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-Reference-Cited by-同舟云学术

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

Published:2009-07 Issue:1-2 Volume:184 Page:79-92
ISSN:0377-0273
Container-title:Journal of Volcanology and Geothermal Research
language:en
Short-container-title:Journal of Volcanology and Geothermal Research

Author:

Villemant B.,Salaün A.,Staudacher T.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference31 articles.

1. The geochemical regimes of Piton de la Fournaise Volcano (Réunion) during the last 530000 years;Albarède;J. Petrol.,1997

2. Location of tremor sources 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

3. Petrology of 1977 to 1998 eruptions of Piton de la Fournaise, La Réunion Island;Boivin;J. Volcanol. Geotherm. Res.,2009

4. Pb, Hf and Nd isotope compositions of the two Reunion volcanoes (Indian Ocean): a tale of two small-scale mantle “blobs”;Bosch;Earth Planet. Sci. Lett.,2008

5. 3-D surface wave tomography of the Piton de la Fournaise volcano using seismic noise correlations;Brenguier;Geophys. Res. Lett.,2007

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