Three differentiation stages of a single magma at Piton de la Fournaise volcano (Reunion hot spot)-Reference-Cited by-同舟云学术

Three differentiation stages of a single magma at Piton de la Fournaise volcano (Reunion hot spot)

Published:2009-01 Issue:1 Volume:10 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Famin Vincent¹,Welsch Benoît¹,Okumura Satoshi²,Bachèlery Patrick¹,Nakashima Satoru³

Affiliation:

1. Laboratoire Géosciences Réunion; Institut de Physique du Globe de Paris, Université de la Réunion; UMR 7154, CNRS, 15 avenue René Cassin,; F-97715; Saint Denis messag CEDEX 9, La Réunion; France

2. Department of Earth and Planetary Materials Science, Graduate School of Science; Tohoku University; Sendai; 980-8578; Japan

3. Department of Earth and Space Science, Graduate School of Science; Osaka University; 1-1 Machikaneyama-cho,; Osaka; 560-0043; Japan

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference61 articles.

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2. The geochemical regimes of Piton de la Fournaise Volcano (Réunion) during the last 530,000 years;Albarède;J. Petrol.,1997

3. Algorithmic modifications extending MELTS to calculate subsolidus phase relations;Asimow;Am. Mineral.,1998

4. The range of spinel compositions in terrestrial mafic and ultramafic rocks;Barnes;J. Petrol.,2001

5. Location of tremor source and estimation of lava output using tremor source amplitude on the Piton de La Fournaise volcano: 1. Location of tremor sources;Battaglia;J. Volcanol. Geotherm. Res.,2005

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