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METALLIUM LIMITED — Capital/Financing Update 2022
Nov 16, 2022
65382_rns_2022-11-16_cf70f4f1-b775-4ca1-9687-697bcc1fb9aa.pdf
Capital/Financing Update
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ASX Announcement
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ASX:MTM
17 November 2022
ASSAYS CONFIRM RARE EARTH ELEMENT MINERALISATION AND DISTRICT-SCALE POTENTIAL AT EAST LAVERTON
Highlights:
-
Results confirm that the broad rare earth element (REE) mineralisation at the Pt Kidman prospect near Laverton, WA contains a significant proportion of valuable heavy, magnet and critical rare earth oxides at clay thickness intervals up to 12m, including:
-
High value Nd+Pr oxides represent an average of 19% of TREO grade
-
High value magnet rare earth oxides represent an average 24% of TREO grade
-
Critical rare earth oxides (CREO) average 23% of TREO
-
Heavy rare earth oxides represent an average of 12% of TREO grade
-
Higher grade drilling intersections include:
-
22ELAC048 – 8m @ 1,467ppm TREO, from 22m & 5m @ 1,427ppm TREO, from 31m
-
22ELAC043 – 6m @ 1,880ppm TREO, from 12m
-
22ELAC023 – 3m @ 1,577ppm TREO, from 23m & 2m @ 1,191ppm TREO from 33m
-
22ELAC003 – 2m @ 1,806ppm TREO, from 27m
-
22ELAC046 – 1m @ 2,107ppm TREO, from 16m
-
Confirms REE grades and continuity of clay-hosted mineralisation
-
Large areas which remain untested are interpreted to be prospective for similar mineralisation occurrences
-
New aircore drilling program to test additional REE targets at Pt Kidman provisionally approved by the Traditional Owners of the area, pending site clearance process.
Mt Monger Resources Limited (ABN 27 645 885 463) Suite 2, 38 Colin Street, West Perth, 6005, Australia P: +61 (0)8 6391 0112, E: [email protected] www.mtmongerresources.com.au Follow us: Twitter - @MtMongerRes LinkedIn – Mt Monger Resources
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Mt Monger Resources Limited (ASX: MTM ) ( Mt Monger or the Company ) has received detailed 1 metre assay results from a recent program of aircore drilling completed to test rare earth element (REE) anomalies at the Pt Kidman prospect, part of the East Laverton Project in the north Eastern Goldfields of Western Australia (Figure 1). Results confirm the REE mineralisation contains a significant proportion of valuable heavy, magnet and critical rare earth oxides.
The Company has previously reported composite sample assay results for this drilling ( see Mt Monger ASX announcement dated 19 August 2022 ) which highlighted broad zones of shallow, flat-laying clay-hosted REE mineralisation. Assay of primary one metre RC drilling samples has confirmed and refined the intersections from the drill holes. A total of 280 new samples were assayed for a multi-element suite.
Regarding the latest results from the Pt Kidman prospect, Managing Director Lachlan Reynolds commented:
“These more detailed assays from the aircore drilling program confirm the presence of shallow, rare earth element mineralisation on our East Laverton project tenements. We are excited by the scale of this opportunity - the mineralisation potentially extends over a very large area, most of which is still untested by drilling.
We are also very pleased to see that the mineralisation ‘basket’ of elements contains a significant proportion of the higher-value heavy and critical rare earth elements. This is important for the potential viability of any new discovery and we are keen to do more work to home-in on the best parts of the system.”
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Figure 1: Summary of REE exploration results from the Pt Kidman Prospect showing areas of potential REE mineralisation based on available geochemical, geophysical and drilling data.
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The Pt Kidman area represents a potentially large-scale, rare earth element project at East Laverton. The current drilling program has only tested a small part of the prospective terrane but has shown significant continuity and grade within the mineralised zone within the regolith. Further aircore drilling is currently being planned to test these areas for additional zones of REE mineralisation.
Aircore Drilling Program
A total of 48 aircore drill holes were completed (see hole details in Appendix I and diagram of collar locations in Figure 1). The drilling was designed to test REE mineralisation which was known only from limited surface sampling and historical drill holes in the Pt Kidman area, approximately 30km northeast of Laverton.
Drilling successfully identified broad zones of shallow REE mineralisation hosted by saprolitic clays above interpreted fertile basement granitoids and gneissic rocks. On the basis of limited available historical exploration and similarities in the geological setting it is anticipated that additional zones of REE mineralisation will be intersected ( refer to Mt Monger ASX announcement dated 1 September 2022 ).
New Assay Results
Assay of the primary 1m drill samples has confirmed and provided better definition of the REE mineralisation intersections in the aircore drill holes. As anticipated, the new downhole intersections compare favourably with the original composite samples, though the intervals are typically slightly narrower and higher grade (see Appendix III).
Assays received have returned significant TREO grades and thickness using a 1,000ppm TREO cut-off grade with clay thickness intervals up to 12m. Overall, Magnet Rare Earth Oxides (MREO) make up an average of 24% of TREO, with Critical Rare Earth Oxides (CREO) averaging 23% and Heavy Rare Earth Oxides (HREO) averaging 12%.
Table 1: Selected significant REE intersections from the East Laverton AC drilling program.
| Hole ID | From (m) |
To (m) |
Interval (m) |
TREO (ppm) |
HREO (%) |
MREO (%) |
CREO (%) |
|---|---|---|---|---|---|---|---|
| 22ELAC003 | 27 | 29 | 2 | 1,806 | 13 | 31 | 28 |
| 22ELAC023 | 23 33 |
26 35 |
3 2 |
1,577 1,191 |
9 23 |
30 28 |
24 25 |
| 22ELAC026 | 18 | 20 | 2 | 1,136 | 13 | 27 | 25 |
| 22ELAC027 | 20 22 |
21 23 |
1 1 |
1,721 1,590 |
4 6 |
22 28 |
17 22 |
| 22ELAC031 | 16 | 17 | 1 | 1,021 | 12 | 25 | 23 |
| 22ELAC039 | 26 28 |
27 29 |
1 1 |
1,982 1,914 |
9 13 |
26 26 |
22 24 |
| 22ELAC040 | 25 | 27 | 2 | 1,726 | 29 | 35 | 38 |
| 22ELAC043 | 12 | 18 | 6 | 1,493 | 7 | 29 | 23 |
| 22ELAC046 | 16 | 17 | 1 | 2,107 | 3 | 22 | 16 |
| 22ELAC048 | 22 31 |
30 36 |
8 5 |
1,467 1,427 |
5 7 |
20 23 |
16 20 |
Downhole intervals shown, interpreted to be approximately true widths. Appropriate rounding of grade values has been applied. Significant intersections are based on a 1,000ppm TREO cut-off grade with no internal dilution.
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TREO (Total Rare Earth Oxide) grade includes CeO2, Dy2O3, Er2O3, Eu2O3, Gd2O3, Ho2O3, La2O3, Lu2O3, Nd2O3, Pr6O11, Sm2O3, Tb4O7, Tm2O3, Yb2O3 and Y2O3 and is calculated using standard oxide conversion factors for each element (see Appendix V).
HREO (Heavy Rare Earth Oxide) grade includes Eu2O3, Gd2O3, Tb4O7, Dy2O3, Ho2O3, Er2O3, Tm2O3, Yb2O3, Lu2O3 and Y2O3. Shown as percentage of TREO.
MREO (Magnet Rare Earth Oxide) grade includes Nd2O3, Pr6O11, Sm2O3, Gd2O3, Tb4O7, Dy2O3, and Ho2O3. Shown as percentage of TREO.
CREO (Critical Rare Earth Oxide) grade includes Nd2O3, Eu2O3, Tb4O7, Dy2O3 and Y2O3. Shown as % percentage of TREO
Further Work
The Company’s proposed drilling east of the Great Central Road at the Pt Kidman prospect (Figure 1) has been granted provisional approval by the Traditional Owners of the area, subject to an on-site clearance process. The approval allows the Company to progress its aircore drilling program to assess the distribution, grade and continuity of clay-hosted REE mineralisation within the weathering profile across the area. Planning for the drilling program is in progress.
End
This announcement has been authorised for release by the Board of Directors.
For further information, please contact:
Lachlan Reynolds Managing Director Mt Monger Resources Limited Tel: +61 (0)8 6391 0112 Email: [email protected]
Simon Adams Company Secretary Mt Monger Resources Limited Tel: +61 (0)8 6391 0112 Email: [email protected]
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About Mt Monger Resources Limited
Mt Monger Resources Limited is an exploration company searching for rare earth elements (REE), lithium, gold, nickel, and base metals in the Goldfields and Ravensthorpe districts of Western Australia. The Company holds over 4,500km[2] of tenements in three prolific and highly prospective mineral regions. The Mt Monger Gold Project comprises a contiguous area of ~120km[2] area containing known gold deposits occurrences in the Mt Monger area, located ~70km SE of Kalgoorlie and immediately adjacent to the Randalls gold mill operated by Silver Lake Resources Limited. The East Laverton Gold Project is a regionally extensive package of underexplored tenements prospective for gold, base metals and REE. The Ravensthorpe Project contains a package of tenements in the southern part of Western Australia between Esperance and Bremer Bay which are prospective for a range of minerals including lithium, REE, nickel and graphite. Priority drilling targets have been identified in all project areas and the Company is well funded to undertake effective exploration programs. The Company has an experienced Board and management team which is focused on discovery to increase value for Shareholders.
Competent Person’s Statement
The information in this announcement that relates to Exploration Results is based on and fairly represents information compiled by Mr Lachlan Reynolds. Mr Reynolds is the Managing Director of Mt Monger Resources Limited and is a member of both the Australasian Institute of Mining and Metallurgy and the Australasian Institute of Geoscientists. Mr Reynolds has sufficient experience of relevance to the styles of mineralisation and types of deposits under consideration, and to the activities undertaken, to qualify as a Competent Person as defined in the 2012 Edition of the Joint Ore Reserves Committee (JORC) Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves. Mr Reynolds consents to the inclusion in this announcement of the matters based on information in the form and context in which they appear.
Previous Disclosure
The information in this announcement is based on the following Mt Monger Resources Limited ASX announcements, which are available from the Mt Monger Resources website www.mtmongerresources.com.au and the ASX website www.asx.com.au.
-
19 August 2022, “Aircore Drilling Confirms Widespread REE Mineralisation at East Laverton”
-
1 September 2022, “Growing Potential for District-Scale REE Mineralisation System at East Laverton”
The Company confirms that it is not aware of any new information or data that materially affects the information included in the Prospectus or the original ASX announcements and that all material assumptions and technical parameters underpinning the Prospectus and relevant ASX announcements continue to apply and have not materially changed. The Company confirms that the form and context in which the Competent Person’s findings are represented have not been materially modified from the original ASX announcements.
Cautionary Statement Regarding Values & Forward-Looking Information
The figures, valuations, forecasts, estimates, opinions and projections contained herein involve elements of subjective judgment and analysis and assumption. Mt Monger Resources does not accept any liability in relation to any such matters, or to inform the Recipient of any matter arising or coming to the company’s notice after the date of this document which may affect any matter referred to herein. Any opinions expressed in this material are subject to change without notice, including as a result of using different assumptions and criteria. This document may contain forward-looking statements. Forward-looking statements are often, but not always, identified by the use of words such as “seek”, “anticipate”, “believe”, “plan”, “expect”, and “intend” and statements than an event or result “may”, “will”, “should”, “could”, or “might” occur or be achieved and other similar expressions. Forward-looking information is subject to business, legal and economic risks and uncertainties and other factors that could cause actual results to differ materially from those contained in forward-looking statements. Such factors include, among other things, risks relating to property interests, the global economic climate, commodity prices, sovereign and legal risks, and environmental risks. Forward-looking statements are based upon estimates and opinions at the date the statements are made. Mt Monger Resources undertakes no obligation to update these forward-looking statements for events or circumstances that occur subsequent to such dates or to update or keep current any of the information contained herein. The Recipient should not place undue reliance upon forward-looking statements. Any estimates or projections as to events that may occur in the future (including projections of revenue, expense, net income and performance) are based upon the best judgment of Mt Monger Resources from information available as of the date of this document. There is no guarantee that any of these estimates or projections will be achieved. Actual results will vary from the projections and such variations may be material. Nothing contained herein is, or shall be relied upon as, a promise or representation as to the past or future. Mt Monger Resources, its affiliates, directors, employees and/or agents expressly disclaim any and all liability relating or resulting from the use of all or any part of this document or any of the information contained herein.
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APPENDIX I – East Laverton Aircore Drilling Summary
| Hole ID | Type | North | East | RL | Depth | Dip | Azimuth |
|---|---|---|---|---|---|---|---|
| MGA | MGA | (m) | (m) | **(o) ** | **(o) ** | ||
| 22ELAC001 22ELAC002 22ELAC003 22ELAC004 22ELAC005 22ELAC006 22ELAC007 22ELAC008 22ELAC009 22ELAC010 22ELAC011 22ELAC012 22ELAC013 22ELAC014 22ELAC015 22ELAC016 22ELAC017 22ELAC018 22ELAC019 22ELAC020 22ELAC021 22ELAC022 22ELAC023 22ELAC024 22ELAC025 22ELAC026 22ELAC027 22ELAC028 22ELAC029 22ELAC030 22ELAC031 22ELAC032 22ELAC033 22ELAC034 22ELAC035 22ELAC036 22ELAC037 22ELAC038 22ELAC039 22ELAC040 22ELAC041 22ELAC042 22ELAC043 22ELAC044 22ELAC045 22ELAC046 22ELAC047 22ELAC048 |
AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC AC |
6860879 6860864 6860832 6860007 6857802 6857804 6857804 6857805 6857802 6857799 6856995 6856999 6856990 6856997 6855801 6855800 6855797 6854998 6854994 6855006 6854980 6854998 6854601 6854596 6854595 6854198 6853803 6853399 6854200 6854201 6854195 6854197 6853798 6853795 6853802 6853801 6853400 6853396 6853401 6853402 6860066 6860110 6859247 6859278 6859322 6858468 6858512 6858528 |
456865 456671 456492 456578 449504 449692 449902 450098 450303 450499 450496 450699 450903 451102 451102 451309 451498 451394 451597 451795 449692 449494 449501 449695 449901 449503 449696 449719 449704 449904 450100 450299 449897 450091 450302 450503 449904 450102 450304 450503 456826 457015 456760 456956 457158 456902 457104 457293 |
518 511 513 510 544 547 545 545 543 539 526 531 528 522 516 515 512 512 511 511 518 518 518 518 516 508 508 507 514 515 511 511 507 511 512 512 511 513 513 513 508 507 505 502 501 501 503 500 |
39 41 32 16 2 2 15 17 2 2 13 23 24 7 28 31 25 59 28 47 8 8 37 21 11 26 25 16 29 23 21 12 26 36 40 27 17 11 44 51 15 36 29 5 9 17 12 36 |
-90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 -90 |
0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 |
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APPENDIX II – Significant Intersection Summary
| Hole ID | From (m) |
To (m) | Interval (m) |
TREO (ppm) |
HREO (ppm) |
MREO (ppm) |
CREO (ppm) |
Nd+Pr REO(ppm) |
Sc2O3 (ppm) |
|---|---|---|---|---|---|---|---|---|---|
| 22ELAC001 | 22 | 27 | 5 | 436 | 28 | 101 | 81 | 83 | 8 |
| 22ELAC002 | 37 | 40 | 3 | 707 | 115 | 184 | 190 | 135 | 15 |
| 22ELAC003 including |
24 27 |
32 29 |
8 2 |
855 1,806 |
108 227 |
266 553 |
238 502 |
209 435 |
9 13 |
| 22ELAC006 | 0 | 2 | 2 | 349 | 64 | 79 | 91 | 55 | 21 |
| 22ELAC011 | 9 | 11 | 2 | 414 | 45 | 113 | 100 | 90 | 5 |
| 22ELAC013 | 19 | 22 | 3 | 402 | 28 | 96 | 77 | 78 | 4 |
| 22ELAC015 | 12 20 |
14 25 |
2 5 |
466 396 |
71 36 |
113 81 |
114 74 |
83 64 |
15 13 |
| 22ELAC016 | 18 28 |
20 30 |
2 2 |
1,052 508 |
80 98 |
237 167 |
195 162 |
186 121 |
22 41 |
| 22ELAC017 | 17 | 25 | 8 | 656 | 110 | 167 | 172 | 120 | 17 |
| 22ELAC018 | 16 | 20 | 4 | 422 | 66 | 109 | 109 | 79 | 18 |
| 22ELAC019 | 21 | 25 | 5 | 720 | 79 | 151 | 141 | 111 | 17 |
| 22ELAC020 | 18 | 24 | 6 | 406 | 60 | 111 | 106 | 82 | 16 |
| 22ELAC023 including and |
21 23 33 |
37 26 35 |
16 3 2 |
788 1,577 1,191 |
108 143 268 |
221 471 338 |
211 383 412 |
172 374 257 |
24 60 2 |
| 22ELAC026 including |
16 18 |
23 20 |
7 2 |
828 1,136 |
147 150 |
223 309 |
230 280 |
158 228 |
73 82 |
| 22ELAC027 including |
18 20 22 |
24 21 23 |
6 1 1 |
1,010 1,721 1,590 |
60 71 88 |
237 385 445 |
193 300 348 |
203 338 385 |
31 6 31 |
| 22ELAC029 | 18 | 24 | 6 | 607 | 63 | 89 | 94 | 64 | 66 |
| 22ELAC031 including |
15 16 |
18 17 |
3 1 |
711 1,021 |
80 124 |
163 253 |
151 235 |
123 191 |
26 40 |
| 22ELAC033 | 13 | 26 | 13 | 571 | 37 | 116 | 101 | 99 | 2 |
| 22ELAC034 | 30 | 36 | 6 | 551 | 26 | 115 | 91 | 98 | 4 |
| 22ELAC035 | 23 | 27 | 4 | 527 | 29 | 41 | 41 | 28 | 77 |
| 22ELAC036 | 23 | 27 | 4 | 575 | 51 | 108 | 103 | 87 | 22 |
| 22ELAC039 including and |
26 26 28 |
30 27 29 |
4 1 1 |
1,156 1,982 1,914 |
131 170 252 |
295 520 491 |
266 429 467 |
228 416 372 |
82 93 82 |
| 22ELAC040 including |
24 25 42 |
28 27 45 |
4 2 3 |
1,102 1,726 344 |
353 504 91 |
374 607 72 |
435 657 110 |
227 375 50 |
112 114 26 |
| 22ELAC042 | 27 | 32 | 5 | 480 | 43 | 149 | 123 | 121 | 9 |
| 22ELAC043 including |
4 8 12 26 |
6 20 16 29 |
2 12 4 3 |
470 1,058 1,880 676 |
71 96 137 63 |
92 300 539 151 |
105 255 435 142 |
67 243 443 122 |
20 6 5 5 |
| 22ELAC045 | 4 | 9 | 5 | 424 | 32 | 102 | 86 | 83 | 6 |
| 22ELAC046 including |
6 15 16 |
8 17 17 |
2 2 1 |
388 1,289 2,107 |
46 54 64 |
69 283 456 |
73 217 335 |
50 244 400 |
21 6 5 |
| 22ELAC048 including and |
18 22 31 |
36 30 36 |
18 8 5 |
1,231 1,466 1,427 |
74 76 103 |
261 299 334 |
213 237 282 |
216 250 274 |
10 13 6 |
TREO (Total Rare Earth Oxide) grade includes CeO2, Dy2O3, Er2O3, Eu2O3, Gd2O3, Ho2O3, La2O3, Lu2O3, Nd2O3, Pr6O11, Sm2O3, Tb4O7, Tm2O3, Yb2O3 and Y2O3 and is calculated using standard oxide conversion factors for each element (see Appendix V).
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HREO (Heavy Rare Earth Oxide) grade includes Eu2O3, Gd2O3, Tb4O7, Dy2O3, Ho2O3, Er2O3, Tm2O3, Yb2O3, Lu2O3 and Y2O3. Shown as percentage of TREO.
MREO (Magnet Rare Earth Oxide) grade includes Nd2O3, Pr6O11, Sm2O3, Gd2O3, Tb4O7, Dy2O3, and Ho2O3. Shown as percentage of TREO.
CREO (Critical Rare Earth Oxide) grade includes Nd2O3, Eu2O3, Tb4O7, Dy2O3 and Y2O3. Shown as percentage of TREO.
Nd+Pr REO (Neodymium-Praseodymium or NdPr) includes Nd2O3 and Pr6O11.
Significant intersections are based on a 300ppm TREO cut-off grade and include a maximum of 3m internal subgrade mineralisation (i.e. one 3m composite sample with grade less than 300ppm TREO).
Reported higher-grade intersections (in bold) are based on a 1,000ppm TREO cut-off grade and do not contain any internal subgrade mineralisation.
No maximum grade cut has been applied. Appropriate rounding of grade values has been applied.
Down hole interval widths are reported. Mineralisation is interpreted to be flat-laying and therefore down hole widths are considered to be close to true width.
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APPENDIX III – Significant Intersection Comparison Summary
| Hole ID | Composite Sample | Composite Sample | Composite Sample | 1m Drill Sample | 1m Drill Sample | |||
|---|---|---|---|---|---|---|---|---|
| From (m) |
To (m) |
Interval (m) |
Grade TREO (ppm) |
From (m) |
To (m) |
Interval (m) |
Grade TREO (ppm) |
|
| 22ELAC001 | 18 | 24 | 6 | 421 | 22 | 27 | 5 | 436 |
| 22ELAC002 | 36 | 41 | 5 | 517 | 37 | 40 | 3 | 707 |
| 22ELAC003 including |
24 27 |
32 32 |
8 5 |
1,278 1,790 |
24 27 |
32 29 |
8 2 |
855 1,806 |
| 22ELAC006 | 0 | 2 | 2 | 482 | 0 | 2 | 2 | 349 |
| 22ELAC011 | 9 | 12 | 3 | 378 | 9 | 11 | 2 | 414 |
| 22ELAC013 | 18 | 24 | 6 | 345 | 19 | 22 | 3 | 402 |
| 22ELAC015 | 12 18 |
15 28 |
3 10 |
310 359 |
12 20 |
14 25 |
2 5 |
466 396 |
| 22ELAC016 | 18 27 |
21 30 |
3 3 |
882 345 |
18 28 |
20 30 |
2 2 |
1,052 508 |
| 22ELAC017 | 15 | 25 | 10 | 637 | 17 | 25 | 8 | 656 |
| 22ELAC018 | 15 | 21 | 6 | 380 | 16 | 20 | 4 | 422 |
| 22ELAC019 | 21 | 24 | 3 | 790 | 21 | 25 | 5 | 720 |
| 22ELAC020 | 18 | 24 | 6 | 392 | 18 | 24 | 6 | 406 |
| 22ELAC021 | 0 | 3 | 3 | 301 | Not assayed | |||
| 22ELAC023 including and |
21 24 33 |
37 27 36 |
16 3 3 |
849 1,135 1,275 |
21 23 33 |
37 26 35 |
16 3 2 |
788 1,577 1,191 |
| 22ELAC026 including |
15 18 |
24 21 |
9 3 |
709 1,034 |
16 18 |
23 20 |
7 2 |
828 1,136 |
| 22ELAC027 including |
18 21 |
24 24 |
6 3 |
1,017 1,194 |
18 20 22 |
24 21 23 |
6 1 1 |
1,010 1,721 1,590 |
| 22ELAC029 | 18 | 24 | 6 | 686 | 18 | 24 | 6 | 607 |
| 22ELAC031 including |
15 | 18 | 3 | 519 | 15 16 |
18 17 |
3 1 |
711 1,021 |
| 22ELAC033 including |
12 18 |
26 21 |
14 3 |
549 1,016 |
13 | 26 | 13 | 571 |
| 22ELAC034 | 30 | 36 | 6 | 461 | 30 | 36 | 6 | 551 |
| 22ELAC035 | 21 | 30 | 9 | 415 | 23 | 27 | 4 | 527 |
| 22ELAC036 | 15 | 27 | 12 | 384 | 23 | 27 | 4 | 575 |
| 22ELAC039 including |
24 27 |
30 30 |
6 3 |
1,089 1,753 |
26 26 28 |
30 27 29 |
4 1 1 |
1,156 1,982 1,914 |
| 22ELAC040 including |
24 24 |
30 27 |
6 3 |
865 1,371 |
24 25 42 |
28 27 45 |
4 2 3 |
1,102 1,726 344 |
| 22ELAC042 | 27 | 33 | 6 | 419 | 27 | 32 | 5 | 480 |
| 22ELAC043 including |
3 12 27 |
21 18 29 |
18 6 2 |
852 1,493 698 |
4 8 12 26 |
6 20 16 29 |
2 12 4 3 |
470 1,058 1,880 676 |
| 22ELAC045 | 3 | 9 | 6 | 444 | 4 | 9 | 5 | 425 |
| 22ELAC046 including |
6 15 |
9 17 |
3 2 |
390 1,889 |
6 15 16 |
8 17 17 |
2 2 1 |
388 1,289 2,107 |
| 22ELAC048 including |
18 21 |
36 36 |
18 15 |
1,297 1,461 |
18 22 **31 ** |
36 30 36 |
18 8 5 |
1,231 1,466 1,427 |
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TREO grade includes CeO2, Dy2O3, Er2O3, Eu2O3, Gd2O3, Ho2O3, La2O3, Lu2O3, Nd2O3, Pr6O11, Sm2O3, Tb4O7, Tm2O3, Yb2O3, and Y2O3 and is calculated using standard oxide conversion factors for each element (see Appendix V).
Significant intersections are based on a 200ppm TREO cut-off grade and include a maximum of 3m internal subgrade mineralisation (i.e. one 3m composite sample with grade less than 300ppm TREO).
Reported higher-grade intersections (in bold) are based on a 1,000ppm TREO cut-off grade and do not contain any internal subgrade mineralisation.
No maximum grade cut has been applied. Appropriate rounding of grade values has been applied.
Down hole interval widths are reported. Mineralisation is interpreted to be flat-laying and therefore down hole widths are considered to be close to true width.
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Page 10
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==> picture [113 x 18] intentionally omitted <==
==> picture [113 x 18] intentionally omitted <==
APPENDIX IV – Rare Earth Element Assay Results
| Hole ID | From (m) |
To (m) |
Interval (m) |
La2O3 (ppm) |
CeO2 (ppm) |
Pr6O11 (ppm) |
Nd2O3 (ppm) |
Sm2O3 (ppm) |
Eu2O3 (ppm) |
Gd2O3 (ppm) |
Tb4O7 (ppm) |
Dy2O3 (ppm) |
Ho2O3 (ppm) |
Er2O3 (ppm) |
Tm2O3 (ppm) |
Yb2O3 (ppm) |
Lu2O3 (ppm) |
Y2O3 (ppm) |
TREO (ppm) |
Sc2O3 (ppm) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 22ELAC001 | 18 | 19 | 1 | 24.2 | 32.1 | 4.5 | 13.4 | 2.0 | 0.4 | 1.4 | 0.2 | 1.0 | 0.2 | 0.5 | 0.1 | 0.5 | 0.1 | 5.3 | 85.8 | 8.3 |
| 22ELAC001 | 19 | 20 | 1 | 50.3 | 89.2 | 9.3 | 26.5 | 3.4 | 0.7 | 1.9 | 0.3 | 1.3 | 0.2 | 0.6 | 0.1 | 0.7 | 0.1 | 6.3 | 190.9 | 9.2 |
| 22ELAC001 | 20 | 21 | 1 | 65.7 | 120.1 | 11.9 | 33.7 | 4.2 | 0.9 | 2.3 | 0.3 | 1.5 | 0.3 | 0.6 | 0.1 | 0.6 | 0.1 | 6.8 | 249.2 | 7.7 |
| 22ELAC001 | 21 | 22 | 1 | 78.3 | 128.4 | 13.7 | 39.2 | 5.0 | 1.0 | 2.8 | 0.4 | 1.9 | 0.3 | 0.8 | 0.1 | 0.7 | 0.1 | 8.3 | 281.1 | 10.6 |
| 22ELAC001 | 22 | 23 | 1 | 104.5 | 171.4 | 19.6 | 54.9 | 7.3 | 1.3 | 4.3 | 0.5 | 2.5 | 0.4 | 1.0 | 0.1 | 0.8 | 0.1 | 10.3 | 379.3 | 7.8 |
| 22ELAC001 | 23 | 24 | 1 | 133.1 | 214.4 | 25.9 | 72.4 | 9.5 | 1.6 | 5.5 | 0.7 | 3.2 | 0.5 | 1.3 | 0.2 | 1.1 | 0.2 | 12.8 | 482.5 | 9.1 |
| 22ELAC001 | 24 | 25 | 1 | 121.4 | 210.7 | 22.7 | 63.0 | 8.1 | 1.7 | 4.6 | 0.6 | 3.0 | 0.5 | 1.3 | 0.2 | 1.2 | 0.2 | 13.1 | 452.0 | 7.1 |
| 22ELAC001 | 25 | 26 | 1 | 85.5 | 165.2 | 16.6 | 48.2 | 6.6 | 1.4 | 4.1 | 0.5 | 2.8 | 0.5 | 1.3 | 0.2 | 1.1 | 0.2 | 11.9 | 346.1 | 8.1 |
| 22ELAC001 | 26 | 27 | 1 | 112.0 | 265.3 | 23.1 | 68.5 | 10.3 | 2.3 | 7.0 | 1.0 | 5.0 | 0.8 | 2.1 | 0.3 | 1.8 | 0.2 | 19.3 | 518.9 | 8.3 |
| 22ELAC001 | 27 | 28 | 1 | 62.2 | 108.1 | 11.6 | 34.4 | 5.0 | 1.3 | 3.4 | 0.5 | 2.5 | 0.4 | 1.2 | 0.2 | 1.1 | 0.2 | 11.3 | 243.3 | 6.5 |
| 22ELAC001 | 28 | 29 | 1 | 73.8 | 104.0 | 13.4 | 40.0 | 5.6 | 1.3 | 3.9 | 0.5 | 2.7 | 0.4 | 1.2 | 0.2 | 1.0 | 0.1 | 12.3 | 260.4 | 6.8 |
| 22ELAC001 | 29 | 30 | 1 | 45.6 | 65.8 | 8.8 | 26.7 | 3.8 | 1.0 | 2.8 | 0.4 | 2.0 | 0.4 | 1.0 | 0.1 | 0.9 | 0.1 | 10.2 | 169.7 | 6.8 |
| 22ELAC002 | 33 | 34 | 1 | 19.5 | 41.0 | 4.7 | 16.2 | 2.7 | 0.6 | 2.3 | 0.3 | 1.6 | 0.3 | 0.8 | 0.1 | 0.6 | 0.1 | 6.5 | 97.2 | 50.0 |
| 22ELAC002 | 34 | 35 | 1 | 31.7 | 72.5 | 8.2 | 29.0 | 5.3 | 1.2 | 4.1 | 0.6 | 2.9 | 0.5 | 1.4 | 0.2 | 1.2 | 0.2 | 12.4 | 171.3 | 52.0 |
| 22ELAC002 | 35 | 36 | 1 | 60.5 | 114.7 | 13.2 | 45.4 | 7.9 | 1.8 | 6.1 | 0.8 | 4.1 | 0.7 | 1.8 | 0.2 | 1.5 | 0.2 | 17.7 | 276.5 | 35.9 |
| 22ELAC002 | 36 | 37 | 1 | 41.4 | 78.0 | 8.0 | 26.5 | 4.4 | 1.1 | 3.8 | 0.5 | 2.9 | 0.6 | 1.7 | 0.2 | 1.6 | 0.2 | 18.5 | 189.6 | 8.3 |
| 22ELAC002 | 37 | 38 | 1 | 151.3 | 286.2 | 30.2 | 103.5 | 17.4 | 3.8 | 15.0 | 2.0 | 10.9 | 1.9 | 5.4 | 0.7 | 4.1 | 0.6 | 63.2 | 696.2 | 13.9 |
| 22ELAC002 | 38 | 39 | 1 | 183.0 | 336.6 | 37.5 | 134.1 | 22.7 | 5.1 | 20.8 | 2.8 | 14.6 | 2.6 | 7.2 | 0.9 | 5.4 | 0.8 | 83.6 | 857.6 | 19.9 |
| 22ELAC002 | 39 | 40 | 1 | 129.0 | 230.9 | 23.4 | 77.3 | 12.2 | 2.4 | 10.5 | 1.5 | 8.5 | 1.6 | 5.2 | 0.7 | 4.9 | 0.8 | 56.9 | 565.8 | 11.1 |
| 22ELAC002 | 40 | 41 | 1 | 53.0 | 92.7 | 10.3 | 34.6 | 5.6 | 1.2 | 4.5 | 0.6 | 3.3 | 0.6 | 1.8 | 0.3 | 1.7 | 0.3 | 20.1 | 230.5 | 11.6 |
| 22ELAC003 | 24 | 25 | 1 | 72.6 | 197.2 | 16.9 | 54.1 | 8.4 | 1.5 | 5.0 | 0.7 | 3.1 | 0.5 | 1.4 | 0.2 | 1.3 | 0.2 | 13.1 | 376.2 | 6.1 |
| 22ELAC003 | 25 | 26 | 1 | 24.4 | 59.1 | 5.1 | 16.8 | 2.9 | 0.6 | 2.1 | 0.3 | 1.6 | 0.3 | 0.9 | 0.1 | 1.0 | 0.2 | 8.0 | 123.3 | 8.3 |
| 22ELAC003 | 26 | 27 | 1 | 269.7 | 242.0 | 60.4 | 190.7 | 28.2 | 5.3 | 17.5 | 2.0 | 8.6 | 1.3 | 3.0 | 0.3 | 2.0 | 0.3 | 31.1 | 862.3 | 13.4 |
| 22ELAC003 | 27 | 28 | 1 | 328.4 | 326.8 | 73.7 | 236.8 | 36.1 | 6.9 | 21.4 | 2.6 | 11.5 | 1.7 | 4.4 | 0.5 | 3.1 | 0.5 | 49.8 | 1104.1 | 13.3 |
| 22ELAC003 | 28 | 29 | 1 | 774.0 | 759.2 | 127.5 | 432.7 | 61.7 | 13.0 | 55.7 | 6.5 | 32.5 | 5.7 | 15.0 | 1.6 | 8.5 | 1.3 | 212.7 | 2507.5 | 12.1 |
| 22ELAC003 | 29 | 30 | 1 | 151.9 | 105.3 | 25.7 | 84.0 | 12.3 | 2.6 | 10.0 | 1.3 | 6.9 | 1.3 | 3.9 | 0.5 | 3.6 | 0.6 | 43.7 | 453.4 | 6.4 |
| 22ELAC003 | 30 | 31 | 1 | 247.5 | 181.2 | 42.3 | 140.0 | 20.6 | 4.3 | 18.7 | 2.3 | 11.4 | 2.0 | 5.5 | 0.7 | 4.1 | 0.6 | 67.8 | 748.9 | 10.9 |
| 22ELAC003 | 31 | 32 | 1 | 217.0 | 165.8 | 37.1 | 127.1 | 19.1 | 4.2 | 16.5 | 2.1 | 10.0 | 1.7 | 4.6 | 0.5 | 3.1 | 0.5 | 57.9 | 667.2 | 4.1 |
| 22ELAC006 | 0 | 1 | 1 | 46.3 | 130.2 | 10.8 | 38.8 | 7.1 | 1.5 | 6.2 | 0.9 | 5.5 | 1.0 | 3.3 | 0.5 | 3.1 | 0.5 | 35.4 | 291.1 | 18.9 |
| 22ELAC006 | 1 | 2 | 1 | 57.0 | 210.1 | 13.3 | 47.8 | 8.8 | 1.9 | 7.8 | 1.2 | 6.9 | 1.3 | 4.0 | 0.6 | 3.6 | 0.6 | 42.8 | 407.7 | 22.3 |
| 22ELAC011 | 9 | 10 | 1 | 71.1 | 137.0 | 16.2 | 48.5 | 6.7 | 1.4 | 4.5 | 0.5 | 2.7 | 0.5 | 1.3 | 0.2 | 1.2 | 0.2 | 12.8 | 304.7 | 6.2 |
| 22ELAC011 | 10 | 11 | 1 | 117.9 | 213.7 | 27.4 | 87.9 | 13.0 | 2.8 | 9.4 | 1.2 | 6.3 | 1.3 | 3.8 | 0.5 | 3.2 | 0.4 | 35.0 | 523.9 | 4.2 |
| 22ELAC011 | 11 | 12 | 1 | 53.5 | 104.7 | 12.9 | 41.5 | 6.4 | 1.5 | 4.6 | 0.6 | 3.2 | 0.7 | 2.0 | 0.3 | 1.8 | 0.3 | 19.4 | 253.1 | 3.9 |
| 22ELAC011 | 12 | 13 | 1 | 27.9 | 58.0 | 6.5 | 19.7 | 2.9 | 0.7 | 2.0 | 0.3 | 1.3 | 0.3 | 0.8 | 0.1 | 0.8 | 0.1 | 7.5 | 128.7 | 2.5 |
| 22ELAC013 | 18 | 19 | 1 | 47.7 | 82.2 | 8.0 | 22.8 | 3.5 | 0.8 | 2.5 | 0.3 | 1.7 | 0.3 | 1.0 | 0.1 | 1.0 | 0.1 | 8.9 | 181.2 | 4.1 |
Page 11
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==> picture [113 x 18] intentionally omitted <==
==> picture [113 x 18] intentionally omitted <==
==> picture [113 x 18] intentionally omitted <==
| Hole ID | From (m) |
To (m) |
Interval (m) |
La2O3 (ppm) |
CeO2 (ppm) |
Pr6O11 (ppm) |
Nd2O3 (ppm) |
Sm2O3 (ppm) |
Eu2O3 (ppm) |
Gd2O3 (ppm) |
Tb4O7 (ppm) |
Dy2O3 (ppm) |
Ho2O3 (ppm) |
Er2O3 (ppm) |
Tm2O3 (ppm) |
Yb2O3 (ppm) |
Lu2O3 (ppm) |
Y2O3 (ppm) |
TREO (ppm) |
Sc2O3 (ppm) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 22ELAC013 | 19 | 20 | 1 | 95.7 | 184.3 | 19.3 | 54.2 | 7.5 | 1.6 | 5.0 | 0.6 | 3.0 | 0.5 | 1.6 | 0.2 | 1.4 | 0.2 | 13.9 | 389.1 | 4.6 |
| 22ELAC013 | 20 | 21 | 1 | 116.0 | 206.4 | 24.1 | 72.8 | 11.2 | 2.5 | 7.5 | 0.9 | 4.2 | 0.7 | 1.8 | 0.2 | 1.4 | 0.2 | 15.9 | 465.8 | 2.8 |
| 22ELAC013 | 21 | 22 | 1 | 100.2 | 160.9 | 17.2 | 46.9 | 5.9 | 1.2 | 3.8 | 0.5 | 2.2 | 0.4 | 1.2 | 0.2 | 1.1 | 0.2 | 10.7 | 352.3 | 3.4 |
| 22ELAC013 | 22 | 23 | 1 | 75.8 | 129.0 | 13.6 | 39.5 | 5.3 | 1.1 | 3.5 | 0.4 | 2.0 | 0.4 | 1.0 | 0.1 | 0.9 | 0.1 | 10.2 | 282.9 | 2.5 |
| 22ELAC013 | 23 | 24 | 1 | 46.6 | 91.3 | 9.7 | 28.3 | 4.2 | 0.9 | 3.0 | 0.4 | 2.2 | 0.4 | 1.3 | 0.2 | 1.2 | 0.2 | 11.7 | 201.7 | 5.3 |
| 22ELAC015 | 12 | 13 | 1 | 70.1 | 126.5 | 13.2 | 40.8 | 8.1 | 1.9 | 7.2 | 1.1 | 6.1 | 1.2 | 3.6 | 0.5 | 3.5 | 0.5 | 36.2 | 320.7 | 13.4 |
| 22ELAC015 | 13 | 14 | 1 | 142.5 | 262.9 | 28.5 | 83.0 | 13.9 | 3.0 | 10.8 | 1.5 | 8.2 | 1.6 | 4.6 | 0.6 | 3.9 | 0.6 | 46.0 | 611.6 | 16.4 |
| 22ELAC015 | 14 | 15 | 1 | 99.8 | 88.3 | 6.8 | 18.3 | 3.5 | 0.8 | 3.1 | 0.5 | 2.8 | 0.6 | 1.9 | 0.3 | 1.8 | 0.3 | 18.4 | 247.3 | 15.5 |
| 22ELAC015 | 15 | 16 | 1 | 6.5 | 12.9 | 1.4 | 4.6 | 0.9 | 0.3 | 1.1 | 0.2 | 1.3 | 0.3 | 1.0 | 0.1 | 1.0 | 0.1 | 9.5 | 41.5 | 26.8 |
| 22ELAC015 | 16 | 17 | 1 | 5.0 | 9.8 | 1.0 | 3.2 | 0.7 | 0.2 | 1.0 | 0.2 | 1.3 | 0.3 | 1.0 | 0.1 | 1.0 | 0.2 | 8.5 | 33.6 | 21.0 |
| 22ELAC015 | 17 | 18 | 1 | 4.6 | 8.3 | 0.9 | 2.6 | 0.6 | 0.2 | 0.7 | 0.1 | 1.1 | 0.3 | 0.9 | 0.1 | 1.0 | 0.2 | 7.1 | 28.6 | 17.4 |
| 22ELAC015 | 18 | 19 | 1 | 71.8 | 113.1 | 11.3 | 30.9 | 4.3 | 1.0 | 3.4 | 0.5 | 2.6 | 0.5 | 1.6 | 0.2 | 1.5 | 0.2 | 16.3 | 259.3 | 9.4 |
| 22ELAC015 | 19 | 20 | 1 | 52.3 | 89.3 | 8.4 | 23.9 | 3.7 | 0.9 | 3.0 | 0.4 | 2.4 | 0.5 | 1.7 | 0.2 | 1.6 | 0.2 | 18.1 | 206.7 | 3.8 |
| 22ELAC015 | 20 | 21 | 1 | 130.8 | 183.6 | 17.6 | 45.8 | 6.4 | 1.4 | 4.2 | 0.6 | 3.0 | 0.5 | 1.5 | 0.2 | 1.1 | 0.2 | 16.9 | 413.8 | 13.5 |
| 22ELAC015 | 21 | 22 | 1 | 133.7 | 199.6 | 19.5 | 53.0 | 7.7 | 1.7 | 4.8 | 0.7 | 3.5 | 0.6 | 1.7 | 0.2 | 1.3 | 0.2 | 18.0 | 445.8 | 17.3 |
| 22ELAC015 | 22 | 23 | 1 | 80.7 | 112.9 | 10.9 | 30.6 | 4.6 | 1.1 | 3.2 | 0.4 | 2.7 | 0.5 | 1.6 | 0.2 | 1.5 | 0.2 | 17.5 | 268.7 | 9.8 |
| 22ELAC015 | 23 | 24 | 1 | 139.0 | 199.0 | 19.9 | 56.7 | 9.1 | 2.1 | 6.3 | 0.9 | 4.7 | 0.8 | 2.3 | 0.3 | 1.9 | 0.2 | 26.0 | 469.2 | 9.2 |
| 22ELAC015 | 24 | 25 | 1 | 120.8 | 140.7 | 16.6 | 50.0 | 8.4 | 2.0 | 6.3 | 0.8 | 4.8 | 0.9 | 2.3 | 0.3 | 1.7 | 0.2 | 24.3 | 380.0 | 16.1 |
| 22ELAC015 | 25 | 26 | 1 | 40.8 | 74.1 | 6.8 | 20.8 | 3.7 | 0.9 | 2.8 | 0.4 | 2.4 | 0.5 | 1.3 | 0.2 | 1.1 | 0.2 | 12.8 | 168.8 | 16.6 |
| 22ELAC015 | 26 | 27 | 1 | 37.3 | 107.0 | 6.9 | 20.4 | 3.7 | 0.9 | 2.6 | 0.4 | 2.1 | 0.4 | 1.3 | 0.2 | 1.1 | 0.2 | 11.6 | 196.0 | 15.7 |
| 22ELAC015 | 27 | 28 | 1 | 104.8 | 124.1 | 17.3 | 51.4 | 7.9 | 1.9 | 5.5 | 0.7 | 3.8 | 0.7 | 1.7 | 0.2 | 1.3 | 0.2 | 18.9 | 340.4 | 15.2 |
| 22ELAC016 | 18 | 19 | 1 | 422.2 | 663.3 | 69.4 | 190.7 | 30.5 | 7.0 | 19.7 | 2.7 | 13.5 | 2.1 | 4.6 | 0.5 | 2.6 | 0.3 | 52.2 | 1481.1 | 22.3 |
| 22ELAC016 | 19 | 20 | 1 | 179.4 | 261.6 | 28.3 | 84.3 | 14.1 | 3.4 | 9.9 | 1.4 | 7.0 | 1.1 | 2.7 | 0.3 | 1.7 | 0.2 | 27.8 | 623.5 | 21.6 |
| 22ELAC016 | 20 | 21 | 1 | 61.5 | 111.9 | 9.6 | 30.4 | 5.6 | 1.5 | 4.6 | 0.7 | 3.7 | 0.6 | 1.6 | 0.2 | 1.4 | 0.2 | 16.2 | 249.8 | 19.3 |
| 22ELAC016 | 21 | 22 | 1 | 57.1 | 97.4 | 9.6 | 31.0 | 6.1 | 1.5 | 4.6 | 0.7 | 3.8 | 0.6 | 1.7 | 0.2 | 1.4 | 0.2 | 16.6 | 232.4 | 18.8 |
| 22ELAC016 | 22 | 23 | 1 | 69.5 | 105.5 | 12.6 | 40.7 | 7.9 | 2.0 | 6.7 | 1.0 | 5.4 | 1.0 | 2.4 | 0.3 | 1.9 | 0.2 | 23.9 | 281.0 | 17.9 |
| 22ELAC016 | 23 | 24 | 1 | 42.9 | 72.7 | 8.4 | 27.2 | 5.5 | 1.4 | 4.6 | 0.7 | 4.0 | 0.7 | 2.0 | 0.3 | 1.7 | 0.3 | 20.2 | 192.5 | 16.5 |
| 22ELAC016 | 24 | 25 | 1 | 33.4 | 70.5 | 7.1 | 21.9 | 4.2 | 1.1 | 3.3 | 0.5 | 3.0 | 0.6 | 1.7 | 0.2 | 1.6 | 0.2 | 16.3 | 165.5 | 15.0 |
| 22ELAC016 | 25 | 26 | 1 | 41.4 | 82.7 | 8.9 | 28.0 | 5.6 | 1.4 | 4.4 | 0.7 | 3.8 | 0.7 | 2.1 | 0.3 | 1.7 | 0.3 | 19.9 | 201.8 | 17.4 |
| 22ELAC016 | 26 | 27 | 1 | 47.3 | 117.1 | 10.0 | 31.4 | 6.2 | 1.6 | 5.0 | 0.8 | 4.4 | 0.8 | 2.5 | 0.3 | 2.1 | 0.3 | 22.6 | 252.3 | 17.9 |
| 22ELAC016 | 27 | 28 | 1 | 43.4 | 91.0 | 8.8 | 27.8 | 5.5 | 1.4 | 4.4 | 0.7 | 4.0 | 0.8 | 2.3 | 0.3 | 2.0 | 0.3 | 23.0 | 215.7 | 18.0 |
| 22ELAC016 | 28 | 29 | 1 | 202.9 | 90.5 | 38.4 | 119.0 | 20.2 | 5.4 | 15.2 | 2.0 | 10.5 | 1.7 | 4.3 | 0.5 | 3.4 | 0.4 | 38.2 | 552.7 | 63.0 |
| 22ELAC016 | 29 | 30 | 1 | 130.2 | 121.6 | 19.0 | 65.1 | 12.9 | 3.5 | 13.7 | 2.0 | 12.3 | 2.4 | 6.4 | 0.8 | 5.4 | 0.7 | 66.3 | 462.3 | 19.3 |
| 22ELAC017 | 17 | 18 | 1 | 166.5 | 260.4 | 36.0 | 111.9 | 20.9 | 4.7 | 15.2 | 2.1 | 10.9 | 1.9 | 5.0 | 0.6 | 4.0 | 0.5 | 47.9 | 688.5 | 19.9 |
| 22ELAC017 | 18 | 19 | 1 | 156.6 | 303.4 | 30.7 | 98.0 | 18.1 | 4.4 | 13.9 | 1.9 | 10.5 | 1.9 | 5.3 | 0.7 | 4.5 | 0.6 | 50.5 | 701.0 | 18.9 |
| 22ELAC017 | 19 | 20 | 1 | 258.0 | 485.2 | 48.3 | 156.3 | 29.0 | 7.1 | 24.7 | 3.3 | 17.6 | 3.0 | 7.4 | 0.9 | 5.3 | 0.7 | 73.1 | 1120.0 | 21.2 |
| 22ELAC017 | 20 | 21 | 1 | 167.1 | 342.7 | 31.2 | 100.2 | 18.8 | 4.7 | 15.7 | 2.2 | 12.1 | 2.2 | 5.7 | 0.7 | 4.5 | 0.6 | 54.6 | 763.0 | 17.3 |
Page 12
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==> picture [113 x 18] intentionally omitted <==
==> picture [113 x 18] intentionally omitted <==
==> picture [113 x 18] intentionally omitted <==
| Hole ID | From (m) |
To (m) |
Interval (m) |
La2O3 (ppm) |
CeO2 (ppm) |
Pr6O11 (ppm) |
Nd2O3 (ppm) |
Sm2O3 (ppm) |
Eu2O3 (ppm) |
Gd2O3 (ppm) |
Tb4O7 (ppm) |
Dy2O3 (ppm) |
Ho2O3 (ppm) |
Er2O3 (ppm) |
Tm2O3 (ppm) |
Yb2O3 (ppm) |
Lu2O3 (ppm) |
Y2O3 (ppm) |
TREO (ppm) |
Sc2O3 (ppm) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 22ELAC017 | 21 | 22 | 1 | 105.1 | 194.1 | 19.6 | 62.2 | 12.1 | 3.0 | 10.4 | 1.5 | 9.0 | 1.8 | 5.1 | 0.6 | 4.3 | 0.6 | 50.7 | 480.0 | 16.3 |
| 22ELAC017 | 22 | 23 | 1 | 101.0 | 178.7 | 19.7 | 62.3 | 11.8 | 2.9 | 9.9 | 1.4 | 8.6 | 1.7 | 5.2 | 0.7 | 4.5 | 0.6 | 51.3 | 460.3 | 16.0 |
| 22ELAC017 | 23 | 24 | 1 | 149.5 | 168.9 | 24.0 | 79.0 | 14.7 | 3.8 | 14.1 | 2.1 | 12.7 | 2.7 | 8.3 | 1.1 | 6.9 | 1.1 | 91.6 | 580.4 | 16.6 |
| 22ELAC017 | 24 | 25 | 1 | 111.8 | 127.1 | 18.2 | 58.8 | 11.0 | 2.8 | 10.4 | 1.6 | 10.8 | 2.3 | 7.4 | 0.9 | 6.7 | 1.0 | 84.8 | 455.7 | 13.3 |
| 22ELAC018 | 15 | 16 | 1 | 60.8 | 71.1 | 10.8 | 35.3 | 6.6 | 1.7 | 6.4 | 0.9 | 4.8 | 0.9 | 2.3 | 0.3 | 2.1 | 0.3 | 25.5 | 229.9 | 16.6 |
| 22ELAC018 | 16 | 17 | 1 | 105.1 | 243.8 | 21.9 | 69.9 | 13.2 | 3.1 | 9.6 | 1.4 | 7.8 | 1.4 | 3.8 | 0.5 | 3.1 | 0.4 | 38.0 | 522.8 | 18.3 |
| 22ELAC018 | 17 | 18 | 1 | 120.8 | 215.0 | 25.1 | 78.6 | 14.6 | 3.5 | 10.4 | 1.5 | 8.0 | 1.4 | 3.8 | 0.5 | 3.0 | 0.4 | 38.2 | 524.7 | 17.3 |
| 22ELAC018 | 18 | 19 | 1 | 65.1 | 125.3 | 12.9 | 42.2 | 8.2 | 2.0 | 6.5 | 1.0 | 5.4 | 1.0 | 3.0 | 0.4 | 2.6 | 0.3 | 29.5 | 305.3 | 17.2 |
| 22ELAC018 | 19 | 20 | 1 | 83.4 | 103.4 | 15.2 | 49.7 | 10.0 | 2.5 | 8.8 | 1.3 | 7.7 | 1.5 | 4.4 | 0.6 | 3.7 | 0.5 | 43.7 | 336.3 | 17.3 |
| 22ELAC018 | 20 | 21 | 1 | 37.1 | 62.3 | 7.1 | 22.9 | 4.8 | 1.2 | 4.3 | 0.6 | 4.1 | 0.9 | 2.5 | 0.3 | 2.3 | 0.3 | 27.2 | 177.9 | 13.7 |
| 22ELAC019 | 21 | 22 | 1 | 170.1 | 329.2 | 31.1 | 99.1 | 18.1 | 4.5 | 14.2 | 2.0 | 10.0 | 1.7 | 4.3 | 0.5 | 3.2 | 0.5 | 41.1 | 729.6 | 19.2 |
| 22ELAC019 | 22 | 23 | 1 | 140.7 | 531.9 | 25.6 | 81.2 | 15.7 | 4.0 | 12.9 | 1.9 | 10.4 | 1.9 | 5.5 | 0.7 | 4.7 | 0.6 | 54.1 | 891.9 | 18.1 |
| 22ELAC019 | 23 | 24 | 1 | 155.4 | 484.0 | 32.5 | 114.3 | 18.8 | 4.8 | 15.4 | 2.1 | 10.9 | 2.0 | 5.0 | 0.7 | 4.4 | 0.6 | 48.5 | 899.4 | 15.8 |
| 22ELAC019 | 24 | 25 | 1 | 64.5 | 183.6 | 13.8 | 48.4 | 7.9 | 2.0 | 6.2 | 0.9 | 4.7 | 0.9 | 2.3 | 0.4 | 2.4 | 0.4 | 21.0 | 359.3 | 14.4 |
| 22ELAC020 | 18 | 19 | 1 | 91.0 | 249.4 | 21.1 | 75.2 | 12.7 | 3.1 | 10.9 | 1.4 | 7.5 | 1.3 | 3.2 | 0.5 | 2.8 | 0.4 | 30.0 | 510.5 | 18.0 |
| 22ELAC020 | 19 | 20 | 1 | 115.3 | 339.0 | 27.5 | 95.3 | 15.9 | 3.6 | 11.9 | 1.5 | 7.9 | 1.3 | 3.2 | 0.5 | 3.0 | 0.4 | 31.1 | 657.6 | 18.2 |
| 22ELAC020 | 20 | 21 | 1 | 69.4 | 122.8 | 16.6 | 58.3 | 9.6 | 2.4 | 7.4 | 1.0 | 5.2 | 1.0 | 2.5 | 0.4 | 2.4 | 0.4 | 23.3 | 322.7 | 15.7 |
| 22ELAC020 | 21 | 22 | 1 | 63.0 | 97.4 | 14.3 | 50.7 | 8.4 | 2.1 | 7.0 | 0.9 | 5.1 | 1.0 | 2.6 | 0.4 | 2.6 | 0.4 | 24.3 | 280.3 | 15.2 |
| 22ELAC020 | 22 | 23 | 1 | 70.0 | 135.7 | 15.6 | 55.5 | 9.3 | 2.4 | 7.8 | 1.1 | 5.9 | 1.1 | 2.9 | 0.4 | 2.8 | 0.4 | 28.4 | 339.5 | 16.0 |
| 22ELAC020 | 23 | 24 | 1 | 68.0 | 97.7 | 12.9 | 48.4 | 8.5 | 2.2 | 8.6 | 1.3 | 7.8 | 1.7 | 4.7 | 0.7 | 4.1 | 0.7 | 55.6 | 323.0 | 13.4 |
| 22ELAC023 | 21 | 22 | 1 | 146.0 | 53.8 | 32.4 | 113.3 | 17.1 | 4.5 | 13.2 | 1.7 | 8.3 | 1.4 | 3.4 | 0.5 | 2.8 | 0.4 | 26.8 | 425.4 | 59.4 |
| 22ELAC023 | 22 | 23 | 1 | 74.9 | 98.1 | 13.5 | 48.2 | 8.0 | 2.1 | 7.6 | 1.1 | 6.2 | 1.2 | 3.1 | 0.5 | 2.8 | 0.4 | 31.9 | 299.7 | 17.9 |
| 22ELAC023 | 23 | 24 | 1 | 562.9 | 577.3 | 114.1 | 383.7 | 54.3 | 14.1 | 43.6 | 5.3 | 25.7 | 4.2 | 9.1 | 1.2 | 6.6 | 0.9 | 87.8 | 1890.7 | 62.9 |
| 22ELAC023 | 24 | 25 | 1 | 457.4 | 733.4 | 99.3 | 328.9 | 45.8 | 11.6 | 34.1 | 4.2 | 20.1 | 3.2 | 7.1 | 0.9 | 5.2 | 0.7 | 67.7 | 1819.7 | 60.9 |
| 22ELAC023 | 25 | 26 | 1 | 200.5 | 528.2 | 47.4 | 148.1 | 21.2 | 5.3 | 15.2 | 2.0 | 9.8 | 1.7 | 3.8 | 0.5 | 3.2 | 0.4 | 34.3 | 1021.7 | 57.2 |
| 22ELAC023 | 26 | 27 | 1 | 158.9 | 450.8 | 39.4 | 122.5 | 19.5 | 5.2 | 15.0 | 2.1 | 11.4 | 2.0 | 4.7 | 0.7 | 4.1 | 0.6 | 38.2 | 875.0 | 63.2 |
| 22ELAC023 | 27 | 28 | 1 | 131.9 | 93.2 | 24.4 | 82.0 | 11.9 | 3.3 | 11.4 | 1.5 | 8.4 | 1.7 | 4.4 | 0.7 | 4.5 | 0.7 | 45.8 | 426.0 | 39.0 |
| 22ELAC023 | 28 | 29 | 1 | 98.2 | 371.0 | 19.8 | 64.2 | 10.2 | 2.8 | 9.2 | 1.4 | 8.2 | 1.7 | 4.6 | 0.7 | 4.6 | 0.7 | 49.3 | 646.3 | 2.6 |
| 22ELAC023 | 29 | 30 | 1 | 86.1 | 202.1 | 17.0 | 55.6 | 8.3 | 2.2 | 7.2 | 1.0 | 6.1 | 1.2 | 3.3 | 0.5 | 3.2 | 0.5 | 35.7 | 430.0 | 1.1 |
| 22ELAC023 | 30 | 31 | 1 | 77.5 | 106.4 | 15.5 | 54.8 | 9.2 | 2.6 | 8.9 | 1.2 | 7.4 | 1.5 | 4.1 | 0.6 | 4.0 | 0.6 | 46.6 | 340.9 | 1.1 |
| 22ELAC023 | 31 | 32 | 1 | 115.5 | 76.4 | 19.6 | 67.7 | 10.4 | 2.9 | 10.2 | 1.4 | 8.5 | 1.8 | 5.1 | 0.8 | 5.0 | 0.8 | 58.5 | 384.6 | 1.2 |
| 22ELAC023 | 32 | 33 | 1 | 176.5 | 169.5 | 28.5 | 94.8 | 12.9 | 3.3 | 12.0 | 1.5 | 8.8 | 1.8 | 4.9 | 0.7 | 4.5 | 0.7 | 57.7 | 578.3 | 3.9 |
| 22ELAC023 | 33 | 34 | 1 | 375.3 | 335.4 | 71.0 | 243.8 | 32.5 | 8.7 | 31.5 | 4.0 | 23.3 | 5.0 | 13.3 | 1.8 | 9.7 | 1.6 | 175.9 | 1332.8 | 2.0 |
| 22ELAC023 | 34 | 35 | 1 | 304.9 | 261.6 | 46.0 | 154.0 | 19.7 | 5.3 | 22.8 | 2.8 | 16.5 | 4.1 | 11.2 | 1.5 | 7.5 | 1.3 | 189.2 | 1048.3 | 1.7 |
| 22ELAC023 | 35 | 36 | 1 | 80.1 | 122.2 | 12.0 | 38.4 | 4.5 | 1.0 | 3.1 | 0.3 | 1.7 | 0.3 | 0.9 | 0.1 | 0.8 | 0.1 | 13.5 | 279.2 | 1.7 |
| 22ELAC023 | 36 | 37 | 1 | 224.6 | 384.5 | 38.3 | 110.8 | 12.0 | 2.4 | 6.9 | 0.6 | 2.8 | 0.5 | 1.3 | 0.2 | 1.0 | 0.2 | 19.0 | 805.2 | 3.6 |
| 22ELAC026 | 14 | 15 | 1 | 9.6 | 22.0 | 3.0 | 10.4 | 1.8 | 0.5 | 1.6 | 0.2 | 1.5 | 0.3 | 0.8 | 0.1 | 0.9 | 0.1 | 5.3 | 58.1 | 108.9 |
Page 13
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==> picture [113 x 18] intentionally omitted <==
==> picture [113 x 18] intentionally omitted <==
==> picture [113 x 18] intentionally omitted <==
| Hole ID | From (m) |
To (m) |
Interval (m) |
La2O3 (ppm) |
CeO2 (ppm) |
Pr6O11 (ppm) |
Nd2O3 (ppm) |
Sm2O3 (ppm) |
Eu2O3 (ppm) |
Gd2O3 (ppm) |
Tb4O7 (ppm) |
Dy2O3 (ppm) |
Ho2O3 (ppm) |
Er2O3 (ppm) |
Tm2O3 (ppm) |
Yb2O3 (ppm) |
Lu2O3 (ppm) |
Y2O3 (ppm) |
TREO (ppm) |
Sc2O3 (ppm) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 22ELAC026 | 15 | 16 | 1 | 39.9 | 78.0 | 9.7 | 34.2 | 5.8 | 1.4 | 4.7 | 0.7 | 3.4 | 0.6 | 1.3 | 0.2 | 1.2 | 0.2 | 10.6 | 191.7 | 114.4 |
| 22ELAC026 | 16 | 17 | 1 | 49.1 | 135.7 | 15.5 | 60.0 | 11.9 | 3.3 | 11.6 | 1.8 | 10.2 | 1.8 | 4.4 | 0.7 | 4.1 | 0.5 | 30.2 | 341.1 | 83.6 |
| 22ELAC026 | 17 | 18 | 1 | 69.7 | 191.6 | 20.1 | 75.5 | 14.1 | 3.8 | 12.9 | 1.9 | 10.8 | 1.9 | 4.5 | 0.7 | 4.1 | 0.5 | 33.5 | 445.7 | 82.4 |
| 22ELAC026 | 18 | 19 | 1 | 209.3 | 432.4 | 53.6 | 180.2 | 30.7 | 8.0 | 25.7 | 3.6 | 18.9 | 3.1 | 7.1 | 0.9 | 5.5 | 0.7 | 58.5 | 1038.4 | 75.6 |
| 22ELAC026 | 19 | 20 | 1 | 224.6 | 592.1 | 50.9 | 170.3 | 27.9 | 7.4 | 25.1 | 3.7 | 20.9 | 3.8 | 9.2 | 1.3 | 7.6 | 1.0 | 87.5 | 1233.3 | 89.1 |
| 22ELAC026 | 20 | 21 | 1 | 293.2 | 870.9 | 67.9 | 235.6 | 35.9 | 9.0 | 31.9 | 4.7 | 26.5 | 4.9 | 12.4 | 1.8 | 10.2 | 1.4 | 128.9 | 1735.4 | 66.1 |
| 22ELAC026 | 21 | 22 | 1 | 135.5 | 162.1 | 22.5 | 87.8 | 15.3 | 4.6 | 19.5 | 3.0 | 18.4 | 3.8 | 10.0 | 1.4 | 8.6 | 1.2 | 104.6 | 598.5 | 53.5 |
| 22ELAC026 | 22 | 23 | 1 | 91.1 | 55.4 | 13.4 | 55.5 | 10.0 | 3.3 | 15.7 | 2.5 | 16.6 | 3.7 | 10.2 | 1.5 | 8.7 | 1.3 | 117.0 | 405.8 | 62.7 |
| 22ELAC026 | 23 | 24 | 1 | 52.1 | 47.2 | 7.6 | 32.7 | 7.2 | 2.5 | 11.3 | 1.8 | 11.9 | 2.7 | 7.4 | 1.1 | 6.1 | 1.0 | 91.9 | 284.2 | 70.1 |
| 22ELAC027 | 17 | 18 | 1 | 32.0 | 114.5 | 6.4 | 21.5 | 3.8 | 1.0 | 3.3 | 0.5 | 2.9 | 0.6 | 1.6 | 0.3 | 1.7 | 0.2 | 16.1 | 206.4 | 4.8 |
| 22ELAC027 | 18 | 19 | 1 | 138.4 | 243.8 | 24.2 | 70.9 | 8.2 | 1.7 | 5.0 | 0.6 | 2.9 | 0.5 | 1.3 | 0.2 | 1.3 | 0.2 | 15.1 | 514.3 | 3.8 |
| 22ELAC027 | 19 | 20 | 1 | 217.0 | 425.0 | 38.5 | 100.3 | 11.7 | 2.5 | 6.4 | 0.7 | 3.7 | 0.7 | 1.9 | 0.3 | 1.7 | 0.3 | 21.8 | 832.6 | 4.8 |
| 22ELAC027 | 20 | 21 | 1 | 527.8 | 759.2 | 89.4 | 248.4 | 25.3 | 5.2 | 13.5 | 1.3 | 5.9 | 1.0 | 2.7 | 0.3 | 2.1 | 0.3 | 39.0 | 1721.4 | 6.1 |
| 22ELAC027 | 21 | 22 | 1 | 180.0 | 293.6 | 30.6 | 86.1 | 9.7 | 2.2 | 5.7 | 0.7 | 3.6 | 0.7 | 2.3 | 0.3 | 2.3 | 0.4 | 27.9 | 646.1 | 19.2 |
| 22ELAC027 | 22 | 23 | 1 | 527.8 | 560.2 | 99.1 | 285.8 | 29.6 | 6.7 | 17.6 | 1.9 | 9.0 | 1.6 | 3.8 | 0.4 | 2.4 | 0.3 | 44.1 | 1590.2 | 69.0 |
| 22ELAC027 | 23 | 24 | 1 | 269.7 | 246.9 | 34.3 | 108.2 | 13.2 | 3.5 | 12.4 | 1.5 | 8.1 | 1.6 | 4.4 | 0.5 | 2.9 | 0.4 | 48.3 | 755.9 | 80.1 |
| 22ELAC027 | 24 | 25 | 1 | 58.5 | 81.2 | 7.7 | 21.0 | 2.4 | 0.6 | 2.1 | 0.3 | 1.9 | 0.5 | 1.6 | 0.3 | 1.9 | 0.3 | 20.3 | 200.5 | 7.4 |
| 22ELAC029 | 18 | 19 | 1 | 52.8 | 567.5 | 9.7 | 30.8 | 5.6 | 1.6 | 6.0 | 1.0 | 6.4 | 1.3 | 4.0 | 0.6 | 4.1 | 0.5 | 35.4 | 727.5 | 73.0 |
| 22ELAC029 | 19 | 20 | 1 | 15.2 | 788.6 | 5.6 | 20.2 | 5.9 | 1.8 | 6.0 | 1.3 | 8.0 | 1.5 | 4.5 | 0.6 | 3.9 | 0.5 | 32.3 | 895.9 | 78.4 |
| 22ELAC029 | 20 | 21 | 1 | 102.5 | 486.4 | 19.3 | 59.4 | 10.3 | 2.9 | 9.2 | 1.6 | 9.5 | 1.8 | 5.0 | 0.6 | 4.1 | 0.5 | 39.2 | 752.3 | 69.5 |
| 22ELAC029 | 21 | 22 | 1 | 132.5 | 132.1 | 20.9 | 62.5 | 8.6 | 2.2 | 7.4 | 1.0 | 5.7 | 1.1 | 2.9 | 0.4 | 2.6 | 0.4 | 27.3 | 407.6 | 70.2 |
| 22ELAC029 | 22 | 23 | 1 | 99.0 | 115.8 | 15.3 | 45.5 | 6.6 | 1.8 | 6.0 | 0.9 | 5.4 | 1.1 | 3.0 | 0.4 | 2.6 | 0.4 | 29.0 | 332.6 | 69.6 |
| 22ELAC029 | 23 | 24 | 1 | 141.9 | 197.8 | 23.6 | 72.7 | 10.8 | 2.9 | 9.7 | 1.4 | 8.3 | 1.6 | 4.5 | 0.6 | 3.9 | 0.6 | 44.6 | 524.9 | 37.3 |
| 22ELAC031 | 13 | 14 | 1 | 2.2 | 17.4 | 0.5 | 1.7 | 0.4 | 0.1 | 0.5 | 0.1 | 0.6 | 0.1 | 0.5 | 0.1 | 0.6 | 0.1 | 3.8 | 28.6 | 37.3 |
| 22ELAC031 | 14 | 15 | 1 | 6.3 | 19.7 | 1.5 | 4.7 | 0.8 | 0.2 | 0.6 | 0.1 | 0.6 | 0.1 | 0.4 | 0.1 | 0.4 | 0.1 | 3.0 | 38.5 | 29.5 |
| 22ELAC031 | 15 | 16 | 1 | 113.8 | 464.3 | 27.1 | 89.5 | 15.1 | 3.6 | 11.2 | 1.6 | 8.8 | 1.5 | 4.2 | 0.5 | 3.5 | 0.5 | 38.5 | 783.7 | 13.2 |
| 22ELAC031 | 16 | 17 | 1 | 173.0 | 509.8 | 45.3 | 145.8 | 23.0 | 5.6 | 18.9 | 2.7 | 14.5 | 2.6 | 6.7 | 0.9 | 5.2 | 0.7 | 66.7 | 1021.2 | 39.9 |
| 22ELAC031 | 17 | 18 | 1 | 69.5 | 149.9 | 14.3 | 46.1 | 7.3 | 1.9 | 6.0 | 0.9 | 4.5 | 0.8 | 2.3 | 0.3 | 1.9 | 0.3 | 22.9 | 328.9 | 24.5 |
| 22ELAC031 | 18 | 19 | 1 | 53.2 | 73.8 | 8.1 | 24.1 | 3.4 | 0.9 | 3.0 | 0.4 | 2.4 | 0.5 | 1.3 | 0.2 | 1.2 | 0.2 | 14.2 | 187.0 | 9.7 |
| 22ELAC031 | 19 | 20 | 1 | 52.3 | 79.7 | 8.0 | 23.4 | 3.2 | 0.8 | 2.9 | 0.4 | 2.2 | 0.4 | 1.1 | 0.1 | 1.0 | 0.1 | 11.1 | 186.8 | 30.2 |
| 22ELAC033 | 11 | 12 | 1 | 90.4 | 104.8 | 13.2 | 38.7 | 5.2 | 1.2 | 3.6 | 0.5 | 2.3 | 0.4 | 1.3 | 0.2 | 1.1 | 0.1 | 15.1 | 278.1 | 3.1 |
| 22ELAC033 | 12 | 13 | 1 | 51.8 | 92.0 | 8.4 | 25.5 | 3.9 | 1.0 | 2.8 | 0.4 | 2.0 | 0.4 | 1.1 | 0.2 | 1.0 | 0.1 | 13.5 | 204.0 | 3.8 |
| 22ELAC033 | 13 | 14 | 1 | 121.4 | 163.4 | 18.1 | 52.8 | 7.0 | 1.6 | 5.1 | 0.6 | 2.9 | 0.6 | 1.5 | 0.2 | 1.1 | 0.2 | 20.9 | 397.3 | 2.1 |
| 22ELAC033 | 14 | 15 | 1 | 83.2 | 232.2 | 14.5 | 43.3 | 6.4 | 1.5 | 4.6 | 0.6 | 3.3 | 0.7 | 1.9 | 0.3 | 1.7 | 0.2 | 23.6 | 417.9 | 2.1 |
| 22ELAC033 | 15 | 16 | 1 | 236.9 | 374.7 | 40.6 | 112.3 | 12.9 | 2.9 | 8.6 | 1.0 | 5.0 | 0.9 | 2.5 | 0.3 | 2.0 | 0.3 | 29.6 | 830.5 | 2.0 |
| 22ELAC033 | 16 | 17 | 1 | 171.2 | 231.6 | 26.1 | 75.7 | 8.9 | 2.1 | 6.7 | 0.8 | 3.9 | 0.7 | 2.1 | 0.3 | 1.8 | 0.3 | 27.9 | 559.9 | 1.9 |
| 22ELAC033 | 17 | 18 | 1 | 177.7 | 275.2 | 26.9 | 80.1 | 8.8 | 2.1 | 7.0 | 0.8 | 4.7 | 1.0 | 2.8 | 0.4 | 2.4 | 0.4 | 40.3 | 630.6 | 1.7 |
Page 14
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LinkedIn – Mt Monger Resources
==> picture [113 x 18] intentionally omitted <==
==> picture [113 x 18] intentionally omitted <==
==> picture [113 x 18] intentionally omitted <==
| Hole ID | From (m) |
To (m) |
Interval (m) |
La2O3 (ppm) |
CeO2 (ppm) |
Pr6O11 (ppm) |
Nd2O3 (ppm) |
Sm2O3 (ppm) |
Eu2O3 (ppm) |
Gd2O3 (ppm) |
Tb4O7 (ppm) |
Dy2O3 (ppm) |
Ho2O3 (ppm) |
Er2O3 (ppm) |
Tm2O3 (ppm) |
Yb2O3 (ppm) |
Lu2O3 (ppm) |
Y2O3 (ppm) |
TREO (ppm) |
Sc2O3 (ppm) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 22ELAC033 | 18 | 19 | 1 | 281.5 | 363.6 | 46.5 | 127.7 | 12.2 | 2.6 | 8.4 | 0.9 | 4.4 | 0.9 | 2.4 | 0.3 | 1.9 | 0.3 | 33.0 | 886.6 | 2.1 |
| 22ELAC033 | 19 | 20 | 1 | 226.9 | 273.9 | 38.1 | 102.3 | 10.1 | 2.1 | 5.8 | 0.6 | 2.9 | 0.5 | 1.5 | 0.2 | 1.2 | 0.2 | 21.1 | 687.5 | 1.7 |
| 22ELAC033 | 20 | 21 | 1 | 183.0 | 599.5 | 29.8 | 85.3 | 9.8 | 2.2 | 6.5 | 0.7 | 3.5 | 0.7 | 1.9 | 0.2 | 1.4 | 0.2 | 33.1 | 957.8 | 1.7 |
| 22ELAC033 | 21 | 22 | 1 | 102.5 | 199.0 | 16.6 | 46.4 | 5.3 | 1.2 | 3.2 | 0.4 | 1.7 | 0.3 | 0.9 | 0.1 | 0.7 | 0.1 | 13.3 | 391.6 | 1.5 |
| 22ELAC033 | 22 | 23 | 1 | 171.8 | 168.9 | 25.0 | 70.1 | 6.7 | 1.4 | 3.8 | 0.4 | 1.9 | 0.3 | 0.9 | 0.1 | 0.8 | 0.1 | 13.1 | 465.4 | 1.5 |
| 22ELAC033 | 23 | 24 | 1 | 124.3 | 140.0 | 17.3 | 49.1 | 5.2 | 1.2 | 3.3 | 0.3 | 1.6 | 0.3 | 0.8 | 0.1 | 0.7 | 0.1 | 12.0 | 356.4 | 2.1 |
| 22ELAC033 | 24 | 25 | 1 | 151.9 | 229.7 | 21.6 | 60.4 | 6.5 | 1.3 | 3.6 | 0.4 | 1.7 | 0.3 | 0.9 | 0.1 | 0.8 | 0.1 | 11.6 | 491.0 | 2.8 |
| 22ELAC033 | 25 | 26 | 1 | 102.7 | 166.4 | 15.6 | 42.9 | 5.0 | 1.1 | 3.0 | 0.4 | 1.7 | 0.3 | 0.9 | 0.1 | 0.8 | 0.1 | 11.0 | 352.1 | 2.7 |
| 22ELAC034 | 30 | 31 | 1 | 105.9 | 186.1 | 16.8 | 47.9 | 5.8 | 1.3 | 3.5 | 0.4 | 1.9 | 0.3 | 0.9 | 0.1 | 0.9 | 0.1 | 10.6 | 382.6 | 4.2 |
| 22ELAC034 | 31 | 32 | 1 | 194.1 | 331.7 | 33.1 | 92.3 | 10.1 | 2.1 | 5.6 | 0.6 | 2.8 | 0.5 | 1.3 | 0.2 | 1.1 | 0.2 | 14.7 | 690.2 | 3.7 |
| 22ELAC034 | 32 | 33 | 1 | 227.5 | 366.1 | 37.1 | 104.2 | 12.0 | 2.6 | 6.6 | 0.7 | 3.5 | 0.6 | 1.6 | 0.2 | 1.5 | 0.2 | 18.1 | 782.5 | 4.3 |
| 22ELAC034 | 33 | 34 | 1 | 128.4 | 225.4 | 21.4 | 62.2 | 7.3 | 1.5 | 4.2 | 0.5 | 2.3 | 0.4 | 1.1 | 0.2 | 1.0 | 0.2 | 13.7 | 469.7 | 6.1 |
| 22ELAC034 | 34 | 35 | 1 | 173.6 | 305.9 | 28.9 | 83.9 | 9.3 | 2.0 | 5.2 | 0.5 | 2.6 | 0.5 | 1.2 | 0.2 | 1.0 | 0.2 | 15.2 | 630.0 | 3.2 |
| 22ELAC034 | 35 | 36 | 1 | 94.3 | 168.3 | 15.9 | 46.4 | 5.5 | 1.2 | 3.2 | 0.4 | 1.7 | 0.3 | 0.8 | 0.1 | 0.7 | 0.1 | 10.1 | 349.0 | 4.1 |
| 22ELAC035 | 20 | 21 | 1 | 4.0 | 5.5 | 1.0 | 3.2 | 0.8 | 0.3 | 0.9 | 0.2 | 1.2 | 0.3 | 0.9 | 0.1 | 1.0 | 0.1 | 5.2 | 24.5 | 63.2 |
| 22ELAC035 | 21 | 22 | 1 | 42.1 | 54.9 | 8.6 | 26.0 | 3.9 | 1.0 | 3.2 | 0.5 | 3.1 | 0.7 | 1.9 | 0.3 | 2.0 | 0.3 | 14.7 | 163.2 | 74.1 |
| 22ELAC035 | 22 | 23 | 1 | 16.8 | 48.9 | 3.8 | 12.1 | 2.3 | 0.7 | 2.3 | 0.4 | 2.9 | 0.7 | 2.0 | 0.3 | 2.1 | 0.3 | 14.2 | 109.8 | 75.3 |
| 22ELAC035 | 23 | 24 | 1 | 12.6 | 524.5 | 3.0 | 9.4 | 1.8 | 0.6 | 1.8 | 0.4 | 2.4 | 0.5 | 1.6 | 0.3 | 1.7 | 0.2 | 10.2 | 571.2 | 80.7 |
| 22ELAC035 | 24 | 25 | 1 | 12.6 | 70.0 | 3.2 | 10.3 | 2.2 | 0.7 | 2.4 | 0.5 | 3.2 | 0.7 | 2.1 | 0.3 | 2.3 | 0.3 | 13.2 | 124.0 | 75.6 |
| 22ELAC035 | 25 | 26 | 1 | 15.9 | 831.6 | 4.1 | 12.9 | 2.6 | 0.8 | 2.6 | 0.5 | 3.3 | 0.7 | 2.1 | 0.3 | 2.2 | 0.3 | 12.4 | 892.4 | 74.1 |
| 22ELAC035 | 26 | 27 | 1 | 81.6 | 313.2 | 17.4 | 53.0 | 8.7 | 2.4 | 6.9 | 1.1 | 6.2 | 1.2 | 3.2 | 0.5 | 3.0 | 0.4 | 22.3 | 521.0 | 75.9 |
| 22ELAC035 | 27 | 28 | 1 | 55.9 | 19.4 | 11.4 | 37.4 | 6.9 | 2.0 | 6.4 | 1.0 | 6.2 | 1.3 | 3.6 | 0.6 | 3.7 | 0.6 | 25.1 | 181.5 | 71.8 |
| 22ELAC035 | 28 | 29 | 1 | 21.4 | 33.2 | 4.3 | 14.8 | 3.0 | 0.9 | 3.2 | 0.6 | 3.6 | 0.8 | 2.2 | 0.4 | 2.3 | 0.3 | 13.5 | 104.5 | 73.9 |
| 22ELAC035 | 29 | 30 | 1 | 55.9 | 68.7 | 11.4 | 38.1 | 7.4 | 2.2 | 7.0 | 1.1 | 6.8 | 1.3 | 3.6 | 0.6 | 3.4 | 0.5 | 27.2 | 235.2 | 75.2 |
| 22ELAC036 | 15 | 16 | 1 | 24.0 | 64.7 | 4.5 | 14.4 | 2.5 | 0.7 | 2.3 | 0.4 | 2.1 | 0.4 | 1.4 | 0.2 | 1.5 | 0.2 | 13.1 | 132.7 | 27.1 |
| 22ELAC036 | 16 | 17 | 1 | 136.0 | 297.3 | 29.1 | 93.9 | 14.6 | 3.5 | 12.0 | 1.7 | 8.7 | 1.7 | 4.2 | 0.7 | 3.3 | 0.5 | 42.2 | 649.3 | 34.7 |
| 22ELAC036 | 17 | 18 | 1 | 27.4 | 51.6 | 4.6 | 15.2 | 2.4 | 0.6 | 2.4 | 0.4 | 2.3 | 0.5 | 1.4 | 0.2 | 1.4 | 0.2 | 13.4 | 124.0 | 34.8 |
| 22ELAC036 | 18 | 19 | 1 | 17.1 | 28.9 | 2.8 | 9.1 | 1.4 | 0.4 | 1.5 | 0.3 | 1.7 | 0.4 | 1.3 | 0.2 | 1.3 | 0.2 | 12.0 | 78.7 | 60.6 |
| 22ELAC036 | 19 | 20 | 1 | 5.8 | 6.9 | 0.6 | 2.0 | 0.4 | 0.1 | 0.4 | 0.1 | 0.6 | 0.2 | 0.5 | 0.1 | 0.6 | 0.1 | 4.2 | 22.7 | 62.7 |
| 22ELAC036 | 20 | 21 | 1 | 6.1 | 8.8 | 0.9 | 2.8 | 0.6 | 0.2 | 0.6 | 0.1 | 0.8 | 0.2 | 0.5 | 0.1 | 0.8 | 0.1 | 4.8 | 27.2 | 69.9 |
| 22ELAC036 | 21 | 22 | 1 | 20.0 | 28.6 | 2.9 | 8.6 | 1.3 | 0.3 | 1.1 | 0.2 | 1.1 | 0.3 | 0.7 | 0.1 | 0.7 | 0.1 | 6.6 | 72.5 | 54.4 |
| 22ELAC036 | 22 | 23 | 1 | 34.4 | 49.5 | 4.4 | 11.8 | 1.5 | 0.4 | 1.3 | 0.2 | 1.1 | 0.2 | 0.7 | 0.1 | 0.6 | 0.1 | 7.3 | 113.7 | 55.8 |
| 22ELAC036 | 23 | 24 | 1 | 258.0 | 389.4 | 34.3 | 90.2 | 10.8 | 2.6 | 8.5 | 1.1 | 5.8 | 1.1 | 3.0 | 0.4 | 2.4 | 0.4 | 39.7 | 847.9 | 25.6 |
| 22ELAC036 | 24 | 25 | 1 | 140.1 | 214.4 | 18.5 | 51.0 | 6.7 | 1.7 | 5.3 | 0.7 | 3.8 | 0.8 | 2.4 | 0.4 | 2.2 | 0.3 | 30.1 | 478.5 | 18.3 |
| 22ELAC036 | 25 | 26 | 1 | 121.4 | 185.5 | 16.9 | 44.8 | 5.6 | 1.4 | 4.2 | 0.5 | 3.0 | 0.6 | 1.7 | 0.2 | 1.5 | 0.2 | 20.6 | 408.0 | 36.8 |
| 22ELAC036 | 26 | 27 | 1 | 148.9 | 256.7 | 23.6 | 70.3 | 9.3 | 2.4 | 7.0 | 0.9 | 4.7 | 1.0 | 2.8 | 0.4 | 2.4 | 0.4 | 34.8 | 565.7 | 8.5 |
| 22ELAC039 | 24 | 25 | 1 | 18.4 | 31.6 | 3.5 | 10.1 | 1.4 | 0.3 | 1.0 | 0.2 | 1.0 | 0.2 | 0.7 | 0.1 | 0.8 | 0.1 | 5.0 | 74.4 | 77.8 |
Page 15
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==> picture [113 x 18] intentionally omitted <==
==> picture [113 x 18] intentionally omitted <==
==> picture [113 x 18] intentionally omitted <==
| Hole ID | From (m) |
To (m) |
Interval (m) |
La2O3 (ppm) |
CeO2 (ppm) |
Pr6O11 (ppm) |
Nd2O3 (ppm) |
Sm2O3 (ppm) |
Eu2O3 (ppm) |
Gd2O3 (ppm) |
Tb4O7 (ppm) |
Dy2O3 (ppm) |
Ho2O3 (ppm) |
Er2O3 (ppm) |
Tm2O3 (ppm) |
Yb2O3 (ppm) |
Lu2O3 (ppm) |
Y2O3 (ppm) |
TREO (ppm) |
Sc2O3 (ppm) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 22ELAC039 | 25 | 26 | 1 | 17.7 | 87.0 | 3.5 | 10.1 | 1.5 | 0.4 | 1.2 | 0.2 | 1.0 | 0.2 | 0.7 | 0.1 | 0.8 | 0.1 | 5.9 | 130.4 | 77.9 |
| 22ELAC039 | 26 | 27 | 1 | 516.0 | 836.5 | 104.8 | 311.4 | 43.0 | 10.6 | 31.1 | 4.2 | 21.7 | 3.9 | 9.4 | 1.2 | 6.1 | 0.8 | 81.4 | 1982.2 | 92.5 |
| 22ELAC039 | 27 | 28 | 1 | 70.5 | 115.3 | 13.2 | 39.7 | 5.6 | 1.5 | 4.2 | 0.6 | 3.1 | 0.6 | 1.5 | 0.2 | 1.3 | 0.2 | 13.5 | 271.0 | 82.4 |
| 22ELAC039 | 28 | 29 | 1 | 562.9 | 685.4 | 87.7 | 284.6 | 40.8 | 11.4 | 38.3 | 5.3 | 28.9 | 5.5 | 13.4 | 1.7 | 9.2 | 1.2 | 137.1 | 1913.7 | 82.4 |
| 22ELAC039 | 29 | 30 | 1 | 119.6 | 179.3 | 16.4 | 55.5 | 9.2 | 2.7 | 10.1 | 1.5 | 8.3 | 1.7 | 4.4 | 0.6 | 3.7 | 0.6 | 41.8 | 455.5 | 68.9 |
| 22ELAC040 | 23 | 24 | 1 | 1.7 | 3.8 | 0.4 | 1.4 | 0.4 | 0.1 | 0.6 | 0.1 | 1.1 | 0.3 | 1.0 | 0.2 | 1.2 | 0.2 | 6.6 | 19.1 | 104.5 |
| 22ELAC040 | 24 | 25 | 1 | 72.8 | 172.6 | 22.9 | 90.7 | 22.3 | 7.0 | 21.8 | 3.4 | 19.7 | 3.9 | 10.7 | 1.6 | 9.4 | 1.4 | 92.1 | 552.3 | 129.6 |
| 22ELAC040 | 25 | 26 | 1 | 281.5 | 800.9 | 105.7 | 424.6 | 99.8 | 32.3 | 103.8 | 15.6 | 88.6 | 16.1 | 41.9 | 5.9 | 35.2 | 4.8 | 369.5 | 2426.2 | 128.7 |
| 22ELAC040 | 26 | 27 | 1 | 146.0 | 321.8 | 43.4 | 176.7 | 42.2 | 14.3 | 46.2 | 7.0 | 37.9 | 6.9 | 17.2 | 2.4 | 13.7 | 1.8 | 147.3 | 1024.9 | 99.7 |
| 22ELAC040 | 27 | 28 | 1 | 37.1 | 78.9 | 8.7 | 37.1 | 9.8 | 3.5 | 14.8 | 2.7 | 18.9 | 4.8 | 16.4 | 2.2 | 15.7 | 2.3 | 152.4 | 405.3 | 91.4 |
| 22ELAC040 | 28 | 29 | 1 | 4.9 | 13.0 | 1.3 | 5.7 | 2.2 | 1.0 | 6.2 | 1.4 | 11.9 | 3.2 | 11.2 | 1.6 | 11.3 | 1.6 | 99.7 | 176.1 | 98.3 |
| 22ELAC040 | 29 | 30 | 1 | 7.4 | 13.7 | 1.6 | 7.3 | 2.4 | 1.0 | 5.1 | 1.1 | 8.6 | 2.3 | 8.0 | 1.1 | 7.5 | 1.1 | 75.2 | 143.3 | 72.4 |
| 22ELAC040 | 30 | 31 | 1 | 8.1 | 13.5 | 1.8 | 8.3 | 2.7 | 1.1 | 5.1 | 1.1 | 8.0 | 2.1 | 7.2 | 1.0 | 7.0 | 1.0 | 67.6 | 135.6 | 67.5 |
| 22ELAC040 | 31 | 32 | 1 | 9.1 | 14.9 | 2.2 | 9.5 | 2.8 | 1.1 | 4.5 | 0.9 | 6.8 | 1.7 | 5.9 | 0.8 | 5.7 | 0.8 | 55.1 | 121.8 | 77.9 |
| 22ELAC040 | 32 | 33 | 1 | 8.6 | 15.6 | 2.1 | 9.7 | 3.0 | 1.3 | 5.6 | 1.2 | 9.1 | 2.4 | 8.2 | 1.1 | 7.9 | 1.2 | 80.5 | 157.4 | 64.0 |
| 22ELAC040 | 33 | 34 | 1 | 7.7 | 13.4 | 1.9 | 8.8 | 3.0 | 1.2 | 6.2 | 1.3 | 10.1 | 2.6 | 9.0 | 1.2 | 8.4 | 1.2 | 91.4 | 167.4 | 60.9 |
| 22ELAC040 | 34 | 35 | 1 | 3.1 | 6.0 | 0.8 | 3.7 | 1.2 | 0.6 | 2.5 | 0.6 | 4.3 | 1.1 | 3.7 | 0.5 | 3.5 | 0.5 | 33.5 | 65.6 | 61.5 |
| 22ELAC040 | 35 | 36 | 1 | 3.9 | 7.8 | 1.1 | 5.2 | 1.9 | 0.8 | 3.3 | 0.7 | 5.0 | 1.2 | 4.0 | 0.6 | 3.9 | 0.6 | 36.1 | 76.0 | 58.6 |
| 22ELAC040 | 36 | 37 | 1 | 2.7 | 6.0 | 0.7 | 3.3 | 1.2 | 0.5 | 2.2 | 0.5 | 3.3 | 0.8 | 2.7 | 0.4 | 2.6 | 0.4 | 22.4 | 49.8 | 62.0 |
| 22ELAC040 | 37 | 38 | 1 | 13.4 | 27.1 | 3.6 | 15.5 | 4.1 | 1.4 | 5.0 | 0.8 | 5.1 | 1.1 | 3.2 | 0.4 | 3.0 | 0.4 | 29.1 | 113.2 | 71.5 |
| 22ELAC040 | 38 | 39 | 1 | 21.2 | 41.2 | 4.5 | 17.3 | 4.2 | 1.5 | 5.6 | 1.0 | 6.8 | 1.6 | 5.3 | 0.7 | 5.1 | 0.7 | 45.7 | 162.6 | 52.3 |
| 22ELAC040 | 39 | 40 | 1 | 2.9 | 8.2 | 0.7 | 3.3 | 1.1 | 0.4 | 2.2 | 0.4 | 3.2 | 0.8 | 2.7 | 0.4 | 2.5 | 0.3 | 23.6 | 52.7 | 66.9 |
| 22ELAC040 | 40 | 41 | 1 | 3.0 | 7.1 | 0.8 | 3.6 | 1.2 | 0.5 | 2.2 | 0.4 | 3.2 | 0.8 | 2.7 | 0.3 | 2.5 | 0.4 | 25.1 | 53.8 | 64.9 |
| 22ELAC040 | 41 | 42 | 1 | 5.3 | 14.3 | 1.3 | 5.6 | 2.0 | 0.8 | 3.6 | 0.8 | 6.2 | 1.6 | 5.7 | 0.7 | 5.1 | 0.7 | 60.7 | 114.4 | 71.8 |
| 22ELAC040 | 42 | 43 | 1 | 39.6 | 73.7 | 7.8 | 31.0 | 7.3 | 2.6 | 10.1 | 1.7 | 11.1 | 2.7 | 8.8 | 1.1 | 7.4 | 1.1 | 103.4 | 309.4 | 68.4 |
| 22ELAC040 | 43 | 44 | 1 | 66.7 | 111.9 | 10.8 | 33.6 | 5.5 | 1.5 | 5.8 | 0.9 | 5.8 | 1.4 | 4.6 | 0.6 | 4.2 | 0.6 | 55.7 | 309.6 | 4.8 |
| 22ELAC040 | 44 | 45 | 1 | 111.7 | 188.6 | 17.4 | 49.3 | 5.5 | 1.3 | 4.0 | 0.5 | 3.1 | 0.7 | 2.1 | 0.3 | 1.7 | 0.2 | 27.3 | 413.7 | 3.6 |
| 22ELAC040 | 45 | 46 | 1 | 32.4 | 65.1 | 6.1 | 19.1 | 3.2 | 0.8 | 2.6 | 0.4 | 2.4 | 0.5 | 1.7 | 0.2 | 1.5 | 0.2 | 20.5 | 156.8 | 4.2 |
| 22ELAC042 | 27 | 28 | 1 | 147.8 | 264.1 | 32.4 | 113.4 | 17.3 | 4.0 | 12.6 | 1.4 | 6.7 | 1.1 | 2.7 | 0.3 | 1.9 | 0.2 | 28.6 | 634.4 | 8.6 |
| 22ELAC042 | 28 | 29 | 1 | 77.1 | 163.4 | 21.6 | 74.4 | 11.3 | 2.1 | 6.5 | 0.8 | 3.5 | 0.6 | 1.6 | 0.2 | 1.3 | 0.2 | 17.1 | 381.6 | 7.3 |
| 22ELAC042 | 29 | 30 | 1 | 105.9 | 199.6 | 29.7 | 99.1 | 14.4 | 2.7 | 8.5 | 1.0 | 4.2 | 0.8 | 1.9 | 0.2 | 1.5 | 0.2 | 20.1 | 489.9 | 9.5 |
| 22ELAC042 | 30 | 31 | 1 | 130.8 | 171.4 | 37.5 | 126.6 | 18.0 | 3.4 | 10.2 | 1.1 | 4.8 | 0.8 | 2.1 | 0.3 | 1.6 | 0.2 | 24.2 | 532.9 | 11.4 |
| 22ELAC042 | 31 | 32 | 1 | 80.5 | 168.9 | 17.1 | 53.7 | 7.5 | 1.5 | 4.9 | 0.6 | 2.9 | 0.6 | 1.6 | 0.2 | 1.3 | 0.2 | 17.2 | 358.6 | 7.2 |
| 22ELAC042 | 32 | 33 | 1 | 52.2 | 97.5 | 11.1 | 36.0 | 5.4 | 1.2 | 3.4 | 0.4 | 2.1 | 0.4 | 1.1 | 0.1 | 1.0 | 0.1 | 12.8 | 224.8 | 6.5 |
| 22ELAC042 | 33 | 34 | 1 | 41.5 | 75.5 | 9.2 | 31.1 | 4.9 | 1.2 | 3.3 | 0.4 | 1.8 | 0.3 | 0.9 | 0.1 | 0.8 | 0.1 | 10.4 | 181.7 | 4.7 |
| 22ELAC042 | 34 | 35 | 1 | 51.4 | 101.0 | 10.9 | 37.1 | 6.0 | 1.2 | 4.3 | 0.5 | 2.5 | 0.5 | 1.3 | 0.2 | 1.2 | 0.2 | 14.3 | 232.5 | 7.4 |
| 22ELAC043 | 3 | 4 | 1 | 27.7 | 65.1 | 5.7 | 18.4 | 3.0 | 0.6 | 2.6 | 0.4 | 2.3 | 0.5 | 1.5 | 0.2 | 1.4 | 0.2 | 15.3 | 144.8 | 18.3 |
Page 16
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==> picture [113 x 18] intentionally omitted <==
==> picture [113 x 18] intentionally omitted <==
==> picture [113 x 18] intentionally omitted <==
| Hole ID | From (m) |
To (m) |
Interval (m) |
La2O3 (ppm) |
CeO2 (ppm) |
Pr6O11 (ppm) |
Nd2O3 (ppm) |
Sm2O3 (ppm) |
Eu2O3 (ppm) |
Gd2O3 (ppm) |
Tb4O7 (ppm) |
Dy2O3 (ppm) |
Ho2O3 (ppm) |
Er2O3 (ppm) |
Tm2O3 (ppm) |
Yb2O3 (ppm) |
Lu2O3 (ppm) |
Y2O3 (ppm) |
TREO (ppm) |
Sc2O3 (ppm) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 22ELAC043 | 4 | 5 | 1 | 82.6 | 267.8 | 15.6 | 51.1 | 8.3 | 1.8 | 7.9 | 1.2 | 6.6 | 1.3 | 4.0 | 0.5 | 3.3 | 0.5 | 43.7 | 496.2 | 19.6 |
| 22ELAC043 | 5 | 6 | 1 | 84.2 | 213.1 | 15.6 | 51.2 | 8.4 | 1.9 | 7.7 | 1.2 | 6.5 | 1.3 | 4.1 | 0.5 | 3.4 | 0.5 | 43.9 | 443.5 | 19.5 |
| 22ELAC043 | 6 | 7 | 1 | 68.0 | 84.5 | 9.3 | 28.8 | 4.0 | 0.8 | 3.5 | 0.5 | 2.8 | 0.6 | 1.9 | 0.3 | 1.8 | 0.3 | 19.5 | 226.6 | 7.6 |
| 22ELAC043 | 7 | 8 | 1 | 71.2 | 124.7 | 11.3 | 33.1 | 4.9 | 0.9 | 3.5 | 0.5 | 2.9 | 0.6 | 1.9 | 0.3 | 1.9 | 0.2 | 17.3 | 275.1 | 7.0 |
| 22ELAC043 | 8 | 9 | 1 | 90.7 | 191.6 | 22.7 | 69.3 | 9.8 | 1.5 | 6.0 | 0.8 | 4.4 | 0.9 | 2.6 | 0.3 | 2.3 | 0.3 | 22.9 | 426.1 | 7.8 |
| 22ELAC043 | 9 | 10 | 1 | 105.2 | 184.3 | 19.5 | 57.6 | 7.9 | 1.2 | 5.2 | 0.8 | 4.0 | 0.8 | 2.4 | 0.3 | 2.2 | 0.3 | 20.4 | 412.0 | 6.2 |
| 22ELAC043 | 10 | 11 | 1 | 184.7 | 398.0 | 36.5 | 108.1 | 14.1 | 2.0 | 8.3 | 1.1 | 5.4 | 1.0 | 2.8 | 0.4 | 2.5 | 0.3 | 26.3 | 791.6 | 6.4 |
| 22ELAC043 | 11 | 12 | 1 | 154.8 | 444.7 | 32.0 | 93.8 | 11.7 | 1.8 | 6.3 | 0.8 | 4.2 | 0.8 | 2.3 | 0.3 | 2.1 | 0.3 | 20.8 | 776.5 | 5.6 |
| 22ELAC043 | 12 | 13 | 1 | 293.2 | 1201.4 | 89.5 | 286.9 | 38.0 | 5.6 | 17.1 | 2.0 | 9.3 | 1.4 | 3.9 | 0.5 | 3.5 | 0.4 | 35.9 | 1988.8 | 6.2 |
| 22ELAC043 | 13 | 14 | 1 | 340.1 | 1289.8 | 84.3 | 269.4 | 36.4 | 5.7 | 21.2 | 2.6 | 12.3 | 2.1 | 5.9 | 0.8 | 5.0 | 0.6 | 58.5 | 2134.8 | 6.3 |
| 22ELAC043 | 14 | 15 | 1 | 245.1 | 523.3 | 62.7 | 204.7 | 28.1 | 4.9 | 17.1 | 2.0 | 9.3 | 1.5 | 4.0 | 0.5 | 3.1 | 0.4 | 41.0 | 1147.6 | 4.6 |
| 22ELAC043 | 15 | 16 | 1 | 551.2 | 567.5 | 168.5 | 605.4 | 87.8 | 16.3 | 56.4 | 6.5 | 30.4 | 4.8 | 12.3 | 1.6 | 9.0 | 1.1 | 131.4 | 2250.2 | 3.7 |
| 22ELAC043 | 16 | 17 | 1 | 213.4 | 211.9 | 59.1 | 217.0 | 32.4 | 6.5 | 26.9 | 3.4 | 18.0 | 3.5 | 11.0 | 1.5 | 9.6 | 1.4 | 129.5 | 944.9 | 5.8 |
| 22ELAC043 | 17 | 18 | 1 | 157.2 | 215.0 | 37.5 | 130.1 | 19.0 | 3.7 | 14.5 | 1.7 | 8.3 | 1.5 | 4.3 | 0.6 | 3.5 | 0.5 | 47.7 | 644.9 | 13.6 |
| 22ELAC043 | 18 | 19 | 1 | 178.9 | 277.6 | 40.7 | 134.1 | 20.0 | 4.0 | 15.8 | 1.8 | 8.7 | 1.5 | 4.2 | 0.5 | 3.1 | 0.4 | 47.4 | 738.8 | 6.0 |
| 22ELAC043 | 19 | 20 | 1 | 107.7 | 173.2 | 20.6 | 68.5 | 10.0 | 2.2 | 8.6 | 1.0 | 5.3 | 0.9 | 2.7 | 0.4 | 2.2 | 0.3 | 31.4 | 434.9 | 4.8 |
| 22ELAC043 | 20 | 21 | 1 | 44.8 | 95.3 | 10.6 | 34.8 | 5.4 | 1.1 | 4.2 | 0.5 | 2.9 | 0.5 | 1.7 | 0.2 | 1.7 | 0.2 | 18.4 | 222.4 | 11.5 |
| 22ELAC043 | 21 | 22 | 1 | 39.6 | 82.1 | 7.6 | 26.0 | 3.5 | 0.8 | 2.4 | 0.3 | 1.8 | 0.4 | 1.0 | 0.2 | 0.9 | 0.1 | 11.9 | 178.6 | 3.0 |
| 22ELAC043 | 22 | 23 | 1 | 26.3 | 55.0 | 5.8 | 18.8 | 2.6 | 0.7 | 1.5 | 0.2 | 1.1 | 0.2 | 0.6 | 0.1 | 0.6 | 0.1 | 6.7 | 120.2 | 2.0 |
| 22ELAC043 | 23 | 24 | 1 | 28.7 | 82.9 | 5.9 | 19.9 | 2.8 | 0.7 | 1.8 | 0.2 | 1.3 | 0.3 | 0.7 | 0.1 | 0.7 | 0.1 | 7.8 | 153.9 | 3.2 |
| 22ELAC043 | 24 | 25 | 1 | NA | ||||||||||||||||
| 22ELAC043 | 25 | 26 | 1 | 23.9 | 45.5 | 4.3 | 13.6 | 2.0 | 0.5 | 1.2 | 0.2 | 1.0 | 0.2 | 0.7 | 0.1 | 0.7 | 0.1 | 8.4 | 102.4 | 2.6 |
| 22ELAC043 | 26 | 27 | 1 | 111.8 | 237.7 | 19.1 | 62.8 | 8.6 | 1.8 | 5.2 | 0.8 | 4.0 | 0.9 | 2.3 | 0.4 | 1.9 | 0.3 | 28.8 | 486.3 | 6.6 |
| 22ELAC043 | 27 | 28 | 1 | 64.6 | 256.7 | 13.8 | 48.9 | 7.0 | 1.5 | 4.0 | 0.5 | 2.5 | 0.5 | 1.1 | 0.1 | 0.8 | 0.1 | 13.5 | 415.7 | 3.1 |
| 22ELAC043 | 28 | 29 | 1 | 247.5 | 515.9 | 48.9 | 171.5 | 24.0 | 4.4 | 14.9 | 2.0 | 11.0 | 2.2 | 5.6 | 0.8 | 4.0 | 0.6 | 73.5 | 1126.7 | 5.5 |
| 22ELAC045 | 3 | 4 | 1 | 24.5 | 45.5 | 4.9 | 16.0 | 2.9 | 0.6 | 2.4 | 0.3 | 2.0 | 0.4 | 1.2 | 0.2 | 1.3 | 0.2 | 11.2 | 113.6 | 16.0 |
| 22ELAC045 | 4 | 5 | 1 | 139.0 | 282.5 | 26.2 | 80.9 | 11.5 | 2.1 | 8.0 | 1.0 | 5.0 | 0.9 | 2.6 | 0.3 | 2.2 | 0.3 | 29.6 | 592.1 | 12.5 |
| 22ELAC045 | 5 | 6 | 1 | 144.3 | 234.0 | 27.2 | 83.3 | 10.6 | 1.8 | 5.7 | 0.6 | 2.9 | 0.5 | 1.3 | 0.2 | 1.1 | 0.1 | 15.6 | 529.0 | 4.6 |
| 22ELAC045 | 6 | 7 | 1 | 130.2 | 249.4 | 25.3 | 79.2 | 10.7 | 1.8 | 6.4 | 0.8 | 3.6 | 0.6 | 1.7 | 0.2 | 1.4 | 0.2 | 20.4 | 531.8 | 5.5 |
| 22ELAC045 | 7 | 8 | 1 | 88.9 | 162.8 | 17.2 | 54.1 | 8.2 | 1.3 | 5.2 | 0.6 | 3.3 | 0.5 | 1.5 | 0.2 | 1.2 | 0.2 | 15.7 | 361.2 | 4.8 |
| 22ELAC045 | 8 | 9 | 1 | 24.7 | 44.7 | 5.9 | 17.7 | 2.8 | 0.6 | 1.8 | 0.2 | 1.2 | 0.2 | 0.7 | 0.1 | 0.6 | 0.1 | 6.8 | 108.2 | 2.2 |
| 22ELAC046 | 6 | 7 | 1 | 54.5 | 146.2 | 12.0 | 41.1 | 7.5 | 1.6 | 6.7 | 0.9 | 5.2 | 1.0 | 2.9 | 0.4 | 2.5 | 0.4 | 29.7 | 312.4 | 21.4 |
| 22ELAC046 | 7 | 8 | 1 | 56.4 | 313.2 | 10.9 | 36.5 | 5.7 | 1.2 | 5.3 | 0.7 | 3.8 | 0.7 | 2.2 | 0.3 | 1.8 | 0.3 | 24.8 | 463.8 | 21.5 |
| 22ELAC046 | 8 | 9 | 1 | 27.2 | 154.8 | 6.7 | 23.4 | 5.0 | 1.1 | 4.9 | 0.7 | 4.3 | 0.8 | 2.4 | 0.3 | 2.0 | 0.3 | 26.5 | 260.6 | 17.3 |
| 22ELAC046 | 9 | 10 | 1 | 30.4 | 131.4 | 7.0 | 24.5 | 5.3 | 1.2 | 4.8 | 0.7 | 4.1 | 0.8 | 2.3 | 0.3 | 2.2 | 0.3 | 22.5 | 237.8 | 12.0 |
| 22ELAC046 | 10 | 11 | 1 | 58.4 | 55.0 | 8.8 | 27.3 | 4.2 | 0.8 | 3.6 | 0.5 | 2.7 | 0.5 | 1.5 | 0.2 | 1.3 | 0.2 | 17.3 | 182.3 | 8.4 |
| 22ELAC046 | 11 | 12 | 1 | 38.8 | 25.7 | 4.8 | 13.1 | 2.2 | 0.4 | 1.7 | 0.3 | 1.5 | 0.3 | 0.9 | 0.1 | 0.9 | 0.1 | 9.9 | 100.7 | 8.2 |
Page 17
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LinkedIn – Mt Monger Resources
==> picture [113 x 18] intentionally omitted <==
==> picture [113 x 18] intentionally omitted <==
==> picture [113 x 18] intentionally omitted <==
| Hole ID | From (m) |
To (m) |
Interval (m) |
La2O3 (ppm) |
CeO2 (ppm) |
Pr6O11 (ppm) |
Nd2O3 (ppm) |
Sm2O3 (ppm) |
Eu2O3 (ppm) |
Gd2O3 (ppm) |
Tb4O7 (ppm) |
Dy2O3 (ppm) |
Ho2O3 (ppm) |
Er2O3 (ppm) |
Tm2O3 (ppm) |
Yb2O3 (ppm) |
Lu2O3 (ppm) |
Y2O3 (ppm) |
TREO (ppm) |
Sc2O3 (ppm) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 22ELAC046 | 12 | 13 | 1 | 9.4 | 7.1 | 1.2 | 3.5 | 0.5 | 0.3 | 0.6 | 0.1 | 0.4 | 0.1 | 0.3 | 0.0 | 0.3 | 0.0 | 3.5 | 27.4 | 3.4 |
| 22ELAC046 | 13 | 14 | 1 | 19.8 | 17.6 | 2.9 | 8.7 | 1.3 | 0.2 | 1.1 | 0.1 | 0.8 | 0.2 | 0.5 | 0.1 | 0.5 | 0.1 | 6.5 | 60.5 | 9.2 |
| 22ELAC046 | 14 | 15 | 1 | 29.8 | 36.7 | 4.5 | 14.0 | 1.6 | 0.3 | 1.2 | 0.1 | 0.7 | 0.1 | 0.4 | 0.1 | 0.5 | 0.1 | 5.9 | 96.0 | 11.2 |
| 22ELAC046 | 15 | 16 | 1 | 120.2 | 208.8 | 21.7 | 66.1 | 9.5 | 1.3 | 6.3 | 0.8 | 4.4 | 0.8 | 2.4 | 0.4 | 2.5 | 0.3 | 25.7 | 471.3 | 7.5 |
| 22ELAC046 | 16 | 17 | 1 | 527.8 | 1083.4 | 108.3 | 291.6 | 32.4 | 3.8 | 14.1 | 1.6 | 6.7 | 1.0 | 2.6 | 0.3 | 2.1 | 0.3 | 31.4 | 2107.2 | 4.5 |
| 22ELAC048 | 18 | 19 | 1 | 79.6 | 176.9 | 13.0 | 37.1 | 5.3 | 0.7 | 3.4 | 0.5 | 2.3 | 0.4 | 1.2 | 0.2 | 1.2 | 0.2 | 11.8 | 333.7 | 10.3 |
| 22ELAC048 | 19 | 20 | 1 | 104.5 | 207.0 | 16.6 | 47.5 | 6.6 | 0.9 | 4.6 | 0.6 | 3.1 | 0.5 | 1.6 | 0.2 | 1.7 | 0.2 | 15.7 | 411.3 | 12.3 |
| 22ELAC048 | 20 | 21 | 1 | 171.8 | 325.5 | 28.8 | 82.2 | 11.3 | 1.5 | 7.0 | 0.9 | 4.3 | 0.7 | 2.1 | 0.3 | 1.8 | 0.2 | 22.1 | 660.6 | 11.7 |
| 22ELAC048 | 21 | 22 | 1 | 255.7 | 487.7 | 46.4 | 127.7 | 17.5 | 2.3 | 11.0 | 1.4 | 6.7 | 1.1 | 3.2 | 0.4 | 2.6 | 0.4 | 32.5 | 996.6 | 10.5 |
| 22ELAC048 | 22 | 23 | 1 | 328.4 | 574.9 | 56.7 | 152.2 | 20.6 | 2.9 | 12.8 | 1.6 | 7.8 | 1.3 | 3.9 | 0.5 | 3.2 | 0.4 | 42.0 | 1209.2 | 13.5 |
| 22ELAC048 | 23 | 24 | 1 | 328.4 | 598.2 | 58.5 | 155.7 | 20.5 | 2.5 | 12.0 | 1.5 | 7.0 | 1.2 | 3.3 | 0.4 | 2.9 | 0.4 | 36.1 | 1228.6 | 12.0 |
| 22ELAC048 | 24 | 25 | 1 | 269.7 | 500.0 | 51.1 | 139.4 | 19.1 | 2.6 | 11.2 | 1.4 | 6.6 | 1.1 | 3.1 | 0.4 | 2.8 | 0.4 | 32.1 | 1041.1 | 17.8 |
| 22ELAC048 | 25 | 26 | 1 | 281.5 | 506.1 | 49.4 | 129.5 | 17.4 | 2.4 | 9.8 | 1.3 | 6.2 | 1.1 | 3.0 | 0.4 | 2.9 | 0.4 | 32.3 | 1043.5 | 11.3 |
| 22ELAC048 | 26 | 27 | 1 | 387.0 | 713.7 | 71.6 | 195.4 | 25.3 | 3.1 | 14.0 | 1.7 | 7.9 | 1.3 | 3.5 | 0.5 | 3.1 | 0.4 | 37.1 | 1465.5 | 9.9 |
| 22ELAC048 | 27 | 28 | 1 | 445.7 | 1357.4 | 86.1 | 249.6 | 31.3 | 4.0 | 17.4 | 2.1 | 9.7 | 1.6 | 4.3 | 0.6 | 3.7 | 0.5 | 44.7 | 2258.7 | 11.9 |
| 22ELAC048 | 28 | 29 | 1 | 433.9 | 781.3 | 78.9 | 229.2 | 29.6 | 3.9 | 14.7 | 2.0 | 9.8 | 1.8 | 4.3 | 0.6 | 3.6 | 0.5 | 46.0 | 1640.0 | 11.8 |
| 22ELAC048 | 29 | 30 | 1 | 328.4 | 1095.7 | 73.3 | 223.4 | 31.0 | 4.4 | 15.8 | 2.2 | 10.7 | 1.9 | 4.8 | 0.7 | 3.9 | 0.5 | 49.0 | 1845.7 | 13.0 |
| 22ELAC048 | 30 | 31 | 1 | 175.3 | 534.4 | 29.8 | 94.6 | 12.3 | 2.0 | 7.0 | 1.0 | 5.4 | 1.0 | 2.7 | 0.4 | 2.3 | 0.3 | 27.2 | 895.7 | 6.7 |
| 22ELAC048 | 31 | 32 | 1 | 50.3 | 1332.8 | 9.7 | 31.6 | 5.0 | 0.8 | 3.3 | 0.5 | 2.9 | 0.6 | 1.7 | 0.3 | 1.9 | 0.3 | 16.7 | 1458.5 | 5.5 |
| 22ELAC048 | 32 | 33 | 1 | 387.0 | 421.3 | 66.6 | 188.4 | 24.6 | 3.7 | 11.3 | 1.6 | 8.3 | 1.5 | 3.8 | 0.5 | 3.1 | 0.4 | 41.1 | 1163.4 | 7.7 |
| 22ELAC048 | 33 | 34 | 1 | 445.7 | 652.3 | 92.3 | 278.8 | 37.5 | 5.5 | 18.2 | 2.5 | 12.0 | 2.2 | 5.3 | 0.7 | 4.2 | 0.6 | 52.7 | 1610.4 | 6.1 |
| 22ELAC048 | 34 | 35 | 1 | 293.2 | 554.0 | 71.8 | 239.1 | 34.9 | 5.5 | 20.5 | 2.9 | 15.2 | 2.9 | 7.4 | 1.0 | 5.7 | 0.8 | 79.4 | 1334.3 | 5.2 |
| 22ELAC048 | 35 | 36 | 1 | 363.6 | 606.8 | 88.4 | 300.9 | 43.4 | 7.1 | 26.5 | 3.5 | 18.2 | 3.3 | 8.0 | 1.1 | 6.2 | 0.9 | 89.5 | 1567.5 | 5.2 |
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APPENDIX V - JORC Compliance Tables
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Section 1 Sampling Techniques and Data
| Criteria | JORC Code Explanation | Commentary |
|---|---|---|
| Sampling techniques | Nature and quality of sampling (eg 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 (eg ‘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 (eg submarine nodules) may warrant disclosure of detailed information. |
Conventional Aircore (AC) drilling was used to obtain representative 1 metre samples of approximately 1.5kg using a rig-mounted cyclone and cone splitter. The remaining material from each metre was collected from the cyclone as a bulk sample of approximately 15-20kg. In the laboratory, samples are riffle split if required, then pulverised to a nominal 85% passing 75 microns to obtain a homogenous sub-sample for assay. Sampling was carried out under MTM's standard protocols and QAQC procedures and is considered standard industry practice. |
| Drilling techniques | Drill type (eg core, reverse circulation, open-hole hammer, rotary air blast, auger, Bangka, sonic, etc) and details (eg 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). |
Aircore drilling was completed using standard industry methods. Drilling used a 3 inch drill bit to refusal, usually saprock to fresh rock. Aircore is considered to be an appropriate drilling technique for saprolitic clay. |
| 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. |
AC drill samples recoveries were assessed visually but not recorded. Samples are not considered to be materially biased, given the nature of the geology and sampling method. Recoveries remained relatively consistent throughout the program and are estimated to be 100% for 95% of drilling. Poor (low) recovery intervals were logged and entered into the drill logs. The cone splitter was routinely cleaned and inspected during drilling. Care was taken to ensure calico samples were of consistent volume. |
| Logging | 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. _ |
AC samples were logged geologically on a one metre interval basis, including but not limited to: recording colour, weathering, regolith, lithology, veining, structure, texture, alteration and mineralisation (type and abundance). Logging was at a qualitative standard appropriate for AC drilling and is not suitable to support future Mineral Resource estimation. |
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| Criteria | JORC Code Explanation | Commentary |
|---|---|---|
| The total length and percentage of the relevant intersections logged. | Representative material was collected from each AC drill sample and stored in a chip tray. These chip trays were transferred to a secure Company storage facility located in Kalgoorlie. All holes and all relevant intersections weregeologicallylogged in full. |
|
| Sub-sampling techniques and sample preparation |
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. |
1m interval samples were submitted to the analytical laboratory for sample preparation. >95% of the samples were dry in nature. AC drilling samples were weighed, dried and pulverized to 85% passing 75 microns. This is considered industry standard and appropriate. MTM has its own internal QAQC procedure involving the use of certified reference materials (standards), blanks and field duplicates which account for approximately 5% of the total submitted samples. The sample sizes are considered appropriate for the style of precious metal mineralisation previously recorded for the area. |
| Quality of assay data and laboratory tests |
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 (eg standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (ie lack of bias) and precision have been established. |
1m drilling samples have been submitted for a multi-element assay technique (ME-MS61L) using multi-acid (4 acid) digestion with an ICP-MS and ICP-AES finish; and rare earth elements with a multi-element technique (MS61L-REE) using a multi-acid digestion (HF-HNO3-HClO4), HCl leach followed by ICP-MS analysis. The assay techniques are considered appropriate and are industry best standard. The techniques are considered to be a near total digest, only the most resistive minerals are only partially dissolved. An internal QAQC procedure involving the use of certified reference materials (standards), blanks and duplicates accounts for approximately 5% of the total submitted samples. The certified reference materials used have a representative range of values typical of low, moderate and high grade gold mineralisation. Standard results for drilling demonstrated assay values are both accurate and precise. Blank results demonstrate there is negligible cross-contamination between samples. Duplicate results suggest there is reasonable repeatabilitybetween samples. |
| Verification of sampling and assaying |
The verification of significant intersections by either independent or alternative company personnel. The use of twinned holes. |
Significant intersections have not been verified. No dedicated twin holes have yet been drilled for comparative purposes. Primary data was collected on paper log sheets and then transferred to digital logginghardware and software usingin-house loggingmethodologyand codes. |
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| Criteria | JORC Code Explanation | Commentary |
|---|---|---|
| Documentation of primary data, data entry procedures, data verification, data storage (physical and electronic) protocols. Discuss any adjustment to assay data. |
Logging data was sent to the Perth based office where the data was validated and entered into an industry standard master database maintained by the MTM database administrator. |
|
| 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. |
Hole collar locations are surveyed prior to rehabilitation with handheld GPS instruments with accuracy ±3m. Downhole surveys were not undertaken. The grid system used for location of all drill holes as shown in tables and on figures is MGA Zone 51, GDA94. Topographic control is based on handheld GPS, suitable for current stage of exploration. |
| Data spacing and distribution |
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. |
Drill hole spacing is variable, as shown in diagrams in the body of the announcement. Drill hole spacing and distribution is not considered sufficient as to make geological and grade continuity assumptions appropriate for Mineral Resource estimation. Drill hole samples were collected at 1m intervals. |
| Orientation of data in relation to geological structure |
Whether the orientation of sampling achieves unbiased sampling of possible structures and the extent to which this is known, considering the deposit type. 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 orientation of drilling and sampling is not anticipated to have any significant biasing effects. The drill holes reported in this announcement are vertical and are interpreted to have intersected the mineralised structures approximately perpendicular to their dip. |
| Sample security | The measures taken to ensure sample security. | Sample chain of custody is managed by MTM. Sampling is carried out by MTM field staff. Samples are transported to a laboratoryin Kalgoorlie byMTM employees. |
| Audits or reviews | The results of any audits or reviews of sampling techniques and data. | No audit or review has been completed. |
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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. |
The results relate to drilling completed on exploration licence E38/3499. The exploration licences are held 100% by Tevel Pty Ltd (Tevel). Mt Monger Resources Ltd has executed an earn-in and joint venture agreement with Tevel that entitles the Company to earn up to a 75% interest in the tenements. The tenement overlies the Laverton Downs pastoral lease. The tenements are held securely and no impediments to obtaining a licence to operate have been identified. |
| Exploration done by other parties |
Acknowledgment and appraisal of exploration by other parties. | The tenement contains extensive sedimentary cover and there has been minimal exploration in the area either by exploration companies or government geological surveys. Earliest exploration within the region was for diamonds, gold, nickel and uranium, with only a limited number of drill holes. Reconnaissance exploration activities including geophysical data interpretation and surface geochemical sampling, have identified a number of rare earth element anomalies requiring further follow up work. A number of early stage exploration programs including shallow RAB and aircore drillinghave been completed in the Pt Kidmanprospect areas. |
| Geology | Deposit type, geological setting and style of mineralisation. | The tenement area is located within the poorly understood Burtville Terrane on the eastern edge of the Eastern Goldfields Superterrane. Interpreted geology comprises predominantly Archaean granite gneiss with relatively narrow remnant greenstone units. The area contains limited outcrop, with the bedrock geology predominantly concealed by younger transported cover. The area is on the eastern fringe of the Yilgarn Craton, surrounded by existing and emerging world class gold camps. To the west, the +25 Moz Au Laverton Greenstone Belt is home to Sunrise Dam (10 Moz Au), Wallaby (8 Moz Au) and Granny Smith (2.5 Moz Au) and a suite of other nearby deposits. Gold production from the belt is estimated to be in excess of 28 Moz Au. Lying to the east of the area is the Yamarna Greenstone Belt, hosting the 6 Moz Au granitoid-host ed Gruyere deposit, whilst the 7.5 Moz Au granite gneiss-hosted Tropicana deposit is located in the Albany-Fraser Province to the southeast. Limited previous exploration within the Point Kidman project area has identified light rare earths(LREE)mineralisation hosted bylaterite clays and strongly |
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| Criteria | JORC Code Explanation | Commentary |
|---|---|---|
| weathered granites associated with Archaean granitoid terrane. Aircore drilling intersected anomalous LREE mineralisation (Ce, La, Nd, Pr and Sm) in reconnaissance aircore drill holes over a wide area that remain to be followed up with additional exploration. Very widely spaced Geological Survey of Western Australia (GSWA) rock chip samples in the area have returned anomalous REEs and indicates the size of the anomalous REE fingerprint in the region is much larger than the area drilled to date. |
||
| Drill hole Information | 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, including Easting and northing of the drill hole collar, Elevation or RL (Reduced Level – elevation above sea level in metres) of the drill hole collar, dip and azimuth of the hole, down hole length and interception depth plus 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. |
All material information is summarised in the Tables and Figures included in the body of the announcement. |
| Data aggregation methods |
In reporting Exploration Results, weighting averaging techniques, maximum and/or minimum grade truncations (eg 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 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. |
Length-weighted average grades are reported. No maximum grade truncations have been applied. Significant intersections are reported based on 300ppm total rare earth oxide (TREO) cut-off grade, with allowance for internal dilution by a maximum of one sub-grade sample. Where appropriate higher-grade intersections are reported based on a 1,000ppm TREO cut-off with no internal dilution. No metal equivalent values have been reported. Multi-element results (REE) are converted to stoichiometric oxide (REO) using element-to-stoichiometric oxide conversion factors. These stoichiometric conversion factors are stated in the table below and can be referenced in appropriate publicly available technical data. Rare earth oxide is the industry accepted form for reporting rare earths. The following calculations are used for compiling REO into their reporting and evaluation groups: Total rare earth oxide (TREO) values were derived by the simple addition of grades for lanthanum (La2O3), cerium (CeO2), praseodymium (Pr6O11), neodymium (Nd2O3), samarium (Sm2O3), europium (Eu2O3), gadolinium (Gd2O3),terbium(Tb4O7),dysprosium(Dy2O3),holmium(Ho2O3),erbium |
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| Criteria | JORC Code Explanation | Commentary | |
|---|---|---|---|
| |
(Er2O3), thulium (Tm2O3), ytterbium (Yb2O3), lutetium (Lu2O3) and yttrium (Y2O3). Heavy Rare Earth Oxide (HREO) grade includes Eu2O3, Gd2O3,Tb4O7,Dy2O3, Ho2O3,Er2O3, Tm2O3, Yb2O3, Lu2O3and Y2O3. Reported as percentage of TREO. Magnet Rare Earth Oxide (MREO) grade includes Nd2O3, Pr6O11, Sm2O3, Gd2O3, Tb4O7, Dy2O3,and Ho2O3. Shown as percentage of TREO. Critical Rare Earth Oxide (CREO) grade includes Nd2O3, Eu2O3, Tb4O7,Dy2O3 and Y2O3. Shown as percentage of TREO. Nd+Pr REO (NdPr) grade includes Nd2O3and Pr6O11. Element Conversion Factor Oxide Form Ce 1.2284 CeO2 Dy 1.1477 Dy2O3 Er 1.1435 Er2O3 Eu 1.1579 Eu2O3 Gd 1.1526 Gd2O3 Ho 1.1455 Ho2O3 La 1.1728 La2O3 Lu 1.1372 Lu2O3 Nd 1.1664 Nd2O3 Pr 1.2082 Pr6O11 Sc 1.5338 Sc2O3 Sm 1.1596 Sm2O3 Tb 1.1762 Tb4O7 Tm 1.1421 Tm2O3 Y 1.2699 Y2O3 Yb 1.1387 Yb2O3 |
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| Relationship between mineralisation widths and intercept lengths |
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 (eg ‘down hole length, true width not known’). |
|
Down hole lengths are reported. The mineralisation is assumed to be subhorizontal in orientation so true width and intercept length is approximately equal. Further drilling is required to determine the geometry of the mineralisation with respect to the drill hole angle. |
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| Criteria | JORC Code Explanation | Commentary |
|---|---|---|
| Diagrams | Appropriate maps and sections (with scales) and tabulations of intercepts should be included for any significant discovery being reported. These should include, but not be limited to a plan view of drill hole collar locations and appropriate sectional views. |
Refer to Figures included in the body of the announcement. |
| Balanced reporting | Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high grades and/or widths should be practiced to avoid misleading reporting of Exploration Results. |
Comprehensive reporting of REO assay results is provided in Appendix IV. Representative reporting of significant intersections is included in the body of the announcement. |
| Other substantive exploration data |
Other exploration data, if meaningful and material, should be reported including (but not limited to): geological observations; geophysical survey results; geochemical survey results; bulk samples – size and method of treatment; metallurgical test results; bulk density, groundwater, geotechnical and rock characteristics; potential deleterious or contaminating substances. |
None. |
| Further work | The nature and scale of planned further work (eg tests for lateral extensions or depth extensions or large-scale step-out drilling). Diagrams clearly highlighting the areas of possible extensions, including the main geological interpretations and future drilling areas, provided this information is not commercially sensitive. |
Further drilling may be undertaken for infill and extension of the known exploration prospects. Soil sampling is being undertaken to evaluate the extension of the mineralised structure to the southeast and further drilling may be undertaken to test exploration targets. |
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