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GREENWING RESOURCES LTD — Capital/Financing Update 2019
Sep 10, 2019
65029_rns_2019-09-10_235cec0f-6403-44b9-972b-e3306d0caefd.pdf
Capital/Financing Update
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ASX Announcement 11 September 2019
Continued exploration success at Graphmada with significant graphite drill intersections encountered.
Bass Metals Limited (ASX: “BSM”) (“Bass” or the “Company”) is pleased to provide a material update on its exploration activities, furthering a primary objective to increase its resource base at its 100% wholly owned Graphmada Mine Complex, located in Madagascar.
HIGHLIGHTS
-
The Company recently completed 34 diamond drill holes for a total 1,092m drilled, to an average depth of 33m without incident at the Mahefedok Large Flake Graphite Deposit. The principal aim of the program was to provide further data to support a reclassification of the existing Mineral Resource of 3.5mt @ 4.2% Total Graphitic Carbon (TGC) and potentially expand the resource.
-
Key results include:
13.8m @ 7.5% TGC 8.2m @ 7.2% TGC 9.8m @ 7.0% TGC 14.4m @ 6.7% TGC
25.9m @ 5.0% TGC 15.9m @ 4.9% TGC 20.9m @ 4.8% TGC 20.3m @ 4.7% TGC
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The deposit remains open in all directs and to depth, providing a solid basis to conduct a subsequent drill program aimed at expanding the resource at Mahefedok with extensions of mineralization discovered outside of the existing open pit footprint, which may lead to an expansion current open pit mining operations.
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The Company is proceeding with a revised Mineral Resource estimate for the Mahefedok Deposit, expected to be announced in October.
MAHEFEDOK DEPOSIT
The Company 100% owns and operates at the Mahefedok Deposit via exploitation permit number 26670. The permit grants the exclusive rights for 40 years to explore and mine graphitic resources.
The graphite mineralization at Mahefedok is hosted in gneissic units, striking north to south and dipping to the west at approx. 40°, with mineralization hosted in regolith (weathered material) and fresh bedrock.
The known strike lengths from historical exploration and 2,300 meters of diamond drilling completed in 2017 for the northern, central and southern zones are approximately 500m, 900m, and 400m respectively for a cumulative strike length of approximately 1,800m. Current mining operations at Mahefedok target the first of three zones of mineralization that constitute the existing Mineral Resource of 3.5mt at 4.2% TGC.
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Figure 1: Mahefedok Mineral Resource in proximity to processing infrastructure.
2019 DRILLING PROGRAM
Recent mining operations confirmed further mineralization not reported as part of the Mahefedok maiden Mineral Resource. To infill and gather additional data 1,092m of drilling was completed in and around the operating Mahefedok North Pit. The information collected is to be assimilated into the existing geological model for an update of the Mahefedok Mineral Resource of 3.5mt @ 4.2% TGC and is expected in October.
Below in blue is a representative long section of the Mineral Resource model used for the maiden Mineral Resource estimate and in red the additional tonnes identified from current mining operations.
==> picture [475 x 236] intentionally omitted <==
Figure 2: Mahefedok Mineral Resource vs tonnes mined from current operations.
During drilling additional mineralization was also intercepted outside of the Mineral Resource footprint and will be incorporated into the update of the Mahefedok Mineral Resource. Any possible extensions of mineralization may lead to an expansion of the Mahefedok North Pit.
The below cross-section of the style of mineralization at Mahefedok demonstrates the drill intercepts outside of current open pit operations. Of particular interest for the re-estimation of Mineral Resources is the potential influence of the thick, high grade intersections such as drill hole BSMD84 at less than 35m in depth, and in soft, low cost and easily mineable regolith.
==> picture [482 x 163] intentionally omitted <==
Figure 3: 2019 drilling (red) vs 2017 Mineral Resource drilling (blue).
The Company will follow up this mineralization with dense grade control augering to assimilate these new ore bodies into current mine designs, and with a reclassification of Mineral Resources in October, look to develop an Ore Reserve estimate in accordance with the JORC Code 2012 later in the year.
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Figure 4: Mahefedok drill collars with weighted average TGC intersections.
Table 1: Weighted average intersections of graphitic mineralization.
| Drill hole ID | From (m) | To (m) | Intersection (m) | WA.TGC (%) |
|---|---|---|---|---|
| BSMD091 | 7.6 | 33.5 | 25.9 | 5.0 |
| BSMD069 | 9.4 | 31.8 | 20.9 | 4.8 |
| BSMD075 | 1.8 | 22.6 | 20.8 | 3.9 |
| BSMD097 | 0.0 | 20.3 | 20.3 | 4.7 |
| BSMD083 | 30.0 | 47.3 | 17.4 | 6.7 |
| BSMD084 | 19.3 | 35.3 | 15.9 | 4.9 |
| BSMD066 | 5.9 | 22.0 | 15.6 | 4.2 |
| BSMD067 | 26.5 | 41.3 | 14.8 | 2.4 |
| BSMD095A | 11.7 | 26.2 | 14.5 | 5.9 |
| BSMD083 | 9.8 | 23.6 | 13.8 | 7.5 |
| BSMD095A | 31.6 | 44.0 | 12.4 | 5.1 |
| BSMD073 | 13.1 | 25.0 | 11.9 | 4.1 |
| BSMD090 | 7.4 | 17.4 | 10.0 | 4.6 |
| BSMD084 | 8.6 | 18.4 | 9.8 | 7.0 |
| BSMD089 | 7.3 | 17.1 | 9.8 | 4.6 |
| BSMD074 | 8.3 | 18.0 | 9.8 | 3.4 |
| BSMD079 | 1.7 | 11.0 | 9.3 | 3.2 |
| BSMD093 | 5.8 | 15.0 | 9.2 | 3.0 |
| BSMD080 | 7.6 | 16.7 | 9.1 | 5.6 |
| BSMD094 | 19.2 | 28.1 | 8.9 | 4.0 |
| BSMD081 | 12.3 | 20.6 | 8.2 | 7.2 |
| BSMD076 | 14.2 | 22.3 | 8.2 | 3.2 |
| BSMD070 | 9.8 | 18.0 | 8.2 | 5.8 |
| BSMD066 | 29.4 | 38.5 | 8.1 | 3.4 |
| BSMD078 | 2.6 | 10.6 | 8.0 | 2.9 |
| BSMD082 | 12.6 | 20.4 | 7.8 | 6.2 |
| BSMD065 | 13.2 | 20.9 | 7.7 | 3.2 |
| BSMD067 | 12.2 | 19.6 | 7.4 | 2.7 |
| BSMD065 | 30.4 | 37.4 | 6.8 | 3.4 |
| BSMD072 | 11.3 | 18.0 | 6.7 | 4.0 |
| BSMD073 | 0.0 | 6.5 | 6.5 | 3.2 |
| BSMD080 | 26.0 | 32.4 | 6.4 | 3.5 |
| BSMD079 | 28.6 | 34.3 | 5.7 | 3.6 |
| BSMD088 | 6.3 | 11.7 | 5.4 | 3.6 |
| Drill hole ID | From (m) | To (m) | Intersection (m) | WA.TGC (%) |
| BSMD096 | 19.0 | 24.3 | 5.3 | 2.8 |
| BSMD071 | 11.0 | 16.1 | 5.1 | 4.9 |
| BSMD078 | 21.6 | 26.3 | 4.7 | 3.9 |
| BSMD075 | 35.7 | 40.4 | 4.7 | 3.0 |
| BSMD092 | 4.3 | 9.0 | 4.7 | 6.0 |
| BSMD079 | 16.1 | 20.7 | 4.6 | 2.5 |
| BSMD087 | 24.8 | 29.3 | 4.6 | 3.6 |
| BSMD071 | 34.4 | 38.7 | 4.4 | 3.4 |
| BSMD094 | 8.8 | 12.9 | 4.1 | 3.3 |
| BSMD088 | 28.4 | 32.4 | 4.0 | 3.7 |
| BSMD088 | 20.9 | 24.9 | 4.0 | 2.4 |
| BSMD093 | 0.0 | 4.0 | 4.0 | 2.8 |
| BSMD087 | 13.3 | 17.3 | 3.9 | 2.3 |
| BSMD076 | 2.7 | 6.5 | 3.8 | 7.8 |
| BSMD087 | 1.9 | 5.6 | 3.7 | 2.9 |
| BSMD077 | 31.2 | 34.8 | 3.6 | 3.7 |
| BSMD092 | 19.4 | 22.8 | 3.4 | 2.0 |
| BSMD074 | 3.8 | 7.1 | 3.2 | 2.5 |
| BSMD072 | 6.5 | 9.7 | 3.2 | 3.4 |
| BSMD096 | 7.1 | 10.3 | 3.2 | 2.7 |
| BSMD088 | 16.5 | 19.4 | 2.9 | 3.3 |
| BSMD073 | 34.9 | 37.8 | 2.9 | 3.4 |
| BSMD077 | 21.8 | 24.5 | 2.7 | 3.6 |
| BSMD092 | 39.4 | 42.0 | 2.6 | 3.3 |
| BSMD068 | 18.7 | 21.3 | 2.6 | 4.7 |
| BSMD077 | 12.4 | 14.9 | 2.5 | 2.5 |
| BSMD070 | 5.0 | 7.4 | 2.4 | 4.4 |
| BSMD071 | 29.4 | 31.6 | 2.3 | 4.0 |
| BSMD068 | 5.3 | 7.4 | 2.2 | 2.2 |
| BSMD077 | 16.3 | 18.3 | 2.0 | 2.6 |
| BSMD090 | 25.5 | 27.4 | 1.9 | 4.7 |
| BSMD091 | 38.0 | 39.8 | 1.8 | 2.6 |
| BSMD065 | 6.9 | 8.6 | 1.8 | 6.4 |
| BSMD096 | 29.7 | 31.3 | 1.6 | 3.1 |
| BSMD097 | 32.0 | 33.5 | 1.6 | 2.4 |
| BSMD068 | 12.5 | 13.8 | 1.4 | 6.0 |
| BSMD093 | 32.2 | 33.5 | 1.3 | 2.9 |
MAHELA DEPOSIT UPDATE
With the completion of diamond drilling at Mahela, samples are now with the laboratory for analysis. The Company expects to receive the results within the next 4-6 weeks, to define a significant mineralization footprint and proceed with a maiden Mineral Resource estimate for the project. To date, results have been very encouraging, with substantial zones of graphite mineralization intersected with the resource open in all directions.
TIM MCMANUS CEO:
“The team at Bass continues to significantly progress both our exploration and operational results, towards development of large-scale mining and processing operations at the lowest capital intensity pathway for our shareholders.
To have again realized significant large flake graphite potential in direct proximity to our fully developed infrastructure is an excellent result, and we eagerly anticipate the findings from our more extensive drilling program at the Mahela Deposit.
Bass will continue to aggressively explore its Permits within the region, to continue to accelerate its growth in Mineral Resources to support large scale operations and downstream integration.”
For more information, please contact:
Tim McManus Peter Wright Chief Executive Officer Executive Director Phone: (07) 3203 5894 Phone: (07) 3203 5894 Email: [email protected] Email: [email protected] www.bassmetals.com.au @bassmetals
Disclaimer
This document has been prepared by Bass Metals Limited (the “Company”). It should not be considered as an invitation or offer to subscribe for or purchase any securities in the Company or as an inducement to make an invitation or offer with respect to those securities. No agreement to subscribe for securities in the Company will be entered into on the basis of this document.
This document is provided on the basis that neither the Company nor its officers, shareholders, related bodies corporate, partners, affiliates, employees, representatives and advisers make any representation or warranty (express or implied) as to the accuracy, reliability, relevance or completeness of the material contained in the document and nothing contained in the document is, or may be relied upon as a promise, representation or warranty, whether as to the past or the future. The Company hereby excludes all warranties that can be excluded by law.
Forward Looking Statements
This announcement contains certain ‘forward-looking statements’ within the meaning of the securities laws of applicable jurisdictions. Forward-looking statements can generally be identified by the use of forward-looking words such as ‘may,’ ‘should,’ ‘expect,’ ‘anticipate,’ ‘estimate,’ ‘scheduled’ or ‘continue’ or the negative version of them or comparable terminology.
Any forecasts or other forward-looking statements contained in this announcement are subject to known and unknown risks and uncertainties and may involve significant elements of subjective judgment and assumptions as to future events which may or may not be correct. There are usually differences between forecast and actual results because events and actual circumstances frequently do not occur as forecast and these differences may be material.
Bass Metals does not give any representation, assurance or guarantee that the occurrence of the events expressed or implied in any forward-looking statements in this announcement will actually occur and you are cautioned not to place undue reliance on forward-looking statements. The information in this document does not take into account the objectives, financial situation or particular needs of any person. Nothing contained in this document constitutes investment, legal, tax or other advice.
Important information
This announcement does not constitute an offer to sell, or a solicitation of an offer to buy, securities in the United States, or in any other jurisdiction in which such an offer would be illegal. The securities referred to in this document have not been and will not be registered under the United States Securities Act of 1933 (the ‘US Securities Act’), or under the securities laws of any state or other jurisdiction of the United States and may not be offered or sold, directly or indirectly, within the United States, unless the securities have been registered under the US Securities Act or an exemption from the registration requirements of the US Securities Act is available.
This document may not be distributed or released in the United States.
Competent Person Statement
The information in this document that relates to Exploration Results, Exploration Targets and Mineral Resources is based on information compiled by Tim McManus, a Competent Person who is a member of the Australasian Institute of Mining and Metallurgy and a full-time employee of the Company.
Tim McManus has sufficient experience that is relevant to the style of mineralization and type of deposit under consideration and to the activity being undertaken to qualify as a Competent Person as defined in the 2012 Edition of the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves.
Tim McManus consents to the inclusion of the information in this document in the form and context in which it appears.
APPENDIX OF RESULTS
Mahefedok Collar Coordinates
| Drill hole ID | Utm39sX | Utm39sY | Azimuth | Inclination | Total Depth |
|---|---|---|---|---|---|
| BSMD065 | 289,005 | 7,905,704 | 90 | -60 | 37.4 |
| BSMD066 | 288,977 | 7,905,701 | 90 | -60 | 41.3 |
| BSMD067 | 288,953 | 7,905,700 | 90 | -60 | 41.3 |
| BSMD068 | 288,929 | 7,905,704 | 90 | -60 | 28.3 |
| BSMD069 | 288,897 | 7,905,699 | 90 | -60 | 35.8 |
| BSMD070 | 288,899 | 7,905,648 | 90 | -60 | 24.4 |
| BSMD071 | 288,924 | 7,905,650 | 90 | -60 | 42.4 |
| BSMD072 | 288,951 | 7,905,650 | 90 | -60 | 20.3 |
| BSMD073 | 288,980 | 7,905,602 | 90 | -60 | 40.3 |
| BSMD074 | 288,957 | 7,905,603 | 90 | -60 | 20.3 |
| BSMD075 | 288,929 | 7,905,602 | 90 | -60 | 41.3 |
| BSMD076 | 289,054 | 7,905,548 | 90 | -60 | 29.3 |
| BSMD077 | 289,020 | 7,905,546 | 90 | -60 | 34.8 |
| BSMD078 | 288,987 | 7,905,503 | 90 | -60 | 26.3 |
| BSMD079 | 288,977 | 7,905,552 | 90 | -60 | 35.2 |
| BSMD080 | 288,946 | 7,905,548 | 90 | -60 | 32.4 |
| BSMD081 | 288,910 | 7,905,546 | 90 | -60 | 26.3 |
| BSMD082 | 288,903 | 7,905,600 | 90 | -60 | 24.4 |
| BSMD083 | 288,906 | 7,905,450 | 90 | -60 | 47.3 |
| BSMD084 | 288,901 | 7,905,501 | 90 | -60 | 35.3 |
| BSMD085 | 289,082 | 7,905,406 | 90 | -60 | 19.4 |
| BSMD086 | 289,081 | 7,905,456 | 90 | -60 | 24.4 |
| BSMD087 | 289,042 | 7,905,458 | 90 | -60 | 29.3 |
| BSMD088 | 288,986 | 7,905,458 | 90 | -60 | 32.4 |
| BSMD089 | 288,957 | 7,905,456 | 90 | -60 | 24.3 |
| BSMD090 | 288,952 | 7,905,502 | 90 | -60 | 27.4 |
| BSMD091 | 288,894 | 7,905,741 | 90 | -60 | 43.4 |
| BSMD092 | 288,920 | 7,905,832 | 90 | -60 | 47.4 |
| BSMD093 | 288,959 | 7,905,650 | 0 | -90 | 33.5 |
| BSMD094 | 288,936 | 7,905,705 | 0 | -90 | 37.5 |
| BSMD095 | 288,918 | 7,905,400 | 90 | -60 | 40.3 |
| BSMD095A | 288,917 | 7,905,404 | 90 | -60 | 44.0 |
| BSMD096 | 288,975 | 7,905,403 | 90 | -60 | 31.3 |
| BSMD097 | 288,964 | 7,905,604 | 0 | -90 | 33.5 |
Mahefedok Assay Results
| Drill hole ID | From(m) | To(m) | Interval(m) | TGC(%) | Lithology |
|---|---|---|---|---|---|
| BSMD065 | 3.9 | 4.5 | 0.6 | 0.2 | Saprolith |
| BSMD065 | 4.5 | 5.5 | 1.0 | 0.7 | Saprolith |
| BSMD065 | 5.5 | 6.6 | 1.1 | 0.5 | Saprolith |
| BSMD065 | 6.6 | 6.9 | 0.3 | 1.1 | Saprolith |
| BSMD065 | 6.9 | 7.8 | 0.9 | 4.7 | Saprolith |
| BSMD065 | 7.8 | 8.6 | 0.9 | 8.2 | Saprolith |
| BSMD065 | 8.6 | 9.6 | 1.0 | 0.7 | Saprolith |
| BSMD065 | 9.6 | 10.6 | 1.0 | 0.6 | Saprolith |
| BSMD065 | 10.6 | 11.5 | 0.9 | 1.5 | Saprolith |
| BSMD065 | 11.5 | 12.3 | 0.8 | 0.9 | Saprolith |
| BSMD065 | 12.3 | 13.2 | 0.9 | 0.6 | Saprolith |
| BSMD065 | 13.2 | 14.0 | 0.8 | 1.9 | Saprolith |
| BSMD065 | 14.0 | 15.1 | 1.0 | 8.1 | Saprolith |
| BSMD065 | 15.1 | 16.2 | 1.1 | 3.0 | Saprolith |
| BSMD065 | 16.2 | 17.4 | 1.2 | 1.3 | Saprolith |
| BSMD065 | 17.4 | 18.5 | 1.2 | 1.2 | Saprolith |
| BSMD065 | 18.5 | 19.9 | 1.4 | 4.6 | Saprolith |
| BSMD065 | 19.9 | 20.9 | 1.0 | 2.5 | Saprolith |
| BSMD065 | 20.9 | 22.1 | 1.2 | 0.9 | Saprolith |
| BSMD065 | 22.1 | 23.0 | 0.9 | 1.1 | Saprolith |
| BSMD065 | 23.0 | 24.4 | 1.3 | 2.1 | Saprolith |
| BSMD065 | 24.4 | 25.4 | 1.1 | 0.5 | Saprolith |
| BSMD065 | 25.4 | 26.3 | 0.9 | 0.8 | Saprolith |
| BSMD065 | 26.3 | 27.4 | 1.1 | 0.4 | Saprolith |
| BSMD065 | 27.4 | 28.3 | 0.9 | 0.5 | Saprolith |
| BSMD065 | 28.3 | 29.4 | 1.1 | 1.1 | Saprolith |
| BSMD065 | 29.4 | 30.6 | 1.2 | 1.5 | Saprolith |
| BSMD065 | 30.6 | 32.0 | 1.4 | 2.4 | Saprolith |
| BSMD065 | 32.0 | 32.7 | 0.8 | 6.0 | Saprolith |
| BSMD065 | 32.7 | 33.4 | 0.6 | 5.0 | Saprolith |
| BSMD065 | 33.4 | 33.9 | 0.5 | 3.3 | Saprolith |
| BSMD065 | 33.9 | 34.9 | 1.0 | 1.5 | Saprolith |
| BSMD065 | 34.9 | 35.7 | 0.8 | 3.3 | Graphitic Gneiss |
| BSMD065 | 35.7 | 36.6 | 0.8 | 2.8 | Graphitic Gneiss |
| BSMD065 | 36.6 | 37.4 | 0.8 | 4.2 | Graphitic Gneiss |
| BSMD066 | 4.0 | 4.8 | 0.8 | 0.2 | Saprolith |
| BSMD066 | 4.8 | 5.1 | 0.3 | 0.4 | Saprolith |
| BSMD066 | 5.1 | 5.9 | 0.8 | 1.4 | Saprolith |
| BSMD066 | 5.9 | 6.7 | 0.8 | 4.7 | Saprolith |
| BSMD066 | 6.7 | 7.5 | 0.9 | 1.7 | Saprolith |
| BSMD066 | 7.5 | 8.1 | 0.6 | 3.7 | Saprolith |
| BSMD066 | 8.1 | 9.4 | 1.3 | 6.7 | Saprolith |
| BSMD066 | 9.4 | 10.6 | 1.1 | 9.6 | Saprolith |
| BSMD066 | 10.6 | 11.6 | 1.1 | 6.5 | Saprolith |
| BSMD066 | 11.6 | 12.3 | 0.7 | 4.8 | Saprolith |
| Drill hole ID | From(m) | To(m) | Interval(m) | TGC(%) | Lithology |
| BSMD066 | 12.3 | 13.4 | 1.1 | 5.0 | Saprolith |
| BSMD066 | 13.4 | 14.3 | 0.9 | 4.0 | Saprolith |
| BSMD066 | 14.3 | 15.8 | 1.6 | 3.6 | Saprolith |
| BSMD066 | 16.3 | 17.4 | 1.1 | 2.5 | Saprolith |
| BSMD066 | 17.4 | 17.8 | 0.3 | 0.5 | Saprolith |
| BSMD066 | 17.8 | 19.4 | 1.6 | 1.3 | Saprolith |
| BSMD066 | 19.4 | 21.4 | 2.0 | 2.0 | Saprolith |
| BSMD066 | 21.4 | 22.0 | 0.6 | 7.2 | Saprolith |
| BSMD066 | 22.0 | 23.0 | 1.0 | 1.3 | Saprolith |
| BSMD066 | 23.0 | 24.6 | 1.6 | 1.1 | Saprolith |
| BSMD066 | 24.6 | 25.3 | 0.8 | 2.5 | Saprolith |
| BSMD066 | 25.3 | 26.5 | 1.1 | 0.9 | Saprolith |
| BSMD066 | 26.5 | 27.5 | 1.1 | 1.4 | Saprolith |
| BSMD066 | 27.5 | 28.4 | 0.9 | 1.8 | Saprolith |
| BSMD066 | 28.4 | 29.4 | 1.0 | 2.0 | Saprolith |
| BSMD066 | 29.4 | 29.9 | 0.5 | 6.8 | Saprolith |
| BSMD066 | 29.9 | 30.8 | 0.9 | 2.5 | Saprolith |
| BSMD066 | 31.3 | 32.1 | 0.8 | 2.1 | Saprolith |
| BSMD066 | 32.1 | 32.8 | 0.7 | 1.6 | Saprolith |
| BSMD066 | 33.3 | 34.4 | 1.1 | 3.0 | Saprolith |
| BSMD066 | 34.4 | 35.8 | 1.4 | 4.9 | Graphitic Gneiss |
| BSMD066 | 35.8 | 36.6 | 0.8 | 4.4 | Graphitic Gneiss |
| BSMD066 | 36.6 | 37.5 | 0.9 | 1.8 | Graphitic Gneiss |
| BSMD066 | 37.5 | 38.5 | 1.0 | 4.2 | Graphitic Gneiss |
| BSMD066 | 38.5 | 39.4 | 0.9 | 1.0 | Graphitic Gneiss |
| BSMD066 | 39.4 | 40.3 | 0.9 | 1.7 | Graphitic Gneiss |
| BSMD066 | 40.3 | 41.3 | 1.0 | 2.0 | Graphitic Gneiss |
| BSMD067 | 6.3 | 6.8 | 0.5 | 0.1 | Saprolith |
| BSMD067 | 6.8 | 7.5 | 0.7 | 0.0 | Saprolith |
| BSMD067 | 7.5 | 8.3 | 0.8 | 2.4 | Saprolith |
| BSMD067 | 8.3 | 9.5 | 1.1 | 3.0 | Saprolith |
| BSMD067 | 9.5 | 10.4 | 1.0 | 1.6 | Saprolith |
| BSMD067 | 10.4 | 11.4 | 0.9 | 1.5 | Saprolith |
| BSMD067 | 11.4 | 12.2 | 0.8 | 1.5 | Saprolith |
| BSMD067 | 12.2 | 12.9 | 0.7 | 5.3 | Saprolith |
| BSMD067 | 12.9 | 13.3 | 0.4 | 7.1 | Saprolith |
| BSMD067 | 13.3 | 14.3 | 0.9 | 2.9 | Saprolith |
| BSMD067 | 14.3 | 15.1 | 0.9 | 2.2 | Saprolith |
| BSMD067 | 15.1 | 16.4 | 1.2 | 1.4 | Saprolith |
| BSMD067 | 16.4 | 17.4 | 1.0 | 2.2 | Saprolith |
| BSMD067 | 17.4 | 18.7 | 1.3 | 2.0 | Saprolith |
| BSMD067 | 18.7 | 19.6 | 0.9 | 2.5 | Saprolith |
| BSMD067 | 19.6 | 20.5 | 0.9 | 0.0 | Saprolith |
| BSMD067 | 20.5 | 21.6 | 1.1 | 0.0 | Saprolith |
| BSMD067 | 21.6 | 22.7 | 1.1 | 0.1 | Saprolith |
| BSMD067 | 22.7 | 23.8 | 1.2 | 1.0 | Saprolith |
| BSMD067 | 23.8 | 24.3 | 0.5 | 2.8 | Saprolith |
| BSMD067 | 24.3 | 25.4 | 1.0 | 1.1 | Saprolith |
| BSMD067 | 25.4 | 25.8 | 0.5 | 0.7 | Saprolith |
| Drill hole ID | From(m) | To(m) | Interval(m) | TGC(%) | Lithology |
| BSMD067 | 25.8 | 26.5 | 0.7 | 1.0 | Saprolith |
| BSMD067 | 26.5 | 27.3 | 0.9 | 3.4 | Saprolith |
| BSMD067 | 27.3 | 28.3 | 1.0 | 3.0 | Saprolith |
| BSMD067 | 28.3 | 29.2 | 0.9 | 4.9 | Saprolith |
| BSMD067 | 29.2 | 30.4 | 1.2 | 1.0 | Saprolith |
| BSMD067 | 30.4 | 31.4 | 1.1 | 1.8 | Saprolith |
| BSMD067 | 31.4 | 32.3 | 0.9 | 1.3 | Saprolith |
| BSMD067 | 32.3 | 33.3 | 1.0 | 2.0 | Saprolith |
| BSMD067 | 33.3 | 34.4 | 1.1 | 1.2 | Saprolith |
| BSMD067 | 34.4 | 35.3 | 0.9 | 2.5 | Saprolith |
| BSMD067 | 35.3 | 36.5 | 1.2 | 1.3 | Saprolith |
| BSMD067 | 36.5 | 37.4 | 0.9 | 3.4 | Saprolith |
| BSMD067 | 37.4 | 38.3 | 0.9 | 3.5 | Saprolith |
| BSMD067 | 38.3 | 39.3 | 1.0 | 2.9 | Saprolith |
| BSMD067 | 39.3 | 40.2 | 0.9 | 2.6 | Saprolith |
| BSMD067 | 40.2 | 41.3 | 1.1 | 2.3 | Saprolith |
| BSMD068 | 4.3 | 5.3 | 1.0 | 0.3 | Saprolith |
| BSMD068 | 5.3 | 6.2 | 0.9 | 0.4 | Saprolith |
| BSMD068 | 6.2 | 7.4 | 1.3 | 0.9 | Saprolith |
| BSMD068 | 7.4 | 8.3 | 0.9 | 0.2 | Saprolith |
| BSMD068 | 8.3 | 9.3 | 1.0 | 1.5 | Saprolith |
| BSMD068 | 9.3 | 10.0 | 0.7 | 1.0 | Saprolith |
| BSMD068 | 10.0 | 10.5 | 0.5 | 2.6 | Saprolith |
| BSMD068 | 10.5 | 11.0 | 0.5 | 0.2 | Saprolith |
| BSMD068 | 11.0 | 11.8 | 0.8 | 0.6 | Saprolith |
| BSMD068 | 11.8 | 12.5 | 0.7 | 1.1 | Saprolith |
| BSMD068 | 12.5 | 13.1 | 0.6 | 2.9 | Saprolith |
| BSMD068 | 13.1 | 13.8 | 0.8 | 8.6 | Saprolith |
| BSMD068 | 13.8 | 14.5 | 0.7 | 1.6 | Saprolith |
| BSMD068 | 14.5 | 15.3 | 0.8 | 0.5 | Saprolith |
| BSMD068 | 15.3 | 16.1 | 0.8 | 1.1 | Saprolith |
| BSMD068 | 16.1 | 16.7 | 0.6 | 1.8 | Saprolith |
| BSMD068 | 16.7 | 17.7 | 1.0 | 2.6 | Saprolith |
| BSMD068 | 17.7 | 18.7 | 1.1 | 1.1 | Saprolith |
| BSMD068 | 18.7 | 19.9 | 1.1 | 3.0 | Saprolith |
| BSMD068 | 19.9 | 20.4 | 0.6 | 6.9 | Saprolith |
| BSMD068 | 20.4 | 21.3 | 0.8 | 8.2 | Saprolith |
| BSMD068 | 21.3 | 22.4 | 1.1 | 2.2 | Saprolith |
| BSMD068 | 22.4 | 23.4 | 1.1 | 1.1 | Saprolith |
| BSMD068 | 23.4 | 24.4 | 1.0 | 2.1 | Saprolith |
| BSMD068 | 24.4 | 25.5 | 1.1 | 0.0 | Dolerite |
| BSMD069 | 6.7 | 7.4 | 0.8 | 0.7 | Saprolith |
| BSMD069 | 7.4 | 8.4 | 1.0 | 1.7 | Saprolith |
| BSMD069 | 8.4 | 9.4 | 0.9 | 2.2 | Saprolith |
| BSMD069 | 9.4 | 11.3 | 2.0 | 4.3 | Saprolith |
| BSMD069 | 12.8 | 13.7 | 0.9 | 4.2 | Saprolith |
| BSMD069 | 13.7 | 14.5 | 0.7 | 3.8 | Saprolith |
| BSMD069 | 14.5 | 15.7 | 1.2 | 4.1 | Saprolith |
| BSMD069 | 15.7 | 16.6 | 0.9 | 3.8 | Saprolith |
| Drill hole ID | From(m) | To(m) | Interval(m) | TGC(%) | Lithology |
| BSMD069 | 16.6 | 17.4 | 0.9 | 4.3 | Saprolith |
| BSMD069 | 17.4 | 18.4 | 1.0 | 3.2 | Saprolith |
| BSMD069 | 18.4 | 19.4 | 1.0 | 4.4 | Saprolith |
| BSMD069 | 19.4 | 20.3 | 0.9 | 4.3 | Saprolith |
| BSMD069 | 20.3 | 21.8 | 1.5 | 2.8 | Saprolith |
| BSMD069 | 21.8 | 22.8 | 1.0 | 6.9 | Saprolith |
| BSMD069 | 22.8 | 23.8 | 1.1 | 5.3 | Saprolith |
| BSMD069 | 23.8 | 25.0 | 1.2 | 5.3 | Saprolith |
| BSMD069 | 25.0 | 26.0 | 1.0 | 4.1 | Saprolith |
| BSMD069 | 26.0 | 26.8 | 0.9 | 5.5 | Saprolith |
| BSMD069 | 26.8 | 27.5 | 0.6 | 6.4 | Saprolith |
| BSMD069 | 27.5 | 28.1 | 0.6 | 7.0 | Saprolith |
| BSMD069 | 28.1 | 28.5 | 0.4 | 6.8 | Saprolith |
| BSMD069 | 28.5 | 29.3 | 0.8 | 7.5 | Saprolith |
| BSMD069 | 29.3 | 30.4 | 1.1 | 8.0 | Saprolith |
| BSMD069 | 30.4 | 31.1 | 0.7 | 3.1 | Saprolith |
| BSMD069 | 31.1 | 31.8 | 0.7 | 3.0 | Saprolith |
| BSMD069 | 31.8 | 32.6 | 0.9 | 1.8 | Graphitic Gneiss |
| BSMD069 | 32.6 | 33.5 | 0.9 | 1.9 | Graphitic Gneiss |
| BSMD069 | 33.5 | 34.3 | 0.8 | 2.1 | Graphitic Gneiss |
| BSMD069 | 34.3 | 35.1 | 0.8 | 0.0 | Graphitic Gneiss |
| BSMD069 | 35.1 | 35.8 | 0.7 | 2.1 | Gneiss |
| BSMD070 | 4.4 | 5.0 | 0.7 | 0.0 | Saprolith |
| BSMD070 | 5.0 | 6.6 | 1.6 | 4.1 | Saprolith |
| BSMD070 | 6.6 | 7.4 | 0.9 | 4.8 | Saprolith |
| BSMD070 | 7.4 | 8.2 | 0.7 | 0.1 | Saprolith |
| BSMD070 | 8.2 | 8.6 | 0.4 | 1.1 | Saprolith |
| BSMD070 | 8.6 | 9.3 | 0.7 | 0.2 | Saprolith |
| BSMD070 | 9.3 | 9.8 | 0.5 | 2.2 | Saprolith |
| BSMD070 | 9.8 | 10.9 | 1.0 | 7.1 | Saprolith |
| BSMD070 | 10.9 | 12.4 | 1.5 | 8.9 | Saprolith |
| BSMD070 | 12.4 | 12.9 | 0.5 | 7.8 | Saprolith |
| BSMD070 | 12.9 | 13.6 | 0.7 | 12.0 | Saprolith |
| BSMD070 | 13.6 | 14.6 | 1.1 | 4.5 | Saprolith |
| BSMD070 | 14.6 | 16.0 | 1.4 | 3.1 | Saprolith |
| BSMD070 | 16.0 | 17.2 | 1.2 | 3.1 | Saprolith |
| BSMD070 | 17.2 | 18.0 | 0.9 | 2.6 | Graphitic Gneiss |
| BSMD070 | 18.0 | 18.9 | 0.9 | 2.1 | Graphitic Gneiss |
| BSMD070 | 18.9 | 19.8 | 0.9 | 2.1 | Graphitic Gneiss |
| BSMD070 | 19.8 | 20.7 | 0.9 | 1.8 | Graphitic Gneiss |
| BSMD070 | 20.7 | 21.6 | 0.9 | 2.5 | Graphitic Gneiss |
| BSMD070 | 21.6 | 22.5 | 0.9 | 1.8 | Graphitic Gneiss |
| BSMD070 | 22.5 | 23.4 | 0.9 | 2.5 | Graphitic Gneiss |
| BSMD070 | 23.4 | 24.4 | 1.0 | 1.8 | Graphitic Gneiss |
| BSMD071 | 5.4 | 5.9 | 0.5 | 0.3 | Saprolith |
| BSMD071 | 5.9 | 6.9 | 1.0 | 2.9 | Saprolith |
| BSMD071 | 6.9 | 7.8 | 1.0 | 3.0 | Saprolith |
| BSMD071 | 7.8 | 8.9 | 1.1 | 2.3 | Saprolith |
| BSMD071 | 8.9 | 10.2 | 1.3 | 2.9 | Saprolith |
| Drill hole ID | From(m) | To(m) | Interval(m) | TGC(%) | Lithology |
| BSMD071 | 10.2 | 11.0 | 0.8 | 2.5 | Saprolith |
| BSMD071 | 11.0 | 11.9 | 0.8 | 4.7 | Saprolith |
| BSMD071 | 11.9 | 12.6 | 0.7 | 7.3 | Saprolith |
| BSMD071 | 12.6 | 13.9 | 1.3 | 3.2 | Saprolith |
| BSMD071 | 13.9 | 15.4 | 1.5 | 5.6 | Saprolith |
| BSMD071 | 15.4 | 16.1 | 0.8 | 4.7 | Saprolith |
| BSMD071 | 16.1 | 16.9 | 0.8 | 2.9 | Saprolith |
| BSMD071 | 16.9 | 17.7 | 0.9 | 2.6 | Saprolith |
| BSMD071 | 17.7 | 18.9 | 1.1 | 1.1 | Saprolith |
| BSMD071 | 18.9 | 19.9 | 1.1 | 1.0 | Saprolith |
| BSMD071 | 19.9 | 21.1 | 1.2 | 2.0 | Saprolith |
| BSMD071 | 21.1 | 22.0 | 1.0 | 0.9 | Saprolith |
| BSMD071 | 22.0 | 22.8 | 0.8 | 0.2 | Saprolith |
| BSMD071 | 22.8 | 23.4 | 0.5 | 0.6 | Saprolith |
| BSMD071 | 23.4 | 24.0 | 0.6 | 1.3 | Saprolith |
| BSMD071 | 24.0 | 24.9 | 1.0 | 0.5 | Saprolith |
| BSMD071 | 24.9 | 25.9 | 1.0 | 2.0 | Saprolith |
| BSMD071 | 25.9 | 26.9 | 1.0 | 1.0 | Saprolith |
| BSMD071 | 26.9 | 28.4 | 1.4 | 1.4 | Saprolith |
| BSMD071 | 28.4 | 29.4 | 1.0 | 1.6 | Saprolith |
| BSMD071 | 29.4 | 29.9 | 0.6 | 4.1 | Saprolith |
| BSMD071 | 29.9 | 30.6 | 0.7 | 4.6 | Saprolith |
| BSMD071 | 30.6 | 31.6 | 1.0 | 3.6 | Saprolith |
| BSMD071 | 31.6 | 32.7 | 1.0 | 0.7 | Saprolith |
| BSMD071 | 32.7 | 33.4 | 0.8 | 1.8 | Saprolith |
| BSMD071 | 33.4 | 34.4 | 1.0 | 0.8 | Saprolith |
| BSMD071 | 34.4 | 35.2 | 0.9 | 2.3 | Saprolith |
| BSMD071 | 35.2 | 35.9 | 0.6 | 2.4 | Saprolith |
| BSMD071 | 35.9 | 36.5 | 0.6 | 2.2 | Saprolith |
| BSMD071 | 36.5 | 37.2 | 0.7 | 4.9 | Saprolith |
| BSMD071 | 37.2 | 37.9 | 0.7 | 4.7 | Saprolith |
| BSMD071 | 37.9 | 38.7 | 0.8 | 3.9 | Saprolith |
| BSMD071 | 38.7 | 39.5 | 0.8 | 0.7 | Saprolith |
| BSMD071 | 39.5 | 40.2 | 0.7 | 0.3 | Saprolith |
| BSMD071 | 40.2 | 40.9 | 0.7 | 1.0 | Graphitic Gneiss |
| BSMD071 | 40.9 | 41.6 | 0.7 | 1.3 | Graphitic Gneiss |
| BSMD071 | 41.6 | 42.4 | 0.8 | 1.0 | Graphitic Gneiss |
| BSMD072 | 0.0 | 1.0 | 1.0 | 6.7 | Saprolith |
| BSMD072 | 1.0 | 2.0 | 1.1 | 0.7 | Saprolith |
| BSMD072 | 2.0 | 2.6 | 0.6 | 0.8 | Saprolith |
| BSMD072 | 2.6 | 3.3 | 0.7 | 2.0 | Saprolith |
| BSMD072 | 3.3 | 3.8 | 0.5 | 1.7 | Saprolith |
| BSMD072 | 3.8 | 4.5 | 0.7 | 0.8 | Saprolith |
| BSMD072 | 4.5 | 5.2 | 0.7 | 1.9 | Saprolith |
| BSMD072 | 5.2 | 5.8 | 0.7 | 1.4 | Saprolith |
| BSMD072 | 5.8 | 6.5 | 0.6 | 1.5 | Saprolith |
| BSMD072 | 6.5 | 7.2 | 0.7 | 3.0 | Saprolith |
| BSMD072 | 7.2 | 7.8 | 0.6 | 8.5 | Saprolith |
| BSMD072 | 7.8 | 8.9 | 1.1 | 1.7 | Saprolith |
| Drill hole ID | From(m) | To(m) | Interval(m) | TGC(%) | Lithology |
| BSMD072 | 8.9 | 9.7 | 0.8 | 2.3 | Saprolith |
| BSMD072 | 9.7 | 10.3 | 0.6 | 2.0 | Saprolith |
| BSMD072 | 10.3 | 10.8 | 0.5 | 1.2 | Saprolith |
| BSMD072 | 10.8 | 11.3 | 0.5 | 1.1 | Saprolith |
| BSMD072 | 11.3 | 12.0 | 0.7 | 7.0 | Saprolith |
| BSMD072 | 12.0 | 12.7 | 0.8 | 6.0 | Saprolith |
| BSMD072 | 12.7 | 13.3 | 0.5 | 2.7 | Saprolith |
| BSMD072 | 13.3 | 13.6 | 0.3 | 3.6 | Saprolith |
| BSMD072 | 13.6 | 14.5 | 1.0 | 5.1 | Saprolith |
| BSMD072 | 14.5 | 15.5 | 0.9 | 3.6 | Saprolith |
| BSMD072 | 15.5 | 16.4 | 0.9 | 3.1 | Saprolith |
| BSMD072 | 16.4 | 17.2 | 0.8 | 2.7 | Graphitic Gneiss |
| BSMD072 | 17.2 | 18.0 | 0.8 | 2.6 | Graphitic Gneiss |
| BSMD072 | 18.0 | 19.0 | 1.0 | 0.0 | Dolerite |
| BSMD073 | 0.0 | 1.0 | 1.0 | 5.1 | Saprolith |
| BSMD073 | 1.0 | 2.0 | 1.0 | 3.0 | Saprolith |
| BSMD073 | 2.0 | 3.0 | 1.0 | 2.9 | Saprolith |
| BSMD073 | 3.0 | 4.1 | 1.1 | 3.4 | Saprolith |
| BSMD073 | 4.1 | 4.7 | 0.6 | 3.6 | Saprolith |
| BSMD073 | 4.7 | 5.6 | 0.9 | 1.8 | Saprolith |
| BSMD073 | 5.6 | 6.5 | 0.9 | 2.7 | Saprolith |
| BSMD073 | 6.5 | 7.3 | 0.9 | 0.4 | Saprolith |
| BSMD073 | 7.3 | 8.2 | 0.8 | 1.1 | Saprolith |
| BSMD073 | 8.2 | 9.0 | 0.9 | 1.2 | Saprolith |
| BSMD073 | 9.0 | 10.1 | 1.0 | 1.6 | Saprolith |
| BSMD073 | 10.1 | 10.4 | 0.4 | 1.0 | Saprolith |
| BSMD073 | 10.4 | 10.9 | 0.5 | 1.0 | Saprolith |
| BSMD073 | 10.9 | 11.4 | 0.5 | 0.9 | Saprolith |
| BSMD073 | 11.4 | 12.2 | 0.8 | 1.2 | Saprolith |
| BSMD073 | 12.2 | 12.6 | 0.4 | 1.7 | Saprolith |
| BSMD073 | 12.6 | 13.1 | 0.5 | 1.5 | Saprolith |
| BSMD073 | 13.1 | 13.8 | 0.7 | 2.2 | Saprolith |
| BSMD073 | 13.8 | 14.8 | 1.1 | 3.6 | Saprolith |
| BSMD073 | 14.8 | 15.8 | 1.0 | 3.0 | Saprolith |
| BSMD073 | 15.8 | 16.5 | 0.7 | 3.8 | Saprolith |
| BSMD073 | 16.5 | 17.1 | 0.6 | 5.2 | Saprolith |
| BSMD073 | 17.1 | 17.5 | 0.4 | 4.0 | Saprolith |
| BSMD073 | 17.5 | 18.3 | 0.9 | 3.0 | Saprolith |
| BSMD073 | 18.3 | 19.4 | 1.1 | 3.5 | Saprolith |
| BSMD073 | 19.4 | 20.1 | 0.7 | 2.6 | Saprolith |
| BSMD073 | 20.1 | 20.7 | 0.6 | 1.9 | Saprolith |
| BSMD073 | 20.7 | 21.1 | 0.4 | 3.0 | Saprolith |
| BSMD073 | 21.1 | 21.9 | 0.8 | 7.4 | Saprolith |
| BSMD073 | 21.9 | 22.7 | 0.8 | 6.1 | Saprolith |
| BSMD073 | 22.7 | 23.4 | 0.7 | 6.5 | Saprolith |
| BSMD073 | 23.4 | 24.2 | 0.8 | 6.3 | Saprolith |
| BSMD073 | 24.2 | 25.0 | 0.8 | 3.6 | Saprolith |
| BSMD073 | 25.0 | 25.7 | 0.7 | 1.1 | Saprolith |
| BSMD073 | 25.7 | 26.2 | 0.5 | 1.0 | Saprolith |
| Drill hole ID | From(m) | To(m) | Interval(m) | TGC(%) | Lithology |
| BSMD073 | 26.2 | 27.3 | 1.1 | 0.9 | Saprolith |
| BSMD073 | 27.3 | 28.2 | 0.9 | 0.7 | Saprolith |
| BSMD073 | 28.2 | 29.1 | 0.9 | 1.7 | Saprolith |
| BSMD073 | 29.1 | 30.3 | 1.3 | 4.9 | Saprolith |
| BSMD073 | 30.3 | 31.8 | 1.4 | 0.9 | Saprolith |
| BSMD073 | 31.8 | 32.8 | 1.0 | 1.1 | Saprolith |
| BSMD073 | 32.8 | 34.1 | 1.3 | 1.5 | Saprolith |
| BSMD073 | 34.1 | 34.9 | 0.9 | 1.9 | Saprolith |
| BSMD073 | 34.9 | 35.8 | 0.8 | 2.8 | Saprolith |
| BSMD073 | 35.8 | 36.6 | 0.8 | 4.9 | Graphitic Gneiss |
| BSMD073 | 36.6 | 37.8 | 1.2 | 2.8 | Graphitic Gneiss |
| BSMD073 | 37.8 | 38.6 | 0.8 | 1.5 | Graphitic Gneiss |
| BSMD073 | 38.6 | 39.5 | 0.9 | 2.2 | Graphitic Gneiss |
| BSMD073 | 39.5 | 40.3 | 0.8 | 0.9 | Graphitic Gneiss |
| BSMD074 | 0.0 | 0.6 | 0.6 | 1.3 | Saprolith |
| BSMD074 | 0.6 | 1.2 | 0.6 | 1.2 | Saprolith |
| BSMD074 | 1.2 | 2.1 | 0.9 | 0.8 | Saprolith |
| BSMD074 | 2.1 | 2.6 | 0.5 | 0.7 | Saprolith |
| BSMD074 | 2.6 | 3.2 | 0.6 | 0.6 | Saprolith |
| BSMD074 | 3.2 | 3.8 | 0.6 | 1.6 | Saprolith |
| BSMD074 | 3.8 | 4.3 | 0.4 | 5.0 | Saprolith |
| BSMD074 | 4.3 | 4.9 | 0.6 | 1.2 | Saprolith |
| BSMD074 | 4.9 | 5.3 | 0.4 | 1.1 | Saprolith |
| BSMD074 | 5.3 | 6.3 | 1.0 | 2.7 | Saprolith |
| BSMD074 | 6.3 | 6.8 | 0.5 | 2.0 | Saprolith |
| BSMD074 | 6.8 | 7.1 | 0.3 | 3.9 | Saprolith |
| BSMD074 | 7.1 | 7.4 | 0.3 | 1.3 | Saprolith |
| BSMD074 | 7.4 | 8.3 | 0.9 | 2.7 | Saprolith |
| BSMD074 | 8.3 | 9.3 | 1.0 | 6.3 | Saprolith |
| BSMD074 | 9.3 | 10.3 | 1.0 | 3.7 | Saprolith |
| BSMD074 | 10.3 | 11.3 | 1.0 | 3.1 | Saprolith |
| BSMD074 | 11.3 | 12.0 | 0.8 | 1.6 | Saprolith |
| BSMD074 | 12.0 | 12.8 | 0.8 | 2.5 | Saprolith |
| BSMD074 | 12.8 | 13.4 | 0.6 | 4.1 | Saprolith |
| BSMD074 | 13.4 | 13.7 | 0.3 | 8.1 | Saprolith |
| BSMD074 | 13.7 | 14.3 | 0.7 | 3.1 | Saprolith |
| BSMD074 | 14.3 | 15.1 | 0.7 | 2.9 | Saprolith |
| BSMD074 | 15.1 | 15.9 | 0.9 | 2.8 | Saprolith |
| BSMD074 | 15.9 | 16.8 | 0.8 | 2.6 | Saprolith |
| BSMD074 | 16.8 | 17.4 | 0.6 | 3.6 | Graphitic Gneiss |
| BSMD074 | 17.4 | 18.0 | 0.7 | 2.6 | Graphitic Gneiss |
| BSMD074 | 18.0 | 19.0 | 1.0 | 0.0 | Dolerite |
| BSMD075 | 0.0 | 1.0 | 1.0 | 0.4 | Saprolith |
| BSMD075 | 1.0 | 1.8 | 0.8 | 1.5 | Saprolith |
| BSMD075 | 1.8 | 2.3 | 0.5 | 8.3 | Saprolith |
| BSMD075 | 2.3 | 3.2 | 0.9 | 2.7 | Saprolith |
| BSMD075 | 3.2 | 4.1 | 0.9 | 1.7 | Saprolith |
| BSMD075 | 4.1 | 5.1 | 1.0 | 3.2 | Saprolith |
| BSMD075 | 5.1 | 5.9 | 0.8 | 2.2 | Saprolith |
| Drill hole ID | From(m) | To(m) | Interval(m) | TGC(%) | Lithology |
| BSMD075 | 5.9 | 6.7 | 0.8 | 2.7 | Saprolith |
| BSMD075 | 6.7 | 7.5 | 0.8 | 1.8 | Saprolith |
| BSMD075 | 7.5 | 8.3 | 0.7 | 2.7 | Saprolith |
| BSMD075 | 8.3 | 9.5 | 1.2 | 4.7 | Saprolith |
| BSMD075 | 9.5 | 9.9 | 0.4 | 2.1 | Saprolith |
| BSMD075 | 9.9 | 10.9 | 1.0 | 3.2 | Saprolith |
| BSMD075 | 10.9 | 11.5 | 0.5 | 2.3 | Saprolith |
| BSMD075 | 11.5 | 12.0 | 0.6 | 1.7 | Saprolith |
| BSMD075 | 12.0 | 12.3 | 0.3 | 3.7 | Saprolith |
| BSMD075 | 12.3 | 13.4 | 1.1 | 2.9 | Saprolith |
| BSMD075 | 13.4 | 14.3 | 0.9 | 3.0 | Saprolith |
| BSMD075 | 14.3 | 15.3 | 1.0 | 3.5 | Saprolith |
| BSMD075 | 15.3 | 15.9 | 0.6 | 4.9 | Saprolith |
| BSMD075 | 15.9 | 16.8 | 0.9 | 5.6 | Saprolith |
| BSMD075 | 16.8 | 17.3 | 0.5 | 8.6 | Saprolith |
| BSMD075 | 17.3 | 17.8 | 0.6 | 7.1 | Saprolith |
| BSMD075 | 17.8 | 18.5 | 0.7 | 4.9 | Saprolith |
| BSMD075 | 18.5 | 19.3 | 0.8 | 5.2 | Saprolith |
| BSMD075 | 19.3 | 20.2 | 0.9 | 7.6 | Saprolith |
| BSMD075 | 20.2 | 21.5 | 1.3 | 4.1 | Saprolith |
| BSMD075 | 21.5 | 22.6 | 1.1 | 2.5 | Saprolith |
| BSMD075 | 22.6 | 23.3 | 0.7 | 0.1 | Saprolith |
| BSMD075 | 23.3 | 24.0 | 0.7 | 0.3 | Saprolith |
| BSMD075 | 24.0 | 24.8 | 0.8 | 1.5 | Saprolith |
| BSMD075 | 24.8 | 25.7 | 1.0 | 0.9 | Saprolith |
| BSMD075 | 25.7 | 26.6 | 0.8 | 0.9 | Saprolith |
| BSMD075 | 26.6 | 27.4 | 0.8 | 1.3 | Saprolith |
| BSMD075 | 27.4 | 28.5 | 1.1 | 1.6 | Saprolith |
| BSMD075 | 28.5 | 29.6 | 1.1 | 1.2 | Saprolith |
| BSMD075 | 29.6 | 30.3 | 0.7 | 2.0 | Saprolith |
| BSMD075 | 30.3 | 31.3 | 1.0 | 1.1 | Saprolith |
| BSMD075 | 31.3 | 32.3 | 1.0 | 1.2 | Saprolith |
| BSMD075 | 32.3 | 33.3 | 1.0 | 0.9 | Saprolith |
| BSMD075 | 33.3 | 34.2 | 0.9 | 1.4 | Saprolith |
| BSMD075 | 34.2 | 34.8 | 0.6 | 1.2 | Saprolith |
| BSMD075 | 34.8 | 35.7 | 0.9 | 1.5 | Saprolith |
| BSMD075 | 35.7 | 36.3 | 0.6 | 7.3 | Saprolith |
| BSMD075 | 36.3 | 36.9 | 0.6 | 1.6 | Saprolith |
| BSMD075 | 36.9 | 37.6 | 0.8 | 2.0 | Saprolith |
| BSMD075 | 37.6 | 38.3 | 0.7 | 3.0 | Saprolith |
| BSMD075 | 38.3 | 39.5 | 1.2 | 2.7 | Graphitic Gneiss |
| BSMD075 | 39.5 | 40.4 | 0.9 | 2.4 | Graphitic Gneiss |
| BSMD075 | 40.4 | 41.3 | 0.9 | 1.6 | Graphitic Gneiss |
| BSMD076 | 1.8 | 2.7 | 1.0 | 0.1 | Saprolith |
| BSMD076 | 2.7 | 3.4 | 0.7 | 2.0 | Saprolith |
| BSMD076 | 3.4 | 4.1 | 0.7 | 13.6 | Saprolith |
| BSMD076 | 4.1 | 4.9 | 0.8 | 10.4 | Saprolith |
| BSMD076 | 4.9 | 5.8 | 0.9 | 10.4 | Saprolith |
| BSMD076 | 5.8 | 6.5 | 0.8 | 2.0 | Saprolith |
| Drill hole ID | From(m) | To(m) | Interval(m) | TGC(%) | Lithology |
| BSMD076 | 6.5 | 7.7 | 1.1 | 0.8 | Saprolith |
| BSMD076 | 7.7 | 8.4 | 0.7 | 0.5 | Saprolith |
| BSMD076 | 8.4 | 9.0 | 0.6 | 0.4 | Saprolith |
| BSMD076 | 9.0 | 9.6 | 0.6 | 1.0 | Saprolith |
| BSMD076 | 9.6 | 10.6 | 1.0 | 0.9 | Saprolith |
| BSMD076 | 10.6 | 11.2 | 0.5 | 1.3 | Saprolith |
| BSMD076 | 11.2 | 12.4 | 1.2 | 1.0 | Saprolith |
| BSMD076 | 12.4 | 13.2 | 0.9 | 1.9 | Saprolith |
| BSMD076 | 13.2 | 14.2 | 0.9 | 1.8 | Saprolith |
| BSMD076 | 14.2 | 15.1 | 0.9 | 3.2 | Saprolith |
| BSMD076 | 15.1 | 16.0 | 0.9 | 2.4 | Saprolith |
| BSMD076 | 16.0 | 17.0 | 1.0 | 4.5 | Saprolith |
| BSMD076 | 17.0 | 17.8 | 0.8 | 3.8 | Saprolith |
| BSMD076 | 17.8 | 18.7 | 0.9 | 4.2 | Saprolith |
| BSMD076 | 18.7 | 19.5 | 0.9 | 2.4 | Saprolith |
| BSMD076 | 19.5 | 20.3 | 0.8 | 3.5 | Saprolith |
| BSMD076 | 20.3 | 21.0 | 0.7 | 1.5 | Saprolith |
| BSMD076 | 21.0 | 21.4 | 0.4 | 1.8 | Saprolith |
| BSMD076 | 21.4 | 22.3 | 0.9 | 3.6 | Saprolith |
| BSMD076 | 22.3 | 23.3 | 1.0 | 1.3 | Saprolith |
| BSMD076 | 23.3 | 24.3 | 1.0 | 0.0 | Saprolith |
| BSMD077 | 1.5 | 1.9 | 0.4 | 0.1 | Saprolith |
| BSMD077 | 1.9 | 2.6 | 0.7 | 1.2 | Saprolith |
| BSMD077 | 2.6 | 3.8 | 1.2 | 0.5 | Saprolith |
| BSMD077 | 4.3 | 5.1 | 0.9 | 1.5 | Saprolith |
| BSMD077 | 5.1 | 5.6 | 0.5 | 0.8 | Saprolith |
| BSMD077 | 5.6 | 6.4 | 0.8 | 0.8 | Saprolith |
| BSMD077 | 6.4 | 7.3 | 0.9 | 0.8 | Saprolith |
| BSMD077 | 7.3 | 8.1 | 0.9 | 0.8 | Saprolith |
| BSMD077 | 8.1 | 9.0 | 0.8 | 0.5 | Saprolith |
| BSMD077 | 9.0 | 9.4 | 0.5 | 0.6 | Saprolith |
| BSMD077 | 9.4 | 10.2 | 0.7 | 1.0 | Saprolith |
| BSMD077 | 10.2 | 10.9 | 0.8 | 1.8 | Saprolith |
| BSMD077 | 10.9 | 11.6 | 0.7 | 1.3 | Saprolith |
| BSMD077 | 11.6 | 12.4 | 0.8 | 1.1 | Saprolith |
| BSMD077 | 12.4 | 13.2 | 0.8 | 1.9 | Saprolith |
| BSMD077 | 13.2 | 14.0 | 0.8 | 1.3 | Saprolith |
| BSMD077 | 14.0 | 14.9 | 0.9 | 4.2 | Saprolith |
| BSMD077 | 14.9 | 15.9 | 1.0 | 1.4 | Saprolith |
| BSMD077 | 15.9 | 16.3 | 0.4 | 0.7 | Saprolith |
| BSMD077 | 16.3 | 16.7 | 0.4 | 2.1 | Saprolith |
| BSMD077 | 16.7 | 17.5 | 0.8 | 1.0 | Saprolith |
| BSMD077 | 17.5 | 18.3 | 0.8 | 4.3 | Saprolith |
| BSMD077 | 18.3 | 19.1 | 0.8 | 1.2 | Saprolith |
| BSMD077 | 19.1 | 19.9 | 0.8 | 1.8 | Saprolith |
| BSMD077 | 19.9 | 20.9 | 0.9 | 1.8 | Saprolith |
| BSMD077 | 20.9 | 21.8 | 0.9 | 1.6 | Saprolith |
| BSMD077 | 21.8 | 22.7 | 1.0 | 3.5 | Saprolith |
| BSMD077 | 22.7 | 23.7 | 1.0 | 1.1 | Saprolith |
| Drill hole ID | From(m) | To(m) | Interval(m) | TGC(%) | Lithology |
| BSMD077 | 23.7 | 24.5 | 0.8 | 7.0 | Saprolith |
| BSMD077 | 24.5 | 25.5 | 1.0 | 0.8 | Saprolith |
| BSMD077 | 25.5 | 26.3 | 0.8 | 0.5 | Saprolith |
| BSMD077 | 26.3 | 26.8 | 0.6 | 1.1 | Saprolith |
| BSMD077 | 26.8 | 27.4 | 0.6 | 1.2 | Saprolith |
| BSMD077 | 27.4 | 28.4 | 1.0 | 0.5 | Saprolith |
| BSMD077 | 28.4 | 29.5 | 1.1 | 0.5 | Saprolith |
| BSMD077 | 29.5 | 30.4 | 0.9 | 1.6 | Saprolith |
| BSMD077 | 30.4 | 31.2 | 0.8 | 1.4 | Saprolith |
| BSMD077 | 31.2 | 32.0 | 0.8 | 2.7 | Saprolith |
| BSMD077 | 32.0 | 32.8 | 0.8 | 1.9 | Saprolith |
| BSMD077 | 32.8 | 33.5 | 0.7 | 6.6 | Graphitic Gneiss |
| BSMD077 | 33.5 | 34.2 | 0.7 | 6.2 | Graphitic Gneiss |
| BSMD077 | 34.2 | 34.8 | 0.6 | 3.3 | Graphitic Gneiss |
| BSMD078 | 0.9 | 1.9 | 1.0 | 2.7 | Pedolith |
| BSMD078 | 1.9 | 2.6 | 0.7 | 1.8 | Saprolith |
| BSMD078 | 2.6 | 3.2 | 0.6 | 4.1 | Saprolith |
| BSMD078 | 3.2 | 4.0 | 0.8 | 2.3 | Saprolith |
| BSMD078 | 4.0 | 4.9 | 0.9 | 3.0 | Saprolith |
| BSMD078 | 4.9 | 5.5 | 0.6 | 3.2 | Saprolith |
| BSMD078 | 5.5 | 6.1 | 0.5 | 1.5 | Saprolith |
| BSMD078 | 6.1 | 6.6 | 0.6 | 3.2 | Saprolith |
| BSMD078 | 6.6 | 7.3 | 0.7 | 4.2 | Saprolith |
| BSMD078 | 7.3 | 8.0 | 0.6 | 3.1 | Saprolith |
| BSMD078 | 8.0 | 9.0 | 1.1 | 2.3 | Saprolith |
| BSMD078 | 9.0 | 9.8 | 0.8 | 2.2 | Saprolith |
| BSMD078 | 9.8 | 10.6 | 0.7 | 2.6 | Saprolith |
| BSMD078 | 10.6 | 11.3 | 0.7 | 0.0 | Dolerite |
| BSMD078 | 11.3 | 12.2 | 1.0 | 0.0 | Dolerite |
| BSMD078 | 12.2 | 13.2 | 1.0 | 0.0 | Dolerite |
| BSMD078 | 13.2 | 14.3 | 1.1 | 0.0 | Dolerite |
| BSMD078 | 14.3 | 15.3 | 1.1 | 0.0 | Dolerite |
| BSMD078 | 15.3 | 16.9 | 1.6 | 1.5 | Saprolith |
| BSMD078 | 16.9 | 18.0 | 1.1 | 2.1 | Saprolith |
| BSMD078 | 18.0 | 18.4 | 0.5 | 0.4 | Saprolith |
| BSMD078 | 18.4 | 19.5 | 1.1 | 3.7 | Saprolith |
| BSMD078 | 19.5 | 20.5 | 1.0 | 0.4 | Saprolith |
| BSMD078 | 20.5 | 21.6 | 1.2 | 0.2 | Saprolith |
| BSMD078 | 21.6 | 22.5 | 0.8 | 2.7 | Saprolith |
| BSMD078 | 22.5 | 23.1 | 0.7 | 2.4 | Saprolith |
| BSMD078 | 23.1 | 23.7 | 0.6 | 7.2 | Graphitic Gneiss |
| BSMD078 | 23.7 | 24.4 | 0.7 | 4.6 | Graphitic Gneiss |
| BSMD078 | 24.4 | 25.1 | 0.7 | 2.5 | Graphitic Gneiss |
| BSMD078 | 25.1 | 25.9 | 0.8 | 5.0 | Graphitic Gneiss |
| BSMD078 | 25.9 | 26.3 | 0.5 | 3.5 | Graphitic Gneiss |
| BSMD079 | 0.0 | 0.7 | 0.7 | 0.0 | Saprolith |
| BSMD079 | 0.7 | 1.1 | 0.4 | 0.2 | Saprolith |
| BSMD079 | 1.1 | 1.7 | 0.5 | 1.3 | Saprolith |
| BSMD079 | 1.7 | 2.3 | 0.6 | 2.6 | Saprolith |
| Drill hole ID | From(m) | To(m) | Interval(m) | TGC(%) | Lithology |
| BSMD079 | 2.3 | 3.0 | 0.7 | 3.0 | Saprolith |
| BSMD079 | 3.0 | 3.8 | 0.8 | 4.2 | Saprolith |
| BSMD079 | 3.8 | 4.4 | 0.7 | 4.0 | Saprolith |
| BSMD079 | 4.4 | 5.1 | 0.6 | 3.7 | Saprolith |
| BSMD079 | 5.1 | 5.9 | 0.9 | 3.3 | Saprolith |
| BSMD079 | 5.9 | 6.8 | 0.9 | 3.2 | Saprolith |
| BSMD079 | 6.8 | 7.6 | 0.8 | 2.5 | Saprolith |
| BSMD079 | 7.6 | 8.5 | 0.9 | 3.3 | Saprolith |
| BSMD079 | 8.5 | 9.4 | 0.8 | 3.0 | Saprolith |
| BSMD079 | 9.4 | 10.2 | 0.8 | 3.0 | Saprolith |
| BSMD079 | 10.2 | 11.0 | 0.8 | 3.0 | Saprolith |
| BSMD079 | 11.0 | 12.0 | 1.1 | 0.2 | Dolerite |
| BSMD079 | 12.0 | 13.0 | 1.0 | 0.0 | Dolerite |
| BSMD079 | 13.0 | 14.2 | 1.1 | 0.0 | Dolerite |
| BSMD079 | 14.2 | 15.1 | 0.9 | 0.0 | Dolerite |
| BSMD079 | 15.1 | 16.1 | 1.0 | 0.0 | Dolerite |
| BSMD079 | 16.1 | 17.1 | 1.0 | 3.9 | Saprolith |
| BSMD079 | 17.1 | 17.7 | 0.6 | 2.5 | Saprolith |
| BSMD079 | 17.7 | 18.4 | 0.7 | 2.3 | Saprolith |
| BSMD079 | 18.4 | 19.0 | 0.6 | 1.2 | Saprolith |
| BSMD079 | 19.0 | 19.8 | 0.9 | 2.6 | Saprolith |
| BSMD079 | 19.8 | 20.7 | 0.9 | 2.1 | Saprolith |
| BSMD079 | 20.7 | 21.5 | 0.8 | 1.8 | Saprolith |
| BSMD079 | 21.5 | 22.6 | 1.1 | 0.0 | Saprolith |
| BSMD079 | 22.6 | 23.3 | 0.7 | 0.9 | Saprolith |
| BSMD079 | 23.3 | 24.1 | 0.7 | 1.1 | Saprolith |
| BSMD079 | 24.1 | 24.9 | 0.8 | 1.8 | Saprolith |
| BSMD079 | 24.9 | 25.6 | 0.8 | 1.1 | Saprolith |
| BSMD079 | 25.6 | 26.5 | 0.9 | 1.5 | Saprolith |
| BSMD079 | 26.5 | 27.3 | 0.8 | 1.0 | Saprolith |
| BSMD079 | 27.3 | 28.0 | 0.7 | 0.9 | Saprolith |
| BSMD079 | 28.0 | 28.6 | 0.6 | 1.7 | Saprolith |
| BSMD079 | 28.6 | 29.5 | 0.9 | 3.2 | Saprolith |
| BSMD079 | 29.5 | 30.3 | 0.8 | 5.6 | Saprolith |
| BSMD079 | 30.3 | 30.9 | 0.6 | 3.5 | Saprolith |
| BSMD079 | 30.9 | 31.5 | 0.6 | 4.5 | Saprolith |
| BSMD079 | 31.5 | 32.4 | 1.0 | 3.7 | Graphitic Gneiss |
| BSMD079 | 32.4 | 33.4 | 0.9 | 2.9 | Graphitic Gneiss |
| BSMD079 | 33.4 | 34.3 | 1.0 | 2.4 | Graphitic Gneiss |
| BSMD079 | 34.3 | 35.2 | 0.9 | 1.4 | Graphitic Gneiss |
| BSMD080 | 1.1 | 1.9 | 0.8 | 0.1 | Pedolith |
| BSMD080 | 1.9 | 2.8 | 0.9 | 0.2 | Saprolith |
| BSMD080 | 2.8 | 3.6 | 0.8 | 0.0 | Saprolith |
| BSMD080 | 3.6 | 4.1 | 0.5 | 0.0 | Saprolith |
| BSMD080 | 4.1 | 4.7 | 0.6 | 0.0 | Saprolith |
| BSMD080 | 4.7 | 5.4 | 0.7 | 0.0 | Saprolith |
| BSMD080 | 5.4 | 6.1 | 0.7 | 0.0 | Saprolith |
| BSMD080 | 6.1 | 6.7 | 0.6 | 0.4 | Saprolith |
| BSMD080 | 6.7 | 7.6 | 0.9 | 1.2 | Saprolith |
| Drill hole ID | From(m) | To(m) | Interval(m) | TGC(%) | Lithology |
| BSMD080 | 7.6 | 8.4 | 0.8 | 3.2 | Saprolith |
| BSMD080 | 8.4 | 9.2 | 0.8 | 3.5 | Saprolith |
| BSMD080 | 9.2 | 10.0 | 0.8 | 3.0 | Saprolith |
| BSMD080 | 10.0 | 10.9 | 0.9 | 3.2 | Saprolith |
| BSMD080 | 10.9 | 11.8 | 0.9 | 3.5 | Saprolith |
| BSMD080 | 11.8 | 12.6 | 0.8 | 4.2 | Saprolith |
| BSMD080 | 12.6 | 13.4 | 0.8 | 6.7 | Saprolith |
| BSMD080 | 13.4 | 14.3 | 1.0 | 6.5 | Saprolith |
| BSMD080 | 14.3 | 15.4 | 1.1 | 10.9 | Saprolith |
| BSMD080 | 15.4 | 16.4 | 1.0 | 10.1 | Saprolith |
| BSMD080 | 16.4 | 16.7 | 0.4 | 3.1 | Saprolith |
| BSMD080 | 16.7 | 17.6 | 0.8 | 1.9 | Saprolith |
| BSMD080 | 17.6 | 18.5 | 0.9 | 0.8 | Saprolith |
| BSMD080 | 18.5 | 19.1 | 0.6 | 3.4 | Saprolith |
| BSMD080 | 19.1 | 20.0 | 0.9 | 1.4 | Saprolith |
| BSMD080 | 20.0 | 20.8 | 0.8 | 1.0 | Saprolith |
| BSMD080 | 20.8 | 21.2 | 0.5 | 1.1 | Saprolith |
| BSMD080 | 21.2 | 22.1 | 0.9 | 1.8 | Saprolith |
| BSMD080 | 22.1 | 23.1 | 1.0 | 1.7 | Saprolith |
| BSMD080 | 23.1 | 23.6 | 0.5 | 0.4 | Saprolith |
| BSMD080 | 23.6 | 24.5 | 0.9 | 1.3 | Saprolith |
| BSMD080 | 24.5 | 25.2 | 0.8 | 1.4 | Saprolith |
| BSMD080 | 25.2 | 26.0 | 0.8 | 1.7 | Saprolith |
| BSMD080 | 26.0 | 27.4 | 1.4 | 4.8 | Saprolith |
| BSMD080 | 27.4 | 28.0 | 0.6 | 5.6 | Saprolith |
| BSMD080 | 28.0 | 28.6 | 0.6 | 2.9 | Saprolith |
| BSMD080 | 28.6 | 29.6 | 1.0 | 2.6 | Graphitic Gneiss |
| BSMD080 | 29.6 | 30.6 | 1.0 | 3.4 | Graphitic Gneiss |
| BSMD080 | 30.6 | 31.5 | 0.9 | 2.4 | Graphitic Gneiss |
| BSMD080 | 31.5 | 32.4 | 0.9 | 2.9 | Graphitic Gneiss |
| BSMD081 | 8.3 | 9.6 | 1.2 | 0.3 | Saprolith |
| BSMD081 | 9.6 | 10.2 | 0.6 | 3.4 | Saprolith |
| BSMD081 | 10.2 | 11.0 | 0.9 | 1.0 | Saprolith |
| BSMD081 | 11.0 | 11.7 | 0.7 | 1.3 | Saprolith |
| BSMD081 | 11.7 | 12.3 | 0.7 | 2.9 | Saprolith |
| BSMD081 | 12.3 | 12.9 | 0.6 | 6.1 | Saprolith |
| BSMD081 | 12.9 | 13.6 | 0.7 | 7.8 | Saprolith |
| BSMD081 | 13.6 | 14.2 | 0.6 | 10.1 | Saprolith |
| BSMD081 | 14.2 | 14.9 | 0.6 | 7.0 | Saprolith |
| BSMD081 | 14.9 | 15.6 | 0.7 | 9.6 | Saprolith |
| BSMD081 | 15.6 | 16.5 | 0.9 | 7.6 | Saprolith |
| BSMD081 | 16.5 | 17.4 | 1.0 | 10.0 | Saprolith |
| BSMD081 | 17.4 | 18.0 | 0.6 | 4.7 | Saprolith |
| BSMD081 | 18.0 | 19.3 | 1.4 | 5.6 | Saprolith |
| BSMD081 | 19.3 | 19.9 | 0.5 | 6.8 | Saprolith |
| BSMD081 | 19.9 | 20.6 | 0.7 | 3.9 | Saprolith |
| BSMD081 | 20.6 | 21.5 | 0.9 | 1.9 | Saprolith |
| BSMD081 | 21.5 | 22.5 | 1.0 | 2.1 | Saprolith |
| BSMD081 | 22.5 | 23.3 | 0.8 | 2.8 | Saprolith |
| Drill hole ID | From(m) | To(m) | Interval(m) | TGC(%) | Lithology |
| BSMD081 | 23.3 | 24.3 | 1.0 | 2.7 | Graphitic Gneiss |
| BSMD081 | 24.3 | 25.1 | 0.8 | 1.7 | Graphitic Gneiss |
| BSMD081 | 25.1 | 26.3 | 1.2 | 2.5 | Graphitic Gneiss |
| BSMD082 | 4.9 | 5.8 | 0.9 | <0.05 | Saprolith |
| BSMD082 | 5.8 | 6.2 | 0.5 | 0.3 | Saprolith |
| BSMD082 | 6.2 | 7.5 | 1.3 | 0.3 | Saprolith |
| BSMD082 | 7.5 | 8.4 | 0.9 | 3.6 | Saprolith |
| BSMD082 | 8.4 | 8.8 | 0.4 | 0.1 | Saprolith |
| BSMD082 | 8.8 | 9.4 | 0.6 | 2.6 | Saprolith |
| BSMD082 | 9.4 | 10.1 | 0.7 | 1.2 | Saprolith |
| BSMD082 | 10.1 | 10.9 | 0.8 | 1.1 | Saprolith |
| BSMD082 | 10.9 | 11.6 | 0.8 | 3.8 | Saprolith |
| BSMD082 | 11.6 | 12.6 | 0.9 | 1.0 | Saprolith |
| BSMD082 | 12.6 | 13.9 | 1.3 | 6.2 | Saprolith |
| BSMD082 | 13.9 | 14.7 | 0.8 | 7.7 | Saprolith |
| BSMD082 | 14.7 | 16.4 | 1.8 | 6.4 | Saprolith |
| BSMD082 | 16.4 | 17.2 | 0.8 | 5.3 | Saprolith |
| BSMD082 | 17.2 | 18.0 | 0.8 | 8.5 | Saprolith |
| BSMD082 | 18.0 | 18.9 | 0.9 | 4.8 | Saprolith |
| BSMD082 | 18.9 | 19.8 | 0.9 | 5.3 | Saprolith |
| BSMD082 | 19.8 | 20.4 | 0.6 | 5.4 | Saprolith |
| BSMD082 | 20.4 | 21.5 | 1.1 | 2.4 | Graphitic Gneiss |
| BSMD082 | 21.5 | 22.5 | 1.0 | 2.4 | Graphitic Gneiss |
| BSMD082 | 22.5 | 23.4 | 0.9 | 1.9 | Graphitic Gneiss |
| BSMD082 | 23.4 | 24.4 | 1.0 | 2.3 | Graphitic Gneiss |
| BSMD083 | 9.3 | 9.8 | 0.5 | 0.2 | Saprolith |
| BSMD083 | 9.8 | 10.2 | 0.4 | 5.6 | Saprolith |
| BSMD083 | 10.2 | 10.6 | 0.4 | 1.0 | Saprolith |
| BSMD083 | 10.6 | 11.4 | 0.8 | 10.9 | Saprolith |
| BSMD083 | 11.4 | 11.7 | 0.4 | 4.9 | Saprolith |
| BSMD083 | 11.7 | 12.2 | 0.5 | 7.4 | Saprolith |
| BSMD083 | 12.2 | 12.7 | 0.5 | 4.0 | Saprolith |
| BSMD083 | 12.7 | 13.1 | 0.4 | 12.0 | Saprolith |
| BSMD083 | 13.1 | 13.8 | 0.7 | 5.7 | Saprolith |
| BSMD083 | 13.8 | 14.5 | 0.7 | 12.6 | Saprolith |
| BSMD083 | 14.5 | 15.2 | 0.7 | 8.9 | Saprolith |
| BSMD083 | 15.2 | 15.9 | 0.7 | 8.9 | Saprolith |
| BSMD083 | 15.9 | 16.6 | 0.7 | 8.1 | Saprolith |
| BSMD083 | 16.6 | 17.3 | 0.7 | 11.3 | Saprolith |
| BSMD083 | 17.3 | 18.2 | 0.9 | 7.3 | Saprolith |
| BSMD083 | 18.2 | 19.0 | 0.8 | 5.9 | Saprolith |
| BSMD083 | 19.0 | 19.9 | 0.9 | 7.8 | Saprolith |
| BSMD083 | 19.9 | 20.9 | 1.0 | 4.9 | Saprolith |
| BSMD083 | 20.9 | 21.9 | 1.0 | 5.9 | Saprolith |
| BSMD083 | 21.9 | 22.8 | 0.9 | 7.7 | Saprolith |
| BSMD083 | 22.8 | 23.6 | 0.8 | 6.5 | Saprolith |
| BSMD083 | 23.6 | 24.5 | 0.9 | 0.7 | Saprolith |
| BSMD083 | 24.5 | 25.5 | 1.0 | 2.3 | Saprolith |
| BSMD083 | 25.5 | 26.4 | 0.9 | 2.7 | Saprolith |
| Drill hole ID | From(m) | To(m) | Interval(m) | TGC(%) | Lithology |
| BSMD083 | 26.4 | 27.4 | 1.0 | 2.2 | Saprolith |
| BSMD083 | 27.4 | 28.0 | 0.6 | 1.4 | Saprolith |
| BSMD083 | 28.0 | 29.0 | 1.0 | 2.7 | Saprolith |
| BSMD083 | 29.0 | 30.0 | 0.9 | 1.8 | Saprolith |
| BSMD083 | 30.0 | 31.1 | 1.1 | 6.8 | Saprolith |
| BSMD083 | 31.1 | 32.3 | 1.2 | 10.8 | Saprolith |
| BSMD083 | 32.3 | 33.3 | 1.0 | 8.7 | Saprolith |
| BSMD083 | 33.3 | 34.3 | 1.1 | 9.7 | Saprolith |
| BSMD083 | 34.3 | 35.0 | 0.7 | 9.6 | Saprolith |
| BSMD083 | 35.0 | 36.4 | 1.4 | 5.8 | Saprolith |
| BSMD083 | 36.4 | 37.4 | 1.0 | 4.8 | Saprolith |
| BSMD083 | 37.4 | 38.4 | 1.0 | 6.6 | Saprolith |
| BSMD083 | 38.4 | 39.5 | 1.0 | 4.3 | Saprolith |
| BSMD083 | 39.5 | 40.1 | 0.7 | 4.0 | Saprolith |
| BSMD083 | 40.1 | 40.9 | 0.7 | 5.3 | Saprolith |
| BSMD083 | 40.9 | 41.6 | 0.7 | 6.1 | Saprolith |
| BSMD083 | 41.6 | 41.9 | 0.4 | 6.6 | Saprolith |
| BSMD083 | 41.9 | 42.8 | 0.8 | 5.7 | Saprolith |
| BSMD083 | 42.8 | 43.8 | 1.0 | 5.4 | Saprolith |
| BSMD083 | 43.8 | 44.6 | 0.9 | 4.2 | Saprolith |
| BSMD083 | 44.6 | 45.5 | 0.8 | 8.7 | Saprolith |
| BSMD083 | 45.5 | 46.5 | 1.0 | 5.8 | Graphitic Gneiss |
| BSMD083 | 46.5 | 47.3 | 0.9 | 6.8 | Graphitic Gneiss |
| BSMD084 | 6.9 | 7.7 | 0.8 | 0.1 | Pedolith |
| BSMD084 | 7.7 | 8.6 | 0.8 | 0.7 | Saprolith |
| BSMD084 | 8.6 | 9.3 | 0.8 | 6.2 | Saprolith |
| BSMD084 | 9.3 | 10.2 | 0.9 | 9.3 | Saprolith |
| BSMD084 | 10.2 | 10.7 | 0.5 | 8.0 | Saprolith |
| BSMD084 | 10.7 | 11.4 | 0.7 | 10.1 | Saprolith |
| BSMD084 | 11.4 | 12.3 | 0.9 | 6.0 | Saprolith |
| BSMD084 | 12.3 | 13.1 | 0.9 | 6.3 | Saprolith |
| BSMD084 | 13.1 | 13.9 | 0.8 | 11.9 | Saprolith |
| BSMD084 | 13.9 | 14.8 | 0.9 | 3.4 | Saprolith |
| BSMD084 | 14.8 | 15.7 | 0.9 | 5.6 | Saprolith |
| BSMD084 | 15.7 | 16.3 | 0.6 | 6.6 | Saprolith |
| BSMD084 | 16.3 | 17.0 | 0.7 | 5.6 | Saprolith |
| BSMD084 | 17.0 | 17.7 | 0.7 | 6.1 | Saprolith |
| BSMD084 | 17.7 | 18.4 | 0.7 | 7.0 | Saprolith |
| BSMD084 | 18.4 | 18.7 | 0.3 | 0.2 | Saprolith |
| BSMD084 | 18.7 | 19.3 | 0.6 | 1.4 | Saprolith |
| BSMD084 | 19.3 | 20.0 | 0.7 | 2.5 | Saprolith |
| BSMD084 | 20.0 | 20.8 | 0.7 | 3.0 | Saprolith |
| BSMD084 | 20.8 | 21.7 | 0.9 | 3.0 | Saprolith |
| BSMD084 | 21.7 | 22.6 | 1.0 | 1.7 | Saprolith |
| BSMD084 | 22.6 | 23.3 | 0.7 | 0.9 | Saprolith |
| BSMD084 | 23.3 | 23.9 | 0.6 | 1.2 | Saprolith |
| BSMD084 | 23.9 | 24.6 | 0.7 | 2.4 | Saprolith |
| BSMD084 | 24.6 | 25.3 | 0.6 | 1.8 | Saprolith |
| BSMD084 | 25.3 | 26.0 | 0.8 | 10.2 | Saprolith |
| Drill hole ID | From(m) | To(m) | Interval(m) | TGC(%) | Lithology |
| BSMD084 | 26.0 | 27.6 | 1.6 | 5.2 | Saprolith |
| BSMD084 | 27.6 | 28.9 | 1.4 | 8.9 | Saprolith |
| BSMD084 | 28.9 | 29.6 | 0.6 | 18.4 | Saprolith |
| BSMD084 | 29.6 | 30.7 | 1.2 | 7.7 | Saprolith |
| BSMD084 | 30.7 | 31.3 | 0.5 | 4.2 | Saprolith |
| BSMD084 | 31.3 | 31.9 | 0.6 | 4.3 | Saprolith |
| BSMD084 | 31.9 | 32.6 | 0.7 | 5.8 | Graphitic Gneiss |
| BSMD084 | 32.6 | 33.5 | 0.9 | 4.5 | Graphitic Gneiss |
| BSMD084 | 33.5 | 34.3 | 0.9 | 2.0 | Graphitic Gneiss |
| BSMD084 | 34.3 | 35.3 | 0.9 | 1.9 | Graphitic Gneiss |
| BSMD089 | 5.5 | 6.7 | 1.2 | 0.4 | Saprolith |
| BSMD089 | 6.7 | 7.3 | 0.6 | 1.9 | Saprolith |
| BSMD089 | 7.3 | 8.3 | 0.9 | 2.9 | Saprolith |
| BSMD089 | 8.3 | 8.9 | 0.6 | 2.2 | Saprolith |
| BSMD089 | 8.9 | 9.3 | 0.5 | 3.7 | Saprolith |
| BSMD089 | 9.3 | 9.9 | 0.6 | 3.6 | Saprolith |
| BSMD089 | 9.9 | 10.5 | 0.6 | 3.7 | Saprolith |
| BSMD089 | 10.5 | 11.3 | 0.8 | 5.9 | Saprolith |
| BSMD089 | 11.3 | 11.9 | 0.6 | 4.7 | Saprolith |
| BSMD089 | 11.9 | 12.6 | 0.6 | 4.6 | Saprolith |
| BSMD089 | 12.6 | 13.2 | 0.7 | 5.7 | Saprolith |
| BSMD089 | 13.2 | 13.8 | 0.6 | 6.9 | Saprolith |
| BSMD089 | 13.8 | 14.3 | 0.5 | 7.7 | Saprolith |
| BSMD089 | 14.3 | 14.9 | 0.5 | 8.1 | Saprolith |
| BSMD089 | 14.9 | 15.3 | 0.5 | 6.6 | Saprolith |
| BSMD089 | 15.3 | 15.9 | 0.6 | 4.6 | Saprolith |
| BSMD089 | 15.9 | 17.1 | 1.2 | 2.0 | Saprolith |
| BSMD089 | 17.1 | 18.2 | 1.1 | 1.7 | Graphitic Gneiss |
| BSMD089 | 18.2 | 19.1 | 0.9 | 0.1 | Gneiss |
| BSMD089 | 19.1 | 20.0 | 0.9 | 1.8 | Graphitic Gneiss |
| BSMD089 | 20.0 | 21.2 | 1.2 | 0.7 | Graphitic Gneiss |
| BSMD089 | 21.2 | 22.1 | 0.9 | 1.5 | Graphitic Gneiss |
| BSMD089 | 22.1 | 23.1 | 1.0 | 0.9 | Graphitic Gneiss |
| BSMD089 | 23.1 | 24.3 | 1.2 | 1.7 | Graphitic Gneiss |
| BSMD090 | 5.9 | 7.4 | 1.5 | 1.1 | Saprolith |
| BSMD090 | 7.4 | 8.5 | 1.2 | 2.5 | Saprolith |
| BSMD090 | 8.5 | 9.6 | 1.1 | 2.6 | Saprolith |
| BSMD090 | 9.6 | 10.7 | 1.1 | 3.5 | Saprolith |
| BSMD090 | 10.7 | 11.2 | 0.5 | 2.9 | Saprolith |
| BSMD090 | 11.2 | 12.4 | 1.1 | 6.3 | Saprolith |
| BSMD090 | 12.4 | 13.3 | 1.0 | 6.9 | Saprolith |
| BSMD090 | 13.3 | 14.0 | 0.6 | 6.5 | Saprolith |
| BSMD090 | 14.0 | 14.7 | 0.7 | 8.3 | Saprolith |
| BSMD090 | 14.7 | 15.4 | 0.7 | 7.0 | Saprolith |
| BSMD090 | 15.4 | 15.6 | 0.2 | 4.2 | Saprolith |
| BSMD090 | 15.6 | 16.5 | 0.9 | 3.9 | Saprolith |
| BSMD090 | 16.5 | 17.4 | 0.8 | 2.0 | Saprolith |
| BSMD090 | 17.4 | 18.1 | 0.7 | 1.5 | Saprolith |
| BSMD090 | 18.1 | 19.4 | 1.3 | 0.0 | Saprolith |
| Drill hole ID | From(m) | To(m) | Interval(m) | TGC(%) | Lithology |
| BSMD090 | 19.4 | 20.4 | 1.1 | 1.6 | Saprolith |
| BSMD090 | 20.4 | 21.5 | 1.1 | 0.8 | Saprolith |
| BSMD090 | 21.5 | 22.5 | 1.0 | 1.2 | Saprolith |
| BSMD090 | 22.5 | 23.5 | 1.0 | 1.1 | Saprolith |
| BSMD090 | 23.5 | 24.5 | 1.0 | 1.1 | Saprolith |
| BSMD090 | 24.5 | 25.5 | 1.0 | 1.2 | Saprolith |
| BSMD090 | 25.5 | 26.4 | 1.0 | 4.3 | Graphitic Gneiss |
| BSMD090 | 26.4 | 27.4 | 0.9 | 5.2 | Graphitic Gneiss |
| BSMD086 | 4.4 | 6.0 | 1.6 | 0.0 | Saprolith |
| BSMD086 | 6.0 | 6.5 | 0.5 | 1.5 | Saprolith |
| BSMD086 | 6.5 | 7.6 | 1.2 | 1.5 | Saprolith |
| BSMD087 | 1.1 | 1.9 | 0.8 | 0.2 | Pedolith |
| BSMD087 | 1.9 | 2.3 | 0.4 | 6.2 | Saprolith |
| BSMD087 | 2.3 | 2.8 | 0.5 | 0.9 | Saprolith |
| BSMD087 | 2.8 | 3.4 | 0.6 | 3.3 | Saprolith |
| BSMD087 | 3.4 | 4.3 | 0.9 | 3.0 | Saprolith |
| BSMD087 | 4.3 | 5.0 | 0.7 | 2.3 | Saprolith |
| BSMD087 | 5.0 | 5.6 | 0.6 | 2.1 | Saprolith |
| BSMD087 | 5.6 | 6.3 | 0.7 | 1.5 | Saprolith |
| BSMD087 | 6.3 | 7.0 | 0.7 | 0.8 | Saprolith |
| BSMD087 | 7.0 | 7.5 | 0.5 | 1.8 | Saprolith |
| BSMD087 | 7.5 | 7.8 | 0.3 | 1.5 | Saprolith |
| BSMD087 | 7.8 | 8.3 | 0.5 | 0.8 | Saprolith |
| BSMD087 | 8.3 | 8.8 | 0.5 | 1.8 | Saprolith |
| BSMD087 | 8.8 | 9.3 | 0.5 | 1.0 | Saprolith |
| BSMD087 | 9.3 | 9.9 | 0.5 | 1.2 | Saprolith |
| BSMD087 | 9.9 | 10.4 | 0.5 | 1.2 | Saprolith |
| BSMD087 | 10.4 | 11.6 | 1.2 | 1.5 | Saprolith |
| BSMD087 | 11.6 | 12.0 | 0.4 | 2.7 | Saprolith |
| BSMD087 | 12.0 | 12.6 | 0.7 | 1.2 | Saprolith |
| BSMD087 | 12.6 | 12.9 | 0.3 | 1.4 | Saprolith |
| BSMD087 | 12.9 | 13.3 | 0.4 | 1.0 | Saprolith |
| BSMD087 | 13.3 | 14.0 | 0.6 | 2.6 | Saprolith |
| BSMD087 | 14.0 | 14.7 | 0.8 | 1.8 | Saprolith |
| BSMD087 | 14.7 | 15.3 | 0.6 | 1.0 | Saprolith |
| BSMD087 | 15.3 | 15.9 | 0.6 | 2.1 | Saprolith |
| BSMD087 | 15.9 | 16.4 | 0.5 | 2.9 | Saprolith |
| BSMD087 | 16.4 | 17.3 | 0.8 | 3.1 | Saprolith |
| BSMD087 | 17.3 | 18.1 | 0.9 | 1.4 | Saprolith |
| BSMD087 | 18.1 | 18.9 | 0.8 | 1.4 | Saprolith |
| BSMD087 | 18.9 | 19.5 | 0.5 | 0.7 | Saprolith |
| BSMD087 | 19.5 | 20.0 | 0.6 | 1.4 | Saprolith |
| BSMD087 | 20.0 | 21.0 | 0.9 | 1.0 | Saprolith |
| BSMD087 | 21.0 | 21.9 | 1.0 | 2.0 | Saprolith |
| BSMD087 | 21.9 | 22.9 | 0.9 | 2.0 | Saprolith |
| BSMD087 | 22.9 | 24.0 | 1.1 | 1.4 | Saprolith |
| BSMD087 | 24.0 | 24.8 | 0.8 | 1.7 | Saprolith |
| BSMD087 | 24.8 | 25.6 | 0.8 | 6.6 | Graphitic Gneiss |
| BSMD087 | 25.6 | 26.4 | 0.8 | 2.1 | Graphitic Gneiss |
| Drill hole ID | From(m) | To(m) | Interval(m) | TGC(%) | Lithology |
| BSMD087 | 26.4 | 27.4 | 1.0 | 2.5 | Graphitic Gneiss |
| BSMD087 | 27.4 | 28.2 | 0.8 | 2.7 | Graphitic Gneiss |
| BSMD087 | 28.2 | 29.3 | 1.1 | 3.8 | Graphitic Gneiss |
| BSMD088 | 5.6 | 6.3 | 0.7 | 0.1 | Saprolith |
| BSMD088 | 6.3 | 7.4 | 1.1 | 3.3 | Saprolith |
| BSMD088 | 7.4 | 8.4 | 1.0 | 4.3 | Saprolith |
| BSMD088 | 8.4 | 9.4 | 1.0 | 4.5 | Saprolith |
| BSMD088 | 9.4 | 10.6 | 1.2 | 3.1 | Saprolith |
| BSMD088 | 10.6 | 11.7 | 1.1 | 3.0 | Saprolith |
| BSMD088 | 11.7 | 13.2 | 1.6 | 0.0 | Dolerite |
| BSMD088 | 13.2 | 14.9 | 1.7 | 0.0 | Dolerite |
| BSMD088 | 14.9 | 16.5 | 1.6 | 0.0 | Dolerite |
| BSMD088 | 16.5 | 17.6 | 1.1 | 2.4 | Saprolith |
| BSMD088 | 17.6 | 18.4 | 0.9 | 4.9 | Saprolith |
| BSMD088 | 18.4 | 19.4 | 1.0 | 3.0 | Saprolith |
| BSMD088 | 19.4 | 20.3 | 0.9 | 1.5 | Saprolith |
| BSMD088 | 20.3 | 20.9 | 0.6 | 0.5 | Saprolith |
| BSMD088 | 20.9 | 22.4 | 1.5 | 2.7 | Saprolith |
| BSMD088 | 22.4 | 23.4 | 1.0 | 1.6 | Saprolith |
| BSMD088 | 23.4 | 24.1 | 0.7 | 2.1 | Saprolith |
| BSMD088 | 24.1 | 24.9 | 0.8 | 3.0 | Saprolith |
| BSMD088 | 24.9 | 25.3 | 0.4 | 1.5 | Saprolith |
| BSMD088 | 25.3 | 25.9 | 0.6 | 0.7 | Saprolith |
| BSMD088 | 25.9 | 26.7 | 0.8 | 1.9 | Saprolith |
| BSMD088 | 26.7 | 27.4 | 0.8 | 1.7 | Saprolith |
| BSMD088 | 27.4 | 28.4 | 0.9 | 1.4 | Saprolith |
| BSMD088 | 28.4 | 28.9 | 0.6 | 2.2 | Saprolith |
| BSMD088 | 28.9 | 29.6 | 0.7 | 3.0 | Saprolith |
| BSMD088 | 29.6 | 30.7 | 1.1 | 2.9 | Graphitic Gneiss |
| BSMD088 | 30.7 | 31.7 | 0.9 | 6.5 | Graphitic Gneiss |
| BSMD088 | 31.7 | 32.4 | 0.7 | 3.2 | Graphitic Gneiss |
| BSMD091 | 6.3 | 7.6 | 1.4 | 1.5 | Saprolith |
| BSMD091 | 7.6 | 8.3 | 0.7 | 3.5 | Saprolith |
| BSMD091 | 8.3 | 8.8 | 0.6 | 3.9 | Saprolith |
| BSMD091 | 8.8 | 9.8 | 1.0 | 9.1 | Saprolith |
| BSMD091 | 9.8 | 10.2 | 0.4 | 4.6 | Saprolith |
| BSMD091 | 10.2 | 10.8 | 0.6 | 5.7 | Saprolith |
| BSMD091 | 10.8 | 11.7 | 0.9 | 4.0 | Saprolith |
| BSMD091 | 11.7 | 12.7 | 1.0 | 3.1 | Saprolith |
| BSMD091 | 12.7 | 13.5 | 0.8 | 8.7 | Saprolith |
| BSMD091 | 13.5 | 13.8 | 0.3 | 9.9 | Saprolith |
| BSMD091 | 13.8 | 14.8 | 1.0 | 3.6 | Saprolith |
| BSMD091 | 14.8 | 15.9 | 1.1 | 4.2 | Saprolith |
| BSMD091 | 15.9 | 16.6 | 0.7 | 2.7 | Saprolith |
| BSMD091 | 16.6 | 17.2 | 0.6 | 1.9 | Saprolith |
| BSMD091 | 17.2 | 17.9 | 0.7 | 3.5 | Saprolith |
| BSMD091 | 17.9 | 18.6 | 0.7 | 5.2 | Saprolith |
| BSMD091 | 18.6 | 19.3 | 0.7 | 4.4 | Saprolith |
| BSMD091 | 19.3 | 20.0 | 0.7 | 5.2 | Saprolith |
| Drill hole ID | From(m) | To(m) | Interval(m) | TGC(%) | Lithology |
| BSMD091 | 20.0 | 20.6 | 0.7 | 4.5 | Saprolith |
| BSMD091 | 20.6 | 21.4 | 0.8 | 4.7 | Saprolith |
| BSMD091 | 21.4 | 22.4 | 1.0 | 6.2 | Saprolith |
| BSMD091 | 22.4 | 23.6 | 1.2 | 4.3 | Saprolith |
| BSMD091 | 23.6 | 24.6 | 1.0 | 5.3 | Saprolith |
| BSMD091 | 24.6 | 25.6 | 1.0 | 5.4 | Saprolith |
| BSMD091 | 25.6 | 26.5 | 1.0 | 6.9 | Saprolith |
| BSMD091 | 26.5 | 27.6 | 1.1 | 5.2 | Saprolith |
| BSMD091 | 27.6 | 28.3 | 0.7 | 3.3 | Saprolith |
| BSMD091 | 28.3 | 29.1 | 0.8 | 4.1 | Saprolith |
| BSMD091 | 29.1 | 30.0 | 0.9 | 5.6 | Saprolith |
| BSMD091 | 30.0 | 30.8 | 0.8 | 6.8 | Saprolith |
| BSMD091 | 30.8 | 31.9 | 1.1 | 5.9 | Saprolith |
| BSMD091 | 31.9 | 32.6 | 0.8 | 4.9 | Saprolith |
| BSMD091 | 32.6 | 33.2 | 0.6 | 5.1 | Saprolith |
| BSMD091 | 33.2 | 33.5 | 0.4 | 3.5 | Saprolith |
| BSMD091 | 33.5 | 34.5 | 1.0 | 2.4 | Saprolith |
| BSMD091 | 34.5 | 35.2 | 0.7 | 0.1 | Saprolith |
| BSMD091 | 35.2 | 35.7 | 0.5 | 1.5 | Saprolith |
| BSMD091 | 35.7 | 37.0 | 1.3 | 0.5 | Saprolith |
| BSMD091 | 37.0 | 38.0 | 1.0 | 1.0 | Saprolith |
| BSMD091 | 38.0 | 39.1 | 1.1 | 2.6 | Saprolith |
| BSMD091 | 39.1 | 39.8 | 0.8 | 2.5 | Saprolith |
| BSMD091 | 39.8 | 40.7 | 0.9 | 1.0 | Graphitic Gneiss |
| BSMD091 | 40.7 | 41.5 | 0.9 | 1.6 | Graphitic Gneiss |
| BSMD091 | 41.5 | 42.5 | 0.9 | 1.8 | Graphitic Gneiss |
| BSMD091 | 42.5 | 43.4 | 0.9 | 1.7 | Graphitic Gneiss |
| BSMD092 | 3.7 | 4.3 | 0.6 | 0.1 | Saprolith |
| BSMD092 | 4.3 | 5.1 | 0.8 | 5.0 | Saprolith |
| BSMD092 | 5.1 | 5.9 | 0.8 | 4.9 | Saprolith |
| BSMD092 | 5.9 | 6.9 | 1.0 | 8.8 | Saprolith |
| BSMD092 | 6.9 | 7.6 | 0.7 | 6.1 | Saprolith |
| BSMD092 | 7.6 | 8.4 | 0.8 | 6.3 | Saprolith |
| BSMD092 | 8.4 | 9.0 | 0.6 | 2.9 | Saprolith |
| BSMD092 | 9.0 | 9.7 | 0.7 | 0.3 | Saprolith |
| BSMD092 | 9.7 | 10.1 | 0.4 | 2.5 | Saprolith |
| BSMD092 | 10.1 | 10.7 | 0.7 | 0.1 | Saprolith |
| BSMD092 | 10.7 | 11.2 | 0.4 | 0.8 | Saprolith |
| BSMD092 | 11.2 | 11.9 | 0.7 | 1.4 | Saprolith |
| BSMD092 | 11.9 | 12.9 | 1.0 | 1.0 | Saprolith |
| BSMD092 | 12.9 | 14.0 | 1.1 | 0.7 | Saprolith |
| BSMD092 | 14.0 | 14.9 | 0.9 | 1.0 | Saprolith |
| BSMD092 | 14.9 | 15.6 | 0.7 | 0.8 | Saprolith |
| BSMD092 | 15.6 | 16.4 | 0.8 | 1.1 | Saprolith |
| BSMD092 | 16.4 | 17.0 | 0.5 | 0.8 | Saprolith |
| BSMD092 | 17.0 | 18.3 | 1.4 | 1.3 | Saprolith |
| BSMD092 | 18.3 | 19.4 | 1.1 | 1.5 | Saprolith |
| BSMD092 | 19.4 | 20.1 | 0.6 | 3.3 | Saprolith |
| BSMD092 | 20.1 | 20.8 | 0.7 | 1.3 | Saprolith |
| Drill hole ID | From(m) | To(m) | Interval(m) | TGC(%) | Lithology |
| BSMD092 | 20.8 | 21.3 | 0.5 | 1.1 | Saprolith |
| BSMD092 | 21.3 | 22.1 | 0.8 | 1.6 | Saprolith |
| BSMD092 | 22.1 | 22.8 | 0.8 | 2.2 | Saprolith |
| BSMD092 | 22.8 | 23.9 | 1.0 | 1.2 | Saprolith |
| BSMD092 | 23.9 | 24.7 | 0.8 | 1.0 | Saprolith |
| BSMD092 | 24.7 | 25.7 | 1.0 | 1.3 | Saprolith |
| BSMD092 | 25.7 | 26.7 | 0.9 | 3.0 | Saprolith |
| BSMD092 | 26.7 | 27.6 | 1.0 | 2.2 | Saprolith |
| BSMD092 | 27.6 | 28.6 | 1.0 | 2.1 | Saprolith |
| BSMD092 | 28.6 | 29.7 | 1.1 | 2.8 | Saprolith |
| BSMD092 | 29.7 | 31.6 | 1.9 | 0.1 | Dolerite |
| BSMD092 | 31.6 | 33.4 | 1.8 | 0.0 | Dolerite |
| BSMD092 | 33.4 | 35.3 | 1.9 | 0.1 | Dolerite |
| BSMD092 | 35.3 | 36.4 | 1.1 | 1.6 | Saprolith |
| BSMD092 | 36.4 | 37.4 | 1.0 | 1.6 | Saprolith |
| BSMD092 | 37.4 | 38.4 | 1.0 | 2.6 | Saprolith |
| BSMD092 | 38.4 | 39.4 | 1.0 | 0.8 | Saprolith |
| BSMD092 | 39.4 | 40.5 | 1.1 | 2.0 | Saprolith |
| BSMD092 | 40.5 | 41.3 | 0.8 | 4.9 | Saprolith |
| BSMD092 | 41.3 | 42.0 | 0.8 | 3.4 | Saprolith |
| BSMD092 | 42.0 | 42.9 | 0.8 | 1.4 | Saprolith |
| BSMD092 | 42.9 | 43.9 | 1.0 | 0.9 | Saprolith |
| BSMD092 | 43.9 | 44.8 | 0.9 | 2.3 | Saprolith |
| BSMD092 | 44.8 | 45.4 | 0.6 | 0.9 | Saprolith |
| BSMD093 | 0.0 | 0.7 | 0.7 | 5.0 | Saprolith |
| BSMD093 | 0.7 | 1.6 | 0.8 | 2.8 | Saprolith |
| BSMD093 | 1.6 | 2.2 | 0.6 | 1.5 | Saprolith |
| BSMD093 | 2.2 | 3.0 | 0.8 | 2.0 | Saprolith |
| BSMD093 | 3.0 | 3.5 | 0.5 | 1.7 | Saprolith |
| BSMD093 | 3.5 | 4.0 | 0.5 | 4.0 | Saprolith |
| BSMD093 | 4.0 | 5.2 | 1.2 | 1.9 | Saprolith |
| BSMD093 | 5.2 | 5.8 | 0.6 | 1.5 | Saprolith |
| BSMD093 | 5.8 | 6.7 | 1.0 | 5.6 | Saprolith |
| BSMD093 | 6.7 | 7.5 | 0.8 | 2.4 | Saprolith |
| BSMD093 | 7.5 | 8.2 | 0.7 | 2.6 | Saprolith |
| BSMD093 | 8.2 | 9.0 | 0.7 | 2.5 | Saprolith |
| BSMD093 | 9.0 | 9.5 | 0.6 | 2.9 | Saprolith |
| BSMD093 | 9.5 | 9.9 | 0.4 | 2.3 | Saprolith |
| BSMD093 | 9.9 | 11.0 | 1.0 | 3.3 | Saprolith |
| BSMD093 | 11.0 | 12.0 | 1.0 | 2.8 | Saprolith |
| BSMD093 | 12.0 | 13.0 | 1.0 | 3.0 | Saprolith |
| BSMD093 | 13.0 | 14.0 | 1.0 | 2.8 | Saprolith |
| BSMD093 | 14.0 | 15.0 | 0.9 | 2.3 | Graphitic Gneiss |
| BSMD093 | 15.0 | 15.9 | 0.9 | 1.9 | Graphitic Gneiss |
| BSMD093 | 15.9 | 16.8 | 0.9 | 2.7 | Graphitic Gneiss |
| BSMD093 | 16.8 | 18.5 | 1.7 | 0.0 | Dolerite |
| BSMD093 | 18.5 | 20.3 | 1.8 | 0.0 | Dolerite |
| BSMD093 | 20.3 | 22.0 | 1.7 | 0.0 | Dolerite |
| BSMD093 | 22.0 | 23.8 | 1.8 | 0.0 | Dolerite |
| Drill hole ID | From(m) | To(m) | Interval(m) | TGC(%) | Lithology |
| BSMD093 | 23.8 | 25.5 | 1.7 | 0.0 | Dolerite |
| BSMD093 | 25.5 | 27.3 | 1.8 | 0.0 | Dolerite |
| BSMD093 | 27.3 | 29.1 | 1.9 | 0.0 | Dolerite |
| BSMD093 | 29.1 | 29.9 | 0.8 | 1.4 | Graphitic Gneiss |
| BSMD093 | 29.9 | 30.8 | 0.8 | 1.7 | Graphitic Gneiss |
| BSMD093 | 30.8 | 31.5 | 0.8 | 1.7 | Graphitic Gneiss |
| BSMD093 | 31.5 | 32.2 | 0.7 | 0.8 | Graphitic Gneiss |
| BSMD093 | 32.2 | 32.8 | 0.6 | 3.1 | Graphitic Gneiss |
| BSMD093 | 32.8 | 33.5 | 0.7 | 2.7 | Graphitic Gneiss |
| BSMD094 | 5.0 | 6.0 | 1.0 | 0.6 | Saprolith |
| BSMD094 | 6.0 | 6.8 | 0.7 | 1.1 | Saprolith |
| BSMD094 | 6.8 | 7.8 | 1.1 | 2.1 | Saprolith |
| BSMD094 | 7.8 | 8.3 | 0.4 | 0.6 | Saprolith |
| BSMD094 | 8.3 | 8.8 | 0.6 | 0.6 | Saprolith |
| BSMD094 | 8.8 | 11.0 | 2.2 | 2.0 | Saprolith |
| BSMD094 | 11.0 | 11.9 | 0.9 | 8.3 | Saprolith |
| BSMD094 | 11.9 | 12.9 | 1.0 | 1.6 | Saprolith |
| BSMD094 | 12.9 | 13.7 | 0.8 | 0.6 | Saprolith |
| BSMD094 | 13.7 | 14.7 | 1.0 | 0.8 | Saprolith |
| BSMD094 | 14.7 | 15.5 | 0.8 | 0.7 | Saprolith |
| BSMD094 | 15.5 | 16.5 | 1.0 | 2.7 | Saprolith |
| BSMD094 | 16.5 | 17.1 | 0.5 | 0.7 | Saprolith |
| BSMD094 | 17.1 | 18.0 | 0.9 | 1.6 | Saprolith |
| BSMD094 | 18.0 | 19.2 | 1.2 | 1.4 | Saprolith |
| BSMD094 | 19.2 | 19.5 | 0.3 | 5.1 | Saprolith |
| BSMD094 | 19.5 | 20.3 | 0.8 | 7.7 | Saprolith |
| BSMD094 | 20.3 | 21.2 | 0.9 | 7.0 | Saprolith |
| BSMD094 | 21.2 | 22.0 | 0.8 | 4.7 | Saprolith |
| BSMD094 | 22.0 | 23.2 | 1.2 | 2.9 | Saprolith |
| BSMD094 | 23.2 | 24.5 | 1.4 | 2.6 | Saprolith |
| BSMD094 | 24.5 | 25.3 | 0.8 | 4.3 | Saprolith |
| BSMD094 | 25.3 | 26.0 | 0.8 | 2.6 | Saprolith |
| BSMD094 | 26.0 | 26.9 | 0.9 | 3.3 | Saprolith |
| BSMD094 | 26.9 | 28.1 | 1.2 | 2.5 | Graphitic Gneiss |
| BSMD094 | 28.1 | 29.1 | 1.1 | 1.2 | Graphitic Gneiss |
| BSMD094 | 29.1 | 30.8 | 1.7 | 0.0 | Dolerite |
| BSMD094 | 30.8 | 32.5 | 1.7 | 0.0 | Dolerite |
| BSMD094 | 32.5 | 34.3 | 1.8 | 0.0 | Dolerite |
| BSMD094 | 34.3 | 35.9 | 1.6 | 0.0 | Dolerite |
| BSMD094 | 35.9 | 36.5 | 0.6 | 0.4 | Graphitic Gneiss |
| BSMD094 | 36.5 | 37.5 | 1.0 | 0.0 | Gneiss |
| BSMD095A | 10.8 | 11.0 | 0.3 | 1.1 | Saprolith |
| BSMD095A | 11.0 | 11.7 | 0.7 | 2.5 | Saprolith |
| BSMD095A | 11.7 | 12.5 | 0.7 | 3.6 | Saprolith |
| BSMD095A | 12.5 | 13.2 | 0.7 | 4.0 | Saprolith |
| BSMD095A | 13.2 | 13.5 | 0.4 | 4.4 | Saprolith |
| BSMD095A | 13.5 | 14.5 | 0.9 | 3.8 | Saprolith |
| BSMD095A | 14.5 | 15.1 | 0.6 | 3.6 | Saprolith |
| BSMD095A | 15.1 | 16.3 | 1.2 | 4.1 | Saprolith |
| Drill hole ID | From(m) | To(m) | Interval(m) | TGC(%) | Lithology |
| BSMD095A | 16.3 | 17.1 | 0.8 | 2.3 | Saprolith |
| BSMD095A | 17.1 | 18.0 | 0.8 | 1.7 | Saprolith |
| BSMD095A | 18.0 | 18.5 | 0.5 | 4.4 | Saprolith |
| BSMD095A | 18.5 | 19.0 | 0.5 | 2.1 | Saprolith |
| BSMD095A | 19.0 | 19.6 | 0.5 | 0.5 | Saprolith |
| BSMD095A | 19.6 | 20.4 | 0.8 | 6.8 | Saprolith |
| BSMD095A | 20.4 | 20.9 | 0.5 | 10.9 | Saprolith |
| BSMD095A | 20.9 | 21.6 | 0.7 | 11.3 | Saprolith |
| BSMD095A | 21.6 | 22.3 | 0.7 | 10.5 | Saprolith |
| BSMD095A | 22.3 | 23.4 | 1.1 | 7.6 | Saprolith |
| BSMD095A | 23.4 | 24.4 | 1.0 | 13.5 | Saprolith |
| BSMD095A | 24.4 | 25.0 | 0.6 | 8.4 | Saprolith |
| BSMD095A | 25.0 | 25.7 | 0.7 | 5.6 | Saprolith |
| BSMD095A | 25.7 | 26.2 | 0.5 | 5.8 | Saprolith |
| BSMD095A | 26.2 | 26.5 | 0.3 | 0.0 | Saprolith |
| BSMD095A | 26.5 | 27.4 | 0.9 | 0.3 | Saprolith |
| BSMD095A | 27.4 | 28.3 | 0.8 | 0.0 | Dolerite |
| BSMD095A | 28.3 | 29.1 | 0.9 | 0.0 | Dolerite |
| BSMD095A | 29.1 | 29.9 | 0.8 | 0.0 | Dolerite |
| BSMD095A | 29.9 | 30.8 | 0.8 | 0.0 | Dolerite |
| BSMD095A | 30.8 | 31.6 | 0.9 | 0.1 | Dolerite |
| BSMD095A | 31.6 | 32.2 | 0.6 | 6.4 | Saprolith |
| BSMD095A | 32.2 | 33.0 | 0.9 | 5.8 | Saprolith |
| BSMD095A | 33.0 | 33.8 | 0.8 | 4.9 | Saprolith |
| BSMD095A | 33.8 | 34.7 | 0.8 | 4.0 | Saprolith |
| BSMD095A | 34.7 | 35.5 | 0.8 | 3.3 | Saprolith |
| BSMD095A | 35.5 | 37.1 | 1.7 | 4.6 | Saprolith |
| BSMD095A | 37.1 | 38.1 | 0.9 | 6.1 | Saprolith |
| BSMD095A | 38.1 | 39.0 | 0.9 | 6.4 | Saprolith |
| BSMD095A | 39.0 | 40.1 | 1.1 | 6.6 | Saprolith |
| BSMD095A | 40.1 | 40.5 | 0.5 | 6.0 | Saprolith |
| BSMD095A | 40.5 | 41.3 | 0.8 | 6.7 | Saprolith |
| BSMD095A | 41.3 | 42.0 | 0.7 | 4.8 | Saprolith |
| BSMD095A | 42.0 | 42.8 | 0.7 | 4.2 | Graphitic Gneiss |
| BSMD095A | 42.8 | 43.4 | 0.6 | 3.4 | Graphitic Gneiss |
| BSMD095A | 43.4 | 44.0 | 0.7 | 2.9 | Graphitic Gneiss |
| BSMD096 | 5.8 | 6.4 | 0.6 | 0.2 | Saprolith |
| BSMD096 | 6.4 | 7.1 | 0.7 | 1.5 | Saprolith |
| BSMD096 | 7.1 | 7.6 | 0.5 | 3.6 | Saprolith |
| BSMD096 | 7.6 | 8.1 | 0.5 | 3.8 | Saprolith |
| BSMD096 | 8.1 | 8.8 | 0.7 | 3.4 | Saprolith |
| BSMD096 | 8.8 | 9.6 | 0.8 | 1.5 | Saprolith |
| BSMD096 | 9.6 | 10.3 | 0.7 | 2.1 | Saprolith |
| BSMD096 | 10.3 | 11.1 | 0.7 | 0.1 | Saprolith |
| BSMD096 | 11.1 | 12.0 | 0.9 | 1.0 | Saprolith |
| BSMD096 | 12.0 | 12.7 | 0.7 | 0.8 | Saprolith |
| BSMD096 | 12.7 | 13.1 | 0.4 | 0.9 | Saprolith |
| BSMD096 | 13.1 | 14.0 | 0.9 | 1.5 | Saprolith |
| BSMD096 | 14.0 | 14.6 | 0.6 | 0.2 | Dolerite |
| Drill hole ID | From(m) | To(m) | Interval(m) | TGC(%) | Lithology |
| BSMD096 | 14.6 | 15.2 | 0.6 | 1.4 | Saprolith |
| BSMD096 | 15.2 | 15.8 | 0.6 | 1.2 | Dolerite |
| BSMD096 | 15.8 | 17.3 | 1.5 | 0.0 | Dolerite |
| BSMD096 | 17.3 | 19.0 | 1.6 | 0.0 | Dolerite |
| BSMD096 | 19.0 | 19.6 | 0.6 | 3.6 | Saprolith |
| BSMD096 | 19.6 | 20.5 | 0.9 | 3.5 | Saprolith |
| BSMD096 | 20.5 | 21.4 | 0.9 | 1.9 | Saprolith |
| BSMD096 | 21.4 | 22.3 | 0.9 | 2.0 | Saprolith |
| BSMD096 | 22.3 | 23.3 | 1.0 | 4.4 | Graphitic Gneiss |
| BSMD096 | 23.3 | 24.3 | 0.9 | 1.6 | Graphitic Gneiss |
| BSMD096 | 24.3 | 26.2 | 2.0 | 0.0 | Dolerite |
| BSMD096 | 26.2 | 28.0 | 1.8 | 0.0 | Dolerite |
| BSMD096 | 28.0 | 29.7 | 1.8 | 0.5 | Dolerite |
| BSMD096 | 29.7 | 30.2 | 0.5 | 2.6 | Graphitic Gneiss |
| BSMD096 | 30.2 | 30.8 | 0.5 | 3.2 | Graphitic Gneiss |
| BSMD096 | 30.8 | 31.3 | 0.6 | 3.5 | Graphitic Gneiss |
| BSMD097 | 0.0 | 0.8 | 0.8 | 9.6 | Saprolith |
| BSMD097 | 0.8 | 1.3 | 0.5 | 2.8 | Saprolith |
| BSMD097 | 1.3 | 2.0 | 0.8 | 16.1 | Saprolith |
| BSMD097 | 2.0 | 3.5 | 1.5 | 1.4 | Saprolith |
| BSMD097 | 3.5 | 3.7 | 0.2 | 8.0 | Saprolith |
| BSMD097 | 3.7 | 4.3 | 0.6 | 7.1 | Saprolith |
| BSMD097 | 4.3 | 4.7 | 0.4 | 3.8 | Saprolith |
| BSMD097 | 4.7 | 5.4 | 0.7 | 8.2 | Saprolith |
| BSMD097 | 5.4 | 6.3 | 0.8 | 7.1 | Saprolith |
| BSMD097 | 6.3 | 7.2 | 1.0 | 5.4 | Saprolith |
| BSMD097 | 7.2 | 8.3 | 1.0 | 7.4 | Saprolith |
| BSMD097 | 8.3 | 9.4 | 1.1 | 3.2 | Saprolith |
| BSMD097 | 9.4 | 10.4 | 1.0 | 3.8 | Saprolith |
| BSMD097 | 10.4 | 11.0 | 0.7 | 4.2 | Saprolith |
| BSMD097 | 11.0 | 12.0 | 1.0 | 2.3 | Saprolith |
| BSMD097 | 12.0 | 13.6 | 1.6 | 5.0 | Saprolith |
| BSMD097 | 13.6 | 14.2 | 0.7 | 5.5 | Saprolith |
| BSMD097 | 14.2 | 15.0 | 0.8 | 3.6 | Saprolith |
| BSMD097 | 15.0 | 15.9 | 0.9 | 2.8 | Saprolith |
| BSMD097 | 15.9 | 16.6 | 0.7 | 3.2 | Saprolith |
| BSMD097 | 16.6 | 17.5 | 0.9 | 2.1 | Saprolith |
| BSMD097 | 17.5 | 18.5 | 1.0 | 3.6 | Graphitic Gneiss |
| BSMD097 | 18.5 | 19.4 | 0.9 | 2.5 | Graphitic Gneiss |
| BSMD097 | 19.4 | 20.3 | 0.9 | 2.3 | Graphitic Gneiss |
| BSMD097 | 20.3 | 22.5 | 2.2 | 0.0 | Dolerite |
| BSMD097 | 22.5 | 24.3 | 1.8 | 0.0 | Dolerite |
| BSMD097 | 24.3 | 26.6 | 2.3 | 0.0 | Dolerite |
| BSMD097 | 26.6 | 28.2 | 1.6 | 0.0 | Dolerite |
| BSMD097 | 28.2 | 30.1 | 1.9 | 0.0 | Dolerite |
| BSMD097 | 30.1 | 32.0 | 1.9 | 0.0 | Dolerite |
| BSMD097 | 32.0 | 32.6 | 0.7 | 2.8 | Graphitic Gneiss |
| BSMD097 | 32.6 | 33.5 | 0.9 | 2.1 | Graphitic Gneiss |
JORC CODE, 2012 EDITION – TABLE 1
Discussion and results within this appendix relate to Mahefedok Deposit.
Section 1 Sampling Techniques and Data
| Criteria | Commentary |
|---|---|
| Sampling techniques | Diamond drilling was used to obtain NTW size core, with the core split (either manually hand split or sawn using a circular saw) 50:50 to collect samples in 1-metre intervals. Samples were taken along the depth intervals and lithological sub-division mark-ups to gather representative samples. Visual estimation of graphite percentages and flake sizes have been used to define mineralization prior to sampling and assaying. Whole core samples were removed for bulk density testing before splitting and sampling. Upon completion of bulk density measurements, the whole core samples were placed back. Samples were collected within lithological sub-divisions only and not across geological boundaries A total of 34 diamond holes were completed and 1,092 metres were drilled in the northern zone of the Mahafedok deposit. Samples were collected and included composite samples of the graphite bearing host rocks. Visual estimation of graphite percentages and flake sizes have been used to define mineralisation prior to return of assays. The samples were oven dried, crushed to -2mm, split twice through a 50/50 riffle splitter to obtain a representative sub- sample, weighing between 100-150g and then pulverized that 85% pass -75µm. The pulp samples were sent to the Bass Metals in-house laboratory for preliminary Fixed Carbon (FC) analysis and to a SANAS accredited laboratory (SGS) in South Africa for Graphitic Carbon (GC), Total Carbon (TC) and Sulphur (S) analysis. |
| Drilling techniques | Conventional wireline diamond drilling was used to obtain all drill core and drilling was undertaken with an EP200 man portable drilling rig. The nominal core diameter was 56.2 mm (NTW). Coring was completed with appropriate diamond impregnated tungsten carbide drilling bits. Drill holes were inclined at -60 °, direction East and three drill holes were drilled vertical -90 °. The core was not orientated as the material recovered was predominantly soft saprolitic material not conducive to orientation. |
| Drill sample recovery | At the completion of each drill run the steel splits containing the core were pumped out of the retrieved core tube. Core was then carefully transferred from the core barrel into plastic sleeves, which were transferred to core trays for recovery measurements and calculations recorded by both the driller and the Company geologist. Drilling, orientated perpendicular to the orebody, was conducted with specific drilling mud additives to aid drill hole wall integrity, along with slow drilling rates to maximize sample recovery and ensure representative nature of the samples. An overall core recovery of >90% was achieved for all sampled core. One drill hole BSMD095 was re-drilled due to poor core recovery and/or core loss within mineralisation zones. There is no known relationship that exists between sample recovery and grade at this time. Inconsequential sample bias would have occurred due to preferential loss/gain of fine/coarse material. |
| Logging | Drill core were geologically logged, and the recording of relevant data was captured on Bass Metals logging templates. All data was codified to a set company codes system as per sampling and logging procedures, which are in place. This offers sufficient detail for the purposes of geological interpretation, further studies and resource estimation where continuity of the orebody needs to be proved and understood. All logging included lithological features, estimates of graphite percentages and flake sizes, which is quantitative and is recorded on the logging sheets. All drill core was photographed prior to geological logging and after sampling and images were digitally catalogued. Photographs have been taken as a qualitative check on logging when the need arises. All drill core intersections (100%) were logged by experienced, competent geoscientists are considered to be reliable and reproducible semi-quantitative estimates of the abundance of minerals present in samples when referenced to past drilling assay data and current mining operations undertaken by the Company in the same style of mineralisation. |
| Sub-sampling techniques and sample preparation |
The NTW core was manually hand split and where appropriate sawn to produce half core (50:50) samples. All equipment was cleaned according to best practise procedures prior to cutting and sampling. Appropriate and documented techniques were used to collect samples in 1-metre intervals. Samples were taken along the depth intervals and lithological sub-division mark-ups to gather representative samples. The samples were oven dried, crushed to -2mm, split twice through a 50/50 riffle splitter to obtain a representative sub-sample, weighing between 100-150g and then pulverized that 85% pass -75µm. The pulp samples were sent to the Bass Metals in- house laboratory for preliminary Fixed Carbon (FC) analysis and to a SANAS accredited laboratory (SGS) in South Africa for Graphitic Carbon (GC), Total Carbon (TC) and Sulphur (S) analysis. Certified graphite standards (GC-09 and GC-11) and silica blanks (AMIS0484 and AMIS0439) and duplicates (a second sample of the same interval) were inserted with the dispatch of the samples to the SANAS accredited laboratory (SGS) in South Africa. The insertion rate of standards/blanks were 1 in 20, and duplicates were 2 in 100. The SANAS Laboratory will insert check samples (blanks, standards and duplicates) to maintain QAQC standards. |
| Quality of assay data and laboratory tests |
Samples were analysed at the Bass Metals in-house laboratory for a preliminary evaluation of the carbon grade. The Muffle Furnace method was used to determine Loss on Ignition (LoI), Volatile Matter (VM) and Fixed Carbon (FC). LoI Test: a crucible is placed on an electronic balance, primarily zeroed and the weight recorded. 1 gram +- 0.01 of the sample are added, the weight of crucible + sample are recorded. The crucible is placed in the Muffle Furnace at 950°C +-25°C for 8 hours continuously. After the crucible is removed and cooled, the ash + crucible is then weighed and recorded. The LoI % is calculated as follows: LOI % = (1 - ) × 100 VM Test: a crucible is placed on an electronic balance, primarily zeroed and the weight recorded. 2 grams +- 0.01 of the sample are added, the weight of crucible + sample are recorded. The crucible is placed in the Muffle Furnace at 950°C +- 25°C for 7 minutes. After the crucible is removed and cooled, the ash + crucible is then weighed and recorded. The VM % is calculated as follows: V M % = (1 - ) × 100 The FC % of the sample is calculated as follows: FC % = (LOI % - VM %) |
| Analysis by the SANAS Accredited Laboratory (SGS) in South Africa may include sub- sample preparation included sorting and pulverizing such that 80% of the sample is -75 micron or less in size. A split of the sub-sample will be analysed using a LECO Analyser to determine Total Carbon (TC), Sulphur (S) and Graphitic Carbon (GC) contents (these are considered both partial and total digestion analyses). For TC and S, a stream of oxygen passes through a prepared sample (2g), it is heated in a furnace to approximately 1350°C and the sulphur dioxide and carbon dioxide released from the sample are measured with infrared detection. For GC, a 0.2g sample is leached with dilute hydrochloric acid to remove inorganic carbon. After filtering, washing and drying, the remaining sample residue is roasted at 425°C to remove organic carbon. The roasted residue is analysed for Carbon - High temperature LECO furnace with infra-red detection. Internal Laboratory check samples (blanks, standards and duplicates) are also analysed as per normal laboratory practice. All in-house and laboratory standards, blanks and duplicate results were reviewed. Performance of the accredited laboratory (SGS) across all assay batches were within acceptable tolerance levels. |
|
| Verification of sampling and assaying |
All work was completed by Bass Metals personnel. Significant mineralization intersections were verified by an external consultant and by internal peer review. No twinned holes were drilled. All data was collected initially on paper log sheets by Bass Metals personnel. This data was hand entered into spreadsheets and validated by an external consultant. All paper log sheets were scanned, and electronic spreadsheets stored together with the photographs of the geological features logged. The master collar, geotechnical, density, lithology and assay database with all photographs are backed-up and stored on an external hard drive. No adjustments were made to the data. |
| Location of data points | DGPS’s were used to locate collar locations, and final location coordinates were completed with estimated positional errors between 15 and 30 centimetres. The WGS84 UTM Zone 39S projection system is used at the Mahafedok Project. |
| Data spacing and distribution |
Collars were spaced along a 50m north orientated grid, with drill hole inclination and strike aligned perpendicular to the orebody orientation. 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. Sample compositing has not been applied. |
| Orientation of data in relation to geological structure |
Drilling was approx. orientated perpendicular to the estimated dip and strike of the mineralization to limit bias. Drill holes were inclined at -60 °, direction East and three drill holes were drilled vertical -90 °. Subsequent samples are deemed to be unbiased in terms of known structures and the deposit type. |
| Sample security | Samples were stored in a secure storage area at the Bass Metals sample storage facility. Samples bags were sealed as soon as sampling was completed and stored securely until dispatch to the preparation laboratory in Antananarivo and after to the laboratory (SGS) in South Africa via courier. |
| Audits or reviews | The sampling techniques and data were reviewed by an external consultant and internally peer reviewed. It is considered by the Company that industry best practice methods have been implemented by the Company at all stages of exploration. |
Section 2 Reporting of Exploration Results
Criteria listed in the preceding section also applies to this section.
| Criteria | Commentary |
|---|---|
| Mineral tenement and land tenure status |
Exploitation permit no PE 26670 is located in the Toamasina Province of Madagascar and held by the Malagasy company, Graphmada SARL which is a wholly owned subsidiary of the ASX listed company, Bass Metals Ltd. Permit no PE 26670 was granted on 21/01/2008and is valid for 40 years. The permit is in good standing, and all statuary approvals are in place to conduct exploration and exploitation activities throughout this permit area, including mining. |
| Exploration done by other parties |
Mahefedok – Prior to the Company’s ownership, Graphmada SARL excavated 4 pits in the northern part of the Mahefedok Deposit in 2013, which revealed significant regolith-hosted graphite mineralization at depth. These pits were excavated over a north-south distance (and along strike of the Mahefedok Orebody) of approx. 70 meters and Graphmada’s in-house laboratory analysis of the pit samples returned up to 3 m @ 7.04 % Total Carbon (TC). In 2015, Stratmin Global Resources PLC, through its subsidiary Graphmada SARL, collected 34 outcrop samples over PE 26670. Also, in 2015 ground magnetic, self- potential, induced polarization and electric resistivity surveys were completed and 75 pits (up to depths of 5.9m) and 6 trenches (up to depths of 6.0m) were excavated over the Mahefedok Deposit. For the ground magnetic survey, a Geotron G5 magnetometer was used and readings were recorded every 10 m in nanotesla (nT). A base station was set-up using a second Geotron G5 magnetometer and readings were recorded every 30 seconds in nT. Diurnal drift corrections were completed using Geotron Dump G5 software. The corrected ground magnetic data were processed (including, gridding, filtering, and contouring) using Encom DiscoverTM (v12) software. The processing methodology involved gridding the diurnally corrected data using the Inverse Distance Weighting (IDW2) interpolation algorithm (to the power of 2), a search distance of 200 m and a spatial resolution / cell size of 5 m. Filtering involved the application of a 3x3 cell averaging filter and contouring was at an interval of 25 m. For the ground self-potential (SP) survey a pair of non-polarising electrodes (e.g. IRIS copper-sulphate pots), a reel of insulated wire and a high impedance voltmeter were used. Procedures for SP surveys involved a series of parallel lines orientated perpendicular to the strike direction of the anticipated mineralization and spaced to suit the required resolution. For the Mahefedok surveys, line and station spacing was 10 m and the surveys were conducted using the fixed-base procedure. Data at each station included the distance from line base (m), normal voltage (mV), resistance (Kilohms), and base revolving pot drift voltage (mV). To obtain the absolute voltage of a station relative to the survey base there were two corrections: the drift correction, and the base tie-in correction. The absolute voltage for any other station on a line was determined by adding the normal voltage at that station to the appropriate drift and tie-in corrections. The corrected SP data were processed using Geosoft Oasis Montaj software and involved using the Kriging technique with a grid size of 20 m. For the ground induced polarization (IP) and electric resistivity (ERT) surveys an IRIS SYSCAL R2 Resistivity and IP system, consisting of multinodes, a battery, 32 stainless- steel electrodes, and electrode reel wires were used. Procedures for IP/ERT surveys involve a series of lines over identified SP anomalies. For the Mahefedok surveys, lines were approx. 150 m in length and station spacing of 5 m. The surveys were conducted using a time domain Wenner / Schlumberger sequence array with a depth penetration of approx. 25 m. All measurements (chargeability and resistivity) were recorded automatically after uploading the sequence array using the IRIS ELECTRE software, and all data was downloaded after the survey using the IRIS PROSYS software. The resistivity of the sub-surface was calculated (in ohm), and the IP response was also recorded, and the chargeability calculated (in milliseconds). Processing was done using the GEOTOMO |
| RES2DINV software, and the program used the smoothness-constrained Gauss-Newton least-squares inversion technique to produce an inverted depth-section of the subsurface from the apparent electrical chargeability and resistivity data. The results of the programs delineated at least three anomalies over a strike distance of approx. 1.6 km for follow up drilling. In 2016, a trial pit at Mahefedok was mined to provide a bulk sample to the existing Graphmada processing plant. Approx. 8,751 tonnes of mined material were processed and produced approx. 135 tonnes of graphite, with graphite purities varying between 78.14 and 89.89 % (corresponding to an average of 83.52 %). Flake size distribution testing completed on the graphite produced yielded the following flake sizes: 21.95 % jumbo (+50 mesh / >300 microns); 28.18 % large (+80 mesh / 180-300 microns); 17.84 % medium (+100 mesh / 150-180 microns) and 31.19 % fine (-100 mesh / <150 microns). The Company is currently mining the Mahefedok North Pit having estimated a Maiden Mineral Resource of 3.5 Mt at 4.2% Total Graphitic Carbon (TGC) in June 2017. |
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| Geology | Crystalline “hard rock” flake graphite deposits occur in graphitic gneisses within Neoproterozoic metasedimentary type rocks and include accessory minerals of biotite (± sillimanite / kyanite, ± garnet). Due to the tropical climate and because graphite is comparatively inert, weathering of the “hard rock” graphitic gneiss units further concentrate the graphite to form residual regolith-hosted accumulations within the weathered profile. Regolith refers to weathered material that occurs above unweathered bedrock. Two primary subdivisions are the pedolith (PED) and the saprolith (SAP). Secondary subdivisions of the pedolith, from the surface downwards, include soil (SL), ferruginous zone (FZ), and the mottled zone (MZ). Secondary subdivisions of the saprolith, include saprolite (SP) and saprock (SR). The Mahafedok deposit contains 3 broad north-south striking graphite mineralisation zones; the northern zone has a strike length of approximately 500 m, the centre zone approximately 850 m, and the southern zone approximately 300 m for a cumulative strike of approximately 1,650 m. The deposit dips to the west at between 30° and 45°. It consists up to seven lenses in the northern and central zones of the deposit, and three in the southern zone. Individual lenses are nominally between 2 m and 14 m in true thickness. The Mahela Project contains at least 3 lenticular bodies of flake graphite within the weathered profile described above. The 3 parallel striking graphitic units strike approx. northwest - southeast and is open ended in to the north and south. |
| Drill hole Information | A summary of all information material to the understanding of the exploration results including a tabulation of visually logged data is supplied in the above announcement. |
| Data aggregation methods |
Samples has been reported as in-situ Total Graphitic Carbon (TGC) grades as analysed by the SANAS accredited (SGS) laboratory in South Africa. No Metal Equivalents have been stated. |
| Relationship between mineralisation widths and intercept lengths |
The mineralization is hosted within a weathered regolith profile and the main mineralized lenses / horizons dip towards the west at between 30° and 45°. Only the down hole lengths are reported - true width has not been estimated and tables have been annotated in the above announcement. |
| Diagrams | This information has been accurately represented in the announcement and contains all relevant information required for the reader to understand the nature of the graphitic mineralization. |
| Balanced reporting | The Company believes visual inspections of a fully complete drilling program by experienced, competent geoscientists are considered to be reliable and reproducible semi- quantitative estimates of the abundance of minerals present in samples when referenced to past drilling assay data and current mining operations undertaken by the Company in the same style of mineralisation. As such, the circumstances warrant that the Company complies with the ASX Listing Rules mandate that appropriate disclosure of these drilling results is made and confirms that the results were not derived solely from a visual inspection of core samples alone. |
| The Company has stated the samples are yet to be assayed and analysed and has made | |||
| no comments about the grade or quality of the mineralisation in the absence of any assay | |||
| data and has outlined the timing of full assay results and the preliminary nature of the | |||
| inspection within the announcement. | |||
| Other substantive | Previous exploration by the Company has demonstrated widespread mineralization at | ||
| exploration data | Mahela and Mahefedok, with mining now underway at Mahefedok. | ||
| Please reference ASX releases: | |||
| 11/06/19 ‘Diamond drilling commences at Mahela prospect.’ | |||
| 03/06/19 ‘Significant Exploration Program to commence at Graphmada.’ | |||
| 09/04/19 ‘Bass progresses exploration at Graphmada Graphite Mine.’ | |||
| 14/12/19 ‘Bass completes Capital Raising for Expansion and Drilling.’ | |||
| Further work | Further exploration will be planned for both deposits, in addition to further work in | ||
| estimating flake size distribution and metallurgical testing. | |||
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