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Tri Origin Exploration Ltd.
Summary
| Project: | North Abitibi | |
|---|---|---|
| Deposit: | North Abitibi | |
| Location: | Canada | |
| Commodities: | Gold | |
| Date: | 11/6/2018 | |
| Report Code: | NI43-101 | |
| Report Type: | Exploration/Drilling Update | |
| Project Stage: | Pursuing Resources Definition | |
| Report details: | 6-11-2018: Tri Origin Exploration Ltd. announces an Exploration/Drilling Update report for its North Abitibi deposit at the North Abitibi project. Drilling results incl. 1m @ 1250ppb Au. Aurora, Ontario- Tri Origin Exploration Ltd. (TSX-V: TOE) (“Tri Orig | |
| Resources: | x | |
| CP/QP: | [Overall Report]: n/a (n/a) | |
| ABSTRACT: | Aurora, Ontario- Tri Origin Exploration Ltd. (TSX-V: TOE) (“Tri Origin” or the “Company”) is nearing completion of a program of diamond drilling at its North Abitibi gold property located 150 kilometres north of Kirkland Lake and 40 kilometres west of the Casa Berardi Gold Mine in the Abitibi Greenstone Belt of Ontario. A total of 3 holes for approximately 1,380 metres of drilling were completed. Drill holes were very widely-spaced and difficulties were encountered with access to drill sites due to peat bog and swampy conditions. Consequently, the program was terminated early prior to evaluating all of the selected targets. Evaluation of primary targets at the Spade Lake and other gold zones on the property will be deferred until after ground has frozen or during drier summer periods. Two holes were completed along trend from the Road Gold Zone which was previously exposed in surface excavations completed by Tri Origin. The first was located approximately 200 metres west of the centre of the surface excavations and the second was approximately 200 metres east of the excavations. The westernmost hole intersected a 5 metre thick pyritic and sericite-altered zone at 339.5 metres downhole near the contact between iron-carbonate altered mafic rock and felsic volcanic rock. The easternmost hole contained a 2.5 metre interval of pyritic rock at 282.5 metres downhole and a volcanic breccia contained 1 to 10 centimetre scale massive pyrite fragments between 317 and 323 metres downhole. The pyrite fragments in the breccia indicate that a primary massive sulphide body may have been disrupted by an ancient volcanic event or subsequent structural deformation. The source of the massive sulphide body is unknown but it comprises a prime exploration target. | |
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