Detailed Summary Report
Assessment Report: 10021
| Property Name |
Carpenter 10021.pdf |
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| Location |
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| Mining Divisions | Skeena | ||||||||||||
| Mining Camp | |||||||||||||
| Title | Geochemical and Geological Report on the Carpenter 1-2 Claims, Skeena Mining Division | ||||||||||||
| Report Year | 1981 | ||||||||||||
| Number of Pages | 18 | ||||||||||||
| Statements of Work | n/a | ||||||||||||
| Affidavit Date | 1981-11-26 | ||||||||||||
| Off Confidential | 1982-11-26 | ||||||||||||
| Claims | CARPENTER | ||||||||||||
| General Work Categories | Geochemical, Geological | ||||||||||||
| Operators |
Ventures West Minerals |
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| Owners | |||||||||||||
| Authors |
Christie, James S. Howell, William A. |
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| MINFILE Nos | |||||||||||||
| Commodities | |||||||||||||
| Work Done |
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| Keywords | |||||||||||||
| Related Report(s) | |||||||||||||
| File(s) |
10021.pdf |
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| Geological Summary |
Kunga Formation (Triassic-Jurassic) limy argillite is intruded by quartz monzonite. The argillite is strongly folded and faulted and cut by a swarm of andesite and minor felsite dykes. Iron sulphide mineralization is prominent.
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