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Bryah Resources Ltd.
Summary
| Project: | Gabanintha | |
|---|---|---|
| Deposit: | Tumblegum South | |
| Location: | Australia | |
| Commodities: | Gold | |
| Date: | 1/12/2018 | |
| Report Code: | JORC | |
| Report Type: | Exploration/Drilling Update | |
| Project Stage: | Pursuing Resources Definition | |
| Report details: | 12-1-2018: Bryah Resources Ltd. announces an Exploration/Drilling Update report for its Tumblegum South deposit at the Gabanintha project. Drilling results incl. 3m @ 23.8g/t Au, 0.32% Cu from 45m. Bryah Resources Limited (“Bryah” or “the Company”) is pl | |
| Resources: | x | |
| CP/QP: | [Overall Report]: Rohan Williams (Internal) | |
| ABSTRACT: | Bryah Resources Limited (“Bryah” or “the Company”) is pleased to announce significant gold mineralisation in the initial results from its maiden drilling programme at the Tumblegum South Gold/Copper Prospect, located within the Gabanintha Project in central Western Australia. The Gabanintha Project is located approximately 40km south of Meekatharra (see Figure 1). A total of 26 RC drill holes for 2,484 metres were completed in this drilling programme. Samples were collected at 1 metre intervals and composited to 3 metre intervals for initial analysis for gold and multi-elements. A full schedule of significant laboratory results is shown in Table 2 with selected results shown on Figure 2 below and in cross sections in Figures 3 - 5. The results reported are based upon 3 metre composites. Composite intervals where over 0.1 g/t Au has been reported will be re-analysed using the individual 1 metre riffle split samples to confirm grades and widths of mineralised intervals. The relevant 1 metre samples will be collected from storage and submitted to the laboratory in the coming weeks. The lithologies intersected were typical of Archaean greenstone rock-types and consisted primarily of mafic and ultramafic volcanics and intrusives of both komatiitic and tholeiitic affinities. These have been overlain by jaspilitic banded iron formations (BIF) and epiclastic sediments. At Gabanintha the komatiitic rocks have been selectively deformed by a regionally extensive NNW to N trending transcurrent shear zone, named the Gabanintha Shear. | |
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