Oxygen isotopic determinations of sequentially erupted plagioclases in the 1974 magma of Fuego Volcano, Guatemala
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.
Citation Information
Publication Year | 1980 |
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Title | Oxygen isotopic determinations of sequentially erupted plagioclases in the 1974 magma of Fuego Volcano, Guatemala |
DOI | 10.1007/BF02597620 |
Authors | W.I. Rose, I. Friedman, L. G. Woodruff |
Publication Type | Article |
Publication Subtype | Journal Article |
Series Title | Bulletin Volcanologique |
Index ID | 70000704 |
Record Source | USGS Publications Warehouse |