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Core Lithium Ltd.
Summary
| Project: | Finniss | |
|---|---|---|
| Deposit: | BP33 | |
| Location: | Australia | |
| Commodities: | Lithium | |
| Date: | 8/22/2018 | |
| Report Code: | JORC | |
| Report Type: | Exploration/Drilling Update | |
| Project Stage: | Pursuing Pre-Feasibility Study | |
| Report details: | 22-8-2018: Core Lithium Ltd. announces an Exploration/Drilling Update report for its BP33 deposit at the Finniss project. Drilling results incl. 63m @ 1.50% Li2O from 76m. Emerging Australian lithium developer, Core Exploration Ltd (ASX: CXO) (“Core” or t | |
| Resources: | (not mentioned in this report) | |
| CP/QP: | [Overall Report]: Steven Biggins (Internal) | |
| ABSTRACT: | Emerging Australian lithium developer, Core Exploration Ltd (ASX: CXO) (“Core” or the “Company”), is pleased to announce several new high-grade intersections returned from the current RC drilling program designed to grow the existing resource base at the BP33 Prospect within Core’s 100%-owned Finniss Lithium Project near Darwin in the Northern Territory. Core’s most recent phase of drilling has focused on the potential southern extension of the current resource and infill at BP33 and has achieved a number of outstanding intersections including. The current extensional drilling at BP33 will be incorporated into a new Mineral Resource estimate in the coming months and is expected to have a positive impact on estimates. Similarly, new drilling positioned within the currently defined Resource at BP33 is expected to enable an upgrade in the classification of the BP33 Mineral Resource to higher confidence categories (Figures 1 and 2). The drilling demonstrated that BP33 continues and appears to increase in width and grade at depth immediately south of the current Resource area. In the very south of the deposit, drill intersections of pegmatite tend to become broken up by intervals of host rock, so it would appear that the pegmatite changes from a coherent tabular body to a segmented series of narrower sheets, dipping at between 75 and 45 degrees to the east. Holes in the far south that were testing for continuation in that direction showed that indeed it continues but is thinner and less mineralised (Figures 1 and 2). | |
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