| Abstract: | The compositionally bimodal Pleistocene Coso volcanic field is located at the western margin of the Basin and Range province ~ 60 km north of the Garlock fault. Thirty-nine nearly aphyric high-silica rhyolite domes were emplaced in the past million years: one at 1 Ma from a transient magma reservoir, one at ~ 0.6 Ma, and the rest since ~ 0.3 Ma. Over the past 0.6 My, the depth from which the rhyolites erupted has decreased and their temperatures have become slightly higher. Pre-eruptive conditions of the rhyolite magmas, calculated from phenocryst compositions using the two-oxide thermometer and the Al-in-hornblende barometer, ranged from 740??C and 270 MPa (2.7 kbar; ~ 10 km depth) for the ~ 0.6 Ma magma, to 770??C and 140 MPa (1.4 kbar; ~ 5.5 km) for the youngest (~ 0.04 Ma) magma. Results are consistent with either a single rhyolitic reservoir moving upward through the crust, or a series of successively shallower reservoirs. As the reservoir has become closer to the surface, eruptions have become both more frequent and more voluminous. |
| Genre: | Article |
| ProdID: | 70023226 |
| Citation Author: | Manley, C. R.; Bacon, C. R. |
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| Citation End Page: | 174 |
| Citation Issue: | 1 |
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| Citation Language: | English |
| Citation Larger Work Title: | Journal of Petrology |
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| Citation Number Of Pages: | 26 |
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| Citation Search Results Text: | Rhyolite thermobarometry and the shallowing of the magma reservoir, Coso volcanic field, California; 2000; Article; Journal; Journal of Petrology; Manley, C. R.; Bacon, C. R. |
| Citation Start Page: | 149 |
| Citation Volume: | 41 |
| Citation Year: | 2000 |
| Type: | citation/reference |
| Text: | Rhyolite thermobarometry and the shallowing of the magma reservoir, Coso volcanic field, California; 2000; Article; Journal; Journal of Petrology; Manley, C. R.; Bacon, C. R. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Sat, 1 Jan 2000 00:00 -0600 |
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