| Article ID | Journal | Published Year | Pages | File Type | 
|---|---|---|---|---|
| 4717600 | Lithos | 2008 | 17 Pages | 
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
												
											Authors
												Gabriel Carlier, Jean-Pierre Lorand, 
											