| Abstract: | Plagioclases in the 1974 high-Al basalt from Fuego Volcano have ??O18 values of +6.0 to +8.5 per mil. Meteoric water cannot have played a significant role in Fuego‘s magma. Large, weakly zone clear phenocrysts had ??O18 values in the accepted mantle range, while patchyzoned and oscillatory-zoned plagioclases inferred to have formed later and shallower levels have slightly heavier oxygen isotopic ratios. ?? 1980 Intern. Association of Volcanology and Chemistry of the Earth‘s Interior. |
| Genre: | Article |
| ProdID: | 70000704 |
| Citation Author: | Rose, Jr. , W. I.; Friedman, I.; Woodruff, L. G. |
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| Citation End Page: | 194 |
| Citation Issue: | 1 |
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| Citation Language: | English |
| Citation Larger Work Title: | Bulletin Volcanologique |
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| Citation Publisher: | Springer-Verlag |
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| Citation Search Results Text: | Oxygen isotopic determinations of sequentially erupted plagioclases in the 1974 magma of Fuego Volcano, Guatemala; 1980; Article; Journal; Bulletin Volcanologique; Rose, Jr. , W. I.; Friedman, I.; Woodruff, L. G. |
| Citation Start Page: | 191 |
| Citation Volume: | 43 |
| Citation Year: | 1980 |
| Type: | citation/reference |
| Text: | Oxygen isotopic determinations of sequentially erupted plagioclases in the 1974 magma of Fuego Volcano, Guatemala; 1980; Article; Journal; Bulletin Volcanologique; Rose, Jr. , W. I.; Friedman, I.; Woodruff, L. G. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| URL (DIGITAL OBJECT IDENTIFIER): | http://dx.doi.org/10.1007/BF02597620 |
| Date Other: | Tue, 28 Sep 2010 23:09 -0500 |
| Publisher: | Springer-Verlag |
