Adakitic Dacites Formed by Intracrustal Crystal Fractionation of Water-rich Parent Magmas at Nevado de Longaví Volcano (36·2°S; Andean Southern Volcanic Zone, Central Chile)
The mid-Holocene eruptive products of Nevado de Longaví volcano (36·2°S, Chile) are the only reported occurrence of adakitic volcanic rocks in the Quaternary Andean Southern Volcanic Zone (33–46°S). Dacites of this volcano are chemically distinct from other evolved magmas of the region in that they...
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Veröffentlicht in: | Journal of petrology 2007-11, Vol.48 (11), p.2033-2061 |
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