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Volumn 184, Issue 1-2, 2009, Pages 79-92

Evidence for a homogeneous primary magma at Piton de la Fournaise (La Réunion): A geochemical study of matrix glass, melt inclusions and Pélé's hairs of the 1998-2008 eruptive activity

Author keywords

basalt glass; cumulates; hotspot; La R union Island; melt inclusion; P l 's hair

Indexed keywords

BASALT GLASS; BASALTIC MAGMA; BASALTIC MELTS; CHEMICAL HOMOGENEITY; CLOSED SYSTEMS; COMPOSITION RANGES; CRYSTAL FRACTIONATION; CRYSTALLISATION; CUMULATES; DENSE BODIES; DIFFERENTIATION PROCESS; ERUPTIVE ACTIVITY; GLASS COMPOSITIONS; HIGH TEMPERATURE; HOTSPOT; LOW PRESSURES; LOW-AMPLITUDE; MAJOR AND TRACE ELEMENTS; MATRIX; MELT COMPOSITIONS; MELT INCLUSION; MELT INCLUSIONS; MINERAL COMPOSITION; OLIVINE CRYSTALS; PITON DE LA FOURNAISE VOLCANO; ROCK INTERACTION; SEISMIC TOMOGRAPHY; TRANSFER PATHS; VOLCANIC ACTIVITIES;

EID: 67349252743     PISSN: 03770273     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jvolgeores.2009.03.015     Document Type: Article
Times cited : (34)

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