The Stillwater Complex, Montana; a subvolcanic magma chamber?
The observed stratigraphy of the basal and ultramafic series may result from mixing of two distinct magmas rather than fractionation of a single magma.
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Veröffentlicht in: | The American mineralogist 1995-12, Vol.80 (11-12), p.1343-1346 |
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Format: | Artikel |
Sprache: | eng |
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Online-Zugang: | Volltext |
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Zusammenfassung: | The observed stratigraphy of the basal and ultramafic series may result from mixing of two distinct magmas rather than fractionation of a single magma. |
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ISSN: | 0003-004X 1945-3027 |
DOI: | 10.2138/am-1995-11-1225 |