| Abstract: | Attempts to understand better the nature and possible source of the mineralizing solutions for both vertical and gash veins and the possible origin of the lead and zinc mineralization. Large deposits of essentially syngenetic sphalerite with minor to trace galena occur in the Proterozoic rocks of the region (eg Balmat-Edwards, New York). Although none of these deposits are known in the immediate vicinity of Rossie veins, the possibility that Rossie veins contain remobilized metals from these older deposits was considered.-from Authors |
| Genre: | Article |
| ProdID: | 70014098 |
| Citation Author: | Ayuso, R. A.; Foley, N. K.; Brown, C. E. |
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| Citation End Page: | 491 |
| Citation Issue: | 2 |
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| Citation Language: | English |
| Citation Larger Work Title: | Economic Geology |
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| Citation Number Of Pages: | 3 |
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| Citation Search Results Text: | Source of lead and mineralizing brines for rossie-type Pb-Zn veins in the Frontenac axis area, New York ( USA).; 1987; Article; Journal; Economic Geology; Ayuso, R. A.; Foley, N. K.; Brown, C. E. |
| Citation Start Page: | 489 |
| Citation Volume: | 82 |
| Citation Year: | 1987 |
| Type: | citation/reference |
| Text: | Source of lead and mineralizing brines for rossie-type Pb-Zn veins in the Frontenac axis area, New York ( USA).; 1987; Article; Journal; Economic Geology; Ayuso, R. A.; Foley, N. K.; Brown, C. E. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Thu, 1 Jan 1987 00:00 -0600 |
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