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Pure Minerals Ltd.
Summary
| Project: | Battery Hub | |
|---|---|---|
| Deposit: | Julia | |
| Location: | Australia | |
| Commodities: | Manganese | |
| Date: | 1/11/2018 | |
| Report Code: | JORC | |
| Report Type: | Exploration/Drilling Update | |
| Project Stage: | Active Mining & Production | |
| Report details: | 11-1-2018: Pure Minerals Ltd. announces an Exploration/Drilling Update report for its Julia deposit at the Battery Hub project. Drilling results incl. 9m @ 14.85% Mn from 0m. Pure Minerals Limited (ASX: PM1) (“Pure Minerals”, “the Company”) is pleased to | |
| Resources: | (not mentioned in this report) | |
| CP/QP: | [Overall Report]: Kell Nielsen (Mannika Resources Group Pty Ltd.) | |
| ABSTRACT: | Pure Minerals Limited (ASX: PM1) (“Pure Minerals”, “the Company”) is pleased to announce initial drill results from its first phase of drilling at its 100%-owned Battery Hub manganese project, located in Western Australia’s Gascoyne region. The initial results come from 42 drill holes located at the Julia Prospect, located at the eastern end of tenement E09/2217 (Figure 1, below). Prior to drilling, Pure Minerals identified the Julia area to have shallow bulk tonnage potential and the recently completed drill program has successfully highlighted this potential. Key statistical highlights of the drilling Moreover, the drill program has been successful in classifying different zones of shallow mineralisation at Julia over an approximate 2,500m strike length, including weathered lateritic mineralisation, together with higher-grade cap-rock mineralisation, and thick stratiform manganese mineralisation within the host siltstone formation. Lateritic mineralisation is represented by nodular manganese mineralisation hosted within recemented manganese nodules near surface (“cap rock”) and at the base of a thick weathering horizon of saprolite clay. Cap rock mineralisation represents a relatively thin Mineralisation at the base of the laterite often dips shallowly to the NNE along a paleaogeographic weathering surface similar to the ridge lines observed in the area. A relatively high level of grade and geological continuity is observed. Key intercepts in this laterite mineralisation | |
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