.3
49
Upper saprolite - east
10.60
50.9
47
Upper saprolite - all
20.61
51.6
48
Lower saprolite - west
5.15
39.6
33
Lower saprolite - west
1.25
49.1
43
Lower saprolite - west
6.39
41.5
35
Chairlift CRM total
27.00
49.2
45
Note that all figures are rounded to reflect appropriate levels of confidence.
Table 5 – Chairlift CRM comparison by domain between Upper and Lower Saprolite in the <45µm
Kaolinite
Chairlift CRM
Mt
Brightness
+
Al2O3
Fe2O3
TiO2
Rheology
<45µm
ISO B
Halloysite
%
%
%
RI
%
Upper saprolite - west
5.23
94.0
83.3
37.5
0.48
0.19
-
Upper saprolite - east
5.40
92.0
82.5
36.8
0.5
0.16
-
Upper saprolite - all
10.63
93.0
82.9
37.2
0.49
0.18
-
Lower saprolite - west
2.04
83.0
82.5
34.8
0.52
0.21
-
Lower saprolite - west
0.61
87.0
82.2
35.9
0.48
0.2
-
Lower saprolite - west
2.65
84.0
82.4
35
0.51
0.21
-
Chairlift CRM total
13.28
91.0
82.8
36.6
0.5
0.18
-
Note that all figures are rounded to reflect appropriate levels of confidence.
Of the remaining blocks, those with >6.0 RI were assigned as HRM, the details for the Chairlift HRM by
domain, are reported below in Tables 6 and 7.
Table 6 – Chairlift HRM by domain
Chairlift HRM
Mt
<45 µm (%)
Kaolinite (%)
Chairlift HRM - west
20.61
51.8
47
Chairlift HRM - east
5.85
50.6
46
Chairlift HRM total
26.46
51.6
47
Note that all figures are rounded to reflect appropriate levels of confidence.
Table 7 – Chairlift HRM by domain in the <45µm
Andromeda Metals Limited | 7
Kaolinite
Chairlift HRM
Mt
Brightness
+
Al2O3
Fe2O3
TiO2
Rheology
<45µm
ISO B
Halloysite
%
%
%
RI
%
Chairlift HRM - west
10.7
91.0
81.3
36.7
0.75
0.18
8.1
Chairlift HRM - east
3.0
91.0
80.2
36.8
0.71
0.16
7.1
Chairlift HRM total
13.7
91.0
81
36.8
0.74
0.18
7.9
Note that all figures are rounded to reflect appropriate levels of confidence.
Comparison between the 2022 Exploration Target and the 2023 MRE
The 2022 Exploration Target6 of 80-120Mt of High Bright White kaolin with an ISO B in the range of 80 to 84 in
the <45 µm fraction was based off 8 mineralisation intersecting aircore drillholes. The 2023 MRE in
comparison comprises of 53.5 Mt with an ISO B of 81.9. Additional exploration potential remains at Chairlift,
particularly extension to the east and the south and to the west of CH22AC016 (from 12m, 10m @ 85.0),
located on Figure 2.
Next Step
Future work to upgrade the resource estimation category will require additional drilling to reduce the
drillhole spacings, obtain more samples for dry bulk density determinations and undertake hydrogeological
studies.
This announcement has been approved for release by the Board of Directors of Andromeda Metals Limited.
For more information about the Company and its projects, visit our website www.andromet.com.au or
contact:
Manager, Investor Relations & Corporate Affairs
Patrick Sinclair
T: 08 7089 9819
M: 0403 708 431
E: Patrick.Sinclair@andromet.com.au
Competent Persons Statement
The data that relates to exploration results and Mineral Resource Estimates are based on information
compiled and evaluated by Mr. Eric Whittaker who is a Member of the Australasian Institute of Mining
and Metallurgy (MAusIMM). Mr. Whittaker is the Chief Geologist of Andromeda Metals Limited and has
sufficient experience relevant to the style of mineralisation and type of deposit 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”). Mr. Whittaker has over 30 years of experience in the mining industry. Mr. Whittaker
consents to the information in the form and context in which it appears.
6
Refer ADN ASX announcement dated 29 November 2022 titled Exploration Target Defined for Chairlift and Extensive HighHalloysite intercepts at Halfpipe.
Andromeda Metals Limited | 8
APPENDIX 1 –CHAIRLIFT AIRCORE DRILL COLLARS
Hole ID
Easting
(MGA94 Z53)
Northing
(MGA94 Z53)
Collar RL
(m)
Hole
Inclination
Hole
Azimuth
Final
Depth (m)
Domain
CH22AC001
519,702.46
6,324,066.56
90.151
-90
0
44
East
CH22AC002
519,104.29
6,325,522.18
103.966
-90
0
23.5
East
CH22AC003
519,600.64
6,325,459.37
116.556
-90
0
27
East
CH22AC004
519,806.11
6,326,197.21
107.791
-90
0
25
CH22AC005
520,188.35
6,325,314.81
117.078
-90
0
5
CH22AC006
520,619.53
6,325,263.28
98.892
-90
0
36
CH22AC007
519,905.88
6,324,879.44
113.287
-90
0
24
CH22AC008
518,995.46
6,324,723.26
99.166
-90
0
26
CH22AC009
518,099.44
6,325,816.04
93.122
-90
0
33
CH22AC010
518,251.72
6,326,757.01
99.789
-90
0
21
CH22AC011
517,151.92
6,325,979.90
85.392
-90
0
45
CH22AC012
516,044.17
6,326,065.23
87.915
-90
0
58
CH22AC013
515,368.99
6,326,711.64
82.826
-90
0
45
CH22AC014
516,135.37
6,327,501.49
72.801
-90
0
47
CH22AC015
516,683.72
6,328,062.80
81.538
-90
0
46
CH22AC016
517,150.87
6,328,547.44
85.23
-90
0
26
CH22AC017
518,104.70
6,328,497.97
83.46
-90
0
42
CH22AC018
519,153.84
6,327,642.17
87.02
-90
0
35
CH22AC019
519,852.18
6,327,064.51
97.925
-90
0
27
CH22AC020
520,023.21
6,327,904.98
91.665
-90
0
46
CH22AC021
519,469.66
6,324,632.48
102.476
-90
0
38
CH22AC022
518,482.28
6,323,461.06
111.863
-90
0
17
CH22AC023
517,589.14
6,323,317.31
107.346
-90
0
20
CH22AC024
518,510.57
6,325,342.47
95.795
-90
0
39
CH22AC025
518,326.80
6,324,930.43
95.955
-90
0
30
CH22AC026
517,026.53
6,323,967.41
106.139
-90
0
25
West
CH22AC027
515,892.61
6,324,128.91
91.304
-90
0
28
West
CH22AC028
517,850.61
6,329,331.35
81.753
-90
0
17
CH23AC001
519,670.44
6,323,584.77
79.53
-90
0
31
CH23AC002
520,275.59
6,323,998.94
82.347
-90
0
22.5
CH23AC003
519,953.33
6,324,501.82
105.684
-90
0
34
CH23AC004
520,448.71
6,324,590.33
95.665
-90
0
18
CH23AC005
519,776.03
6,325,862.57
115.912
-90
0
13
CH23AC006
519,044.36
6,326,018.60
103.621
-90
0
35
East
CH23AC007
519,161.16
6,326,547.04
98.69
-90
0
36
East
CH23AC008
518,099.63
6,326,367.68
90.081
-90
0
25
East
CH23AC009
518,408.68
6,327,154.32
102.055
-90
0
15
East
CH23AC010
518,575.59
6,327,562.24
90.755
-90
0
18.1
East
CH23AC011
517,806.78
6,327,589.85
85.8
-90
0
31
CH23AC012
517,247.42
6,328,051.76
84.788
-90
0
40
CH23AC013
517,591.42
6,326,995.02
89.47
-90
0
39
CH23AC014
519,398.25
6,325,028.89
108.878
-90
0
29
East
CH23AC015
518,996.24
6,325,200.61
102.113
-90
0
28
East
CH23AC016
518,995.26
6,323,931.22
99.664
-90
0
24
East
East
East
East
East
Andromeda Metals Limited | 9
Hole ID
Easting
(MGA94 Z53)
Northing
(MGA94 Z53)
Collar RL
(m)
Hole
Inclination
Hole
Azimuth
Final
Depth (m)
Domain
CH23AC017
517,408.75
6,324,236.10
104.427
-90
0
21
West
CH23AC018
516,666.76
6,324,147.40
103.509
-90
0
21.2
West
CH23AC019
516,275.26
6,324,351.66
99.953
-90
0
24
West
CH23AC020
515,926.01
6,324,533.03
94.111
-90
0
21
CH23AC021
516,287.82
6,324,003.90
97.184
-90
0
21
West
CH23AC022
515,863.90
6,323,273.96
105.273
-90
0
33
West
CH23AC023
515,847.07
6,323,663.64
94.947
-90
0
31
West
CH23AC024
516,844.27
6,323,739.95
102.82
-90
0
34
West
CH23AC025
516,533.26
6,323,326.74
100.916
-90
0
37
West
CH23AC026
516,201.48
6,323,235.15
103.931
-90
0
20
West
CH23AC027
516,192.73
6,323,520.24
97.348
-90
0
33
West
CH23AC028
516,472.61
6,323,656.89
96.95
-90
0
27
West
CH23AC029
516,598.33
6,323,921.01
100
-90
0
26
West
CH23AC030
516,951.26
6,323,173.60
100.781
-90
0
29
West
CH23AC031
516,628.56
6,324,641.84
101.565
-90
0
25
West
Andromeda Metals Limited | 10
APPENDIX 2 – CHAIRLIFT AIRCORE DRILL CHEMISTRY RESULTS
Hole ID
From (m)
To (m)
Interval (m)
<45µm
(%)
Kaolinite +
Halloysite
ISO B (%)
Al2O3
(%)
Fe2O3
(%)
TiO2 (%)
(%)
Rheology
(RI)
CH22AC001
19
24
5
55.7
93
82.2
37.5
0.6
0.18
8.9
CH22AC001
24
25
1
55.9
90
70.8
36.4
1.3
0.17
6.6
CH22AC001
25
30
5
50.1
91
79.3
37
0.96
0.21
8
CH22AC001
30
35
5
53.4
91
81.7
36.9
0.8
0.16
7.3
CH22AC001
35
37
2
52.1
91
84.7
37.1
0.67
0.2
5.9
CH22AC001
37
41
4
45.5
87
84.3
36.6
0.66
0.18
6.8
CH22AC001
41
42
1
41
78
80.7
34.5
0.68
0.24
4
CH22AC002
9
14
5
47.6
92
86.2
37.3
0.3
0.26
2.4
CH22AC002
14
17
3
57.2
93
87.3
38
0.27
0.23
2.9
CH22AC002
17
20
3
39.9
79
76.7
35.1
0.57
0.23
1.2
CH22AC003
11
16
5
41.3
88
77.9
35.3
0.73
0.15
3.9
CH22AC003
16
20
4
48.4
84
85.7
36
0.56
0.17
6.6
CH22AC003
20
25
5
28.4
77
81.7
34.2
0.79
0.25
2.6
CH22AC004
11
15
4
22.7
75
68
30.2
0.94
0.28
0
CH22AC004
15
20
5
27.1
74
81.3
31.8
0.75
0.28
0.1
CH22AC004
20
24
4
23.8
69
79.9
31.4
0.8
0.36
0.1
CH22AC007
9
11
2
30.6
77
78.5
30.9
0.53
0.22
0
CH22AC007
11
16
5
36.9
86
83.4
34.7
0.61
0.24
1.6
CH22AC007
16
20
4
43.8
84
84.6
35.6
0.7
0.27
3.3
CH22AC010
8
12
4
50.4
94
83.5
37.8
0.43
0.19
3.2
CH22AC010
12
14
2
48.1
94
77.9
37.6
0.42
0.19
0.9
CH22AC010
14
18
4
49.5
93
81.7
37.5
0.4
0.17
1.4
CH22AC011
21
23
2
52.9
90
70.8
36.5
0.59
0.38
1.7
CH22AC011
23
27
4
51.8
90
65.5
36.4
0.56
0.37
0.2
CH22AC011
27
30
3
53.1
91
69.5
36.9
0.67
0.2
0
CH22AC011
30
35
5
45.4
82
56
35.2
0.53
0.24
0
CH22AC011
35
40
5
29.9
65
52
30.9
0.86
0.33
0
CH22AC012
21
23
2
49.3
84
68.6
33.9
0.86
1.08
1.8
CH22AC012
23
28
5
49.9
91
71.3
37
0.57
0.27
6.1
CH22AC012
28
32
4
48.3
92
69.3
37.2
0.62
0.2
5.9
CH22AC012
32
36
4
46.5
92
65
37.5
0.43
0.24
4.1
CH22AC012
36
41
5
45.8
92
59.7
37.3
0.5
0.19
0.9
CH22AC012
41
45
4
37
84
52
35.8
0.5
0.15
0
CH22AC012
45
48
3
32.1
70
45.9
32.1
0.97
0.19
0
CH22AC012
48
52
4
29.1
70
48.3
31.8
1.16
0.27
0
CH22AC012
52
56
4
24.1
65
53.8
30.1
1.13
0.43
0
CH22AC013
26
31
5
44.5
90
59.1
36.1
0.44
0.52
0.7
CH22AC013
31
36
5
50.3
93
68.9
37.5
0.55
0.19
2.8
CH22AC013
36
40
4
41.9
81
68.8
35.2
0.69
0.17
2.3
CH22AC014
31
33
2
48.1
83
51.6
33.4
0.56
0.64
0
CH22AC014
33
37
4
52.6
92
66.6
37.1
0.65
0.27
1.8
CH22AC014
37
40
3
47.4
93
52.4
37.4
0.53
0.2
0
CH22AC014
40
44
4
47.6
91
51.2
37.1
0.54
0.21
0
Andromeda Metals Limited | 11
Hole ID
From (m)
To (m)
Interval (m)
<45µm
(%)
Kaolinite +
Halloysite
ISO B (%)
Al2O3
(%)
Fe2O3
(%)
TiO2 (%)
(%)
Rheology
(RI)
CH22AC015
21
24
3
45.4
88
75.9
35.3
0.66
0.35
7.1
CH22AC015
24
26
2
46.3
87
71.3
35.7
0.83
0.26
4.8
CH22AC015
26
31
5
46.6
90
67.9
36.6
0.72
0.26
5.6
CH22AC015
31
35
4
47.8
90
69.8
36.7
0.63
0.27
5.5
CH22AC015
35
40
5
37.5
78
70.7
34.6
0.67
0.28
4.3
CH22AC015
40
42
2
30.7
73
54.4
33
0.8
0.37
0
CH22AC016
13
17
4
53.5
95
86.8
38.1
0.45
0.15
0
CH22AC016
17
20
3
54.8
95
85.8
38.2
0.45
0.14
0
CH22AC016
20
23
3
41.1
83
81.9
35.8
0.52
0.19
5.6
CH22AC017
30
32
2
31.5
70
49
31.5
1.06
0.35
2.7
CH22AC017
32
36
4
31.6
70
42.4
32.1
1.01
0.32
6.7
CH22AC017
36
38
2
22.6
72
46
32.1
1.08
0.21
5.3
CH22AC018
17
22
5
54.5
91
68.6
36.7
0.65
0.25
5.6
CH22AC018
22
25
3
53.8
92
49.9
37.2
0.55
0.15
5.6
CH22AC018
25
29
4
43.7
83
50.1
35.7
0.44
0.15
5.6
CH22AC018
29
30
1
25.2
78
60.4
34.6
0.43
0.16
5.6
CH22AC018
30
32
2
35.5
81
61.3
35.2
0.6
0.18
1.8
CH22AC020
28
31
3
48
87
46.3
35.5
0.76
0.67
0.8
CH22AC020
31
36
5
42.3
78
42
34.1
0.78
0.44
0.5
CH22AC020
36
40
4
30.6
72
48.1
32.9
0.95
0.36
0.1
CH22AC020
40
44
4
29.3
67
55
31.6
1.44
0.36
5.6
CH22AC021
10
14
4
49.3
95
80.1
37.8
0.56
0.16
6.5
CH22AC021
14
19
5
45
93
67.5
37.4
0.63
0.2
9.1
CH22AC021
19
21
2
45.8
94
67.6
37.7
0.55
0.21
9.4
CH22AC021
21
26
5
41
83
63.8
35.6
0.63
0.26
0.5
CH22AC021
26
31
5
35
75
65.4
33.8
0.66
0.26
0
CH22AC021
31
36
5
32.2
68
65.7
31.6
0.84
0.42
1.8
CH22AC022
8
10
2
32.6
82
66.2
33.5
1.03
0.36
0
CH22AC022
10
14
4
34
80
77.4
32.8
0.78
0.22
0.5
CH22AC022
14
15
1
31.6
73
75.3
31.5
0.72
0.28
2.1
CH22AC023
6
11
5
35.9
82
73.8
33.3
0.96
0.24
4
CH22AC023
11
14
3
35.4
78
79.2
32.5
0.97
0.19
5.4
CH22AC023
14
16
2
36.1
70
79.3
31.3
1.1
0.22
4.4
CH22AC023
16
18
2
29.6
70
58.4
31.9
1.96
0.2
5.4
CH22AC024
27
32
5
39.1
79
64.5
33.6
1.29
0.34
6.1
CH22AC024
32
36
4
33.6
71
69
32.5
0.83
0.37
4.9
CH22AC024
36
38
2
32
65
70.2
31
0.56
0.45
2.9
CH22AC025
20
24
4
40.4
74
55.2
33
1.59
0.22
3.4
CH22AC025
24
27
3
26.9
66
47.8
30.5
3
0.18
2
CH22AC026
9
13
4
49.4
94
83.7
37.7
0.52
0.15
3.6
CH22AC026
13
18
5
51.4
94
79.9
38.1
0.26
0.17
7.9
CH22AC026
18
21
3
36
81
82.9
35.3
0.42
0.24
5.2
CH22AC027
11
16
5
56.2
95
85.1
38
0.63
0.12
2.7
CH22AC027
16
18
2
51.2
93
85.3
37.7
0.5
0.13
0
Andromeda Metals Limited | 12
Hole ID
From (m)
To (m)
Interval (m)
<45µm
(%)
Kaolinite +
Halloysite
ISO B (%)
Al2O3
(%)
Fe2O3
(%)
TiO2 (%)
(%)
Rheology
(RI)
CH22AC027
18
20
2
39.4
82
85.3
35.3
0.56
0.17
0.1
CH22AC027
20
22
2
31.3
79
83.6
34.5
0.61
0.22
3.1
CH23AC003
10
12
2
50.8
88
74.55
35.3
1.05
0.21
0.2
CH23AC003
12
13
1
53.4
91
75.45
36.4
0.94
0.18
2
CH23AC003
13
18
5
56.8
94
83.98
37.6
0.71
0.16
7.8
CH23AC003
18
22
4
54.4
94
82.68
37.8
0.69
0.19
9.4
CH23AC003
22
24
2
57.9
95
77.02
38.1
0.58
0.14
7.3
CH23AC003
24
26
2
53.3
87
75.96
36.6
0.37
0.21
5.2
CH23AC003
26
28
2
58.6
94
70.57
38.5
0.51
0.18
6.6
CH23AC003
28
30
2
34.9
79
63.81
34.4
1.38
0.3
2.7
CH23AC006
20
22
2
49
85
70.05
34.5
1.24
0.4
1.9
CH23AC006
22
24
2
49.2
85
82.22
35.9
0.47
0.2
5.8
CH23AC006
24
26
2
36
78
77.55
34.3
0.73
0.22
4.4
CH23AC006
26
28
2
32.4
68
72.2
31.7
1
0.29
1.7
CH23AC006
28
30
2
29.1
63
69.91
30
1.14
0.32
0.2
CH23AC007
13
15
2
56.1
92
78.14
37
0.89
0.17
3.8
CH23AC007
15
18
3
51.7
93
74.64
37.5
0.49
0.15
5.1
CH23AC007
18
23
5
40.1
80
65.87
34.9
0.55
0.18
1.4
CH23AC007
23
28
5
28.7
61
69.74
30
0.73
0.33
1.1
CH23AC007
28
30
2
23.7
61
67.7
29.4
1.01
0.34
0.5
CH23AC007
30
32
2
19.7
57
67.58
28.1
0.96
0.36
0
CH23AC008
9
12
3
58
94
85.98
37.7
0.74
0.14
8.9
CH23AC008
12
15
3
50.1
93
82.74
37.3
0.92
0.19
13.6
CH23AC008
15
18
3
60.5
95
62.9
37.9
0.74
0.16
2.8
CH23AC008
18
19
1
55.6
95
66.46
38.1
0.41
0.16
3.3
CH23AC008
19
23
4
45.2
86
82.64
36.5
0.5
0.14
4.5
CH23AC009
5
6
1
37.7
76
59.4
30.5
1.59
0.25
0
CH23AC009
6
10
4
49.7
91
79.27
36.5
0.79
0.19
1.2
CH23AC010
10
12
2
57.2
93
82.49
37.1
0.49
0.19
6.9
CH23AC010
12
14
2
49.3
84
81.42
35.7
0.64
0.11
6.8
CH23AC010
14
18
4
34.5
73
78.73
33.3
0.72
0.16
4.6
CH23AC011
18
20
2
52.8
91
73.92
36.5
1.13
0.47
6.2
CH23AC011
20
22
2
46.7
80
72.33
34.8
1.05
0.21
3.7
CH23AC011
22
24
2
33.8
74
62.7
33.1
1.73
0.16
2.3
CH23AC011
24
27
3
25.8
70
70.19
32.1
0.92
0.2
1.2
CH23AC011
27
29
2
31.5
67
70.13
30.6
1.65
0.29
1
CH23AC011
29
30
1
27.2
41
57.61
21.7
1.42
0.16
0
CH23AC012
21
22
1
53.2
93
63.92
37.4
0.73
0.31
4.2
CH23AC012
22
27
5
49.7
87
54.5
35.1
2
0.96
4.6
CH23AC012
27
31
4
50.3
91
59.55
37.1
0.89
0.2
0
CH23AC012
31
35
4
46.6
91
46
36.9
0.79
0.15
0
CH23AC012
35
40
5
38.1
84
48.12
35.4
0.99
0.19
9.4
CH23AC013
21
24
3
55.7
90
75.51
36
1
0.31
1.5
CH23AC013
24
29
5
38.2
70
58.51
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