Elastic flexure controls magma trajectories and explains the offset of primary volcanic activity upstream of mantle plume axis at la Réunion and Hawaii hotspot islands-Reference-Cited by-同舟云学术

Elastic flexure controls magma trajectories and explains the offset of primary volcanic activity upstream of mantle plume axis at la Réunion and Hawaii hotspot islands

Published:2017-03 Issue: Volume:462 Page:142-156
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Gerbault Muriel,Fontaine Fabrice J.^ORCID,Rabinowicz Michel,Bystricky Misha^ORCID

Funder

CNRS–INSU

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference57 articles.

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3. Double layering of a thermochemical plume in the upper mantle beneath Hawaii;Ballmer;Earth Planet. Sci. Lett.,2013

4. Mantle flow beneath La Réunion hotspot track from SKS splitting;Barruol;Earth Planet. Sci. Lett.,2013

5. Elasticity of minerals, glasses, and melts;Bass,1995

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5. Extensive CO2 degassing in the upper mantle beneath oceanic basaltic volcanoes: First insights from Piton de la Fournaise volcano (La Réunion Island);Geochimica et Cosmochimica Acta;2018-08