| Abstract: | Metamorphic zonation overprinted on the volcanic member and overlying volcanogenic sediments of the ophiolite complex increases downward in grade and is characterized by the sequential appearance with depth of zeolites, ferric pumpellyite and pistacitic epidote. Metamorphic assemblages of the plutonic member of the complex are characterized by the presence of calcic amphibole. The overprinting represents the effects of hydrothermal metamorphism resulting from the massive interaction between hot igneous rocks and convecting sea-water in a submarine environment. A thermal gradient of 100oC/km is postulated to account for the zonal recrystallization effects in the volcanic member. The diversity and sporadic distribution of mineral assemblages in the amphibole zone are considered due to the limited availability of H2O in the deeper part of the complex. Details of the zonation and representative microprobe analyses are tabulated.-M.S. |
| Genre: | Article |
| ProdID: | 70011348 |
| Citation Author: | Evarts, R. C.; Schiffman, P. |
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| Citation End Page: | 340 |
| Citation Issue: | 4 |
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| Citation Language: | English |
| Citation Larger Work Title: | American Journal of Science |
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| Citation Number Of Pages: | 52 |
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| Citation Search Results Text: | Submarine hydrothermal metamorphism of the Del Puerto ophiolite, California.; 1983; Article; Journal; American Journal of Science; Evarts, R. C.; Schiffman, P. |
| Citation Start Page: | 289 |
| Citation Volume: | 283 |
| Citation Year: | 1983 |
| Type: | citation/reference |
| Text: | Submarine hydrothermal metamorphism of the Del Puerto ophiolite, California.; 1983; Article; Journal; American Journal of Science; Evarts, R. C.; Schiffman, P. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Sat, 1 Jan 1983 00:00 -0600 |
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