Article ID Journal Published Year Pages File Type
4717600 Lithos 2008 17 Pages PDF
Abstract

The Oroscocha Quaternary volcano, in the Inner Arc Domain of the Andean Cordillera (southern Peru), emitted peraluminous rhyolites and trachydacites that entrained decimetric to millimetric lamprophyric blobs. These latter show kersantite modal compositions (equal proportion of groundmass plagioclase and K-feldspar) and potassic bulk-rock compositions (1

Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
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