| Abstract: | The Brick Flat massive sulfide body is one of a group of 8 individual bodies that constitute the Iron Mountain cluster in the S part of the West Shasta district. Before they were separated by postmineral faulting, 5 of the 8 sulfide bodies formed a single large deposit about 1375 m long with a mass of some 23 million metric tons. The pyritic Brick Flat sulfide body is one of the 5 faulted segements of this deposit. The Brick Flat massive sulfide lies within medium phenocryst rhyolite that is characteristic of the ore-bearing middle unit of the Balaklala Rhyolite. It is interpreted to be downfaulted a vertical distance of 75 to 85 m from the Old Mine sulfide-gossan orebody along the N-dipping Camden South fault. It is bounded in turn on its N side by another parallel fault, the Camden North, which drops the orebody down another 75 m to the level of the Richmond orebody. -from Author |
| Genre: | Article |
| ProdID: | 70013026 |
| Citation Author: | Albers, J. P. |
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| Citation End Page: | 2099 |
| Citation Issue: | 8 |
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| Citation Language: | English |
| Citation Larger Work Title: | Economic Geology |
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| Citation Number Of Pages: | 8 |
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| Citation Search Results Text: | Geology of the Brick Flat massive sulfide body, Iron Mountain cluster, West Shasta district, California ( USA).; 1985; Article; Journal; Economic Geology; Albers, J. P. |
| Citation Start Page: | 2092 |
| Citation Volume: | 80 |
| Citation Year: | 1985 |
| Type: | citation/reference |
| Text: | Geology of the Brick Flat massive sulfide body, Iron Mountain cluster, West Shasta district, California ( USA).; 1985; Article; Journal; Economic Geology; Albers, J. P. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Tue, 1 Jan 1985 00:00 -0600 |
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