La Réunion Island dunites as analogs of the Martian chassignites: Tracking trapped melts with incompatible trace elements-Reference-Cited by-同舟云学术

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La Réunion Island dunites as analogs of the Martian chassignites: Tracking trapped melts with incompatible trace elements

Published:2019-11 Issue: Volume:344-345 Page:452-463
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Barrat Jean-Alix,Bachèlery Patrick

Funder

Institut National des Sciences de l'Univers, Centre National de la Recherche Scientifique

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference78 articles.

1. Modeling the recent geochemical evolution of the Piton de la Fournaise volcano, Reunion Island;Albarède;J. Petrol.,1988

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

3. Quantitative models of trace-element behavior in magmatic processes;Allègre;Earth Planet. Sci. Lett.,1978

4. The Grand Brûlé exploration drilling: new data on the deep framework of the Piton de la Fournaise volcano. Part 3: Mineral chemistry of the cumulate rocks;Augé;J. Volcanol. Geotherm. Res.,1989

5. Nodules de péridotite et cumulats d'olivine;Babkine;Bull. Soc. Franc. Mineral. Crist.,1966

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1. A heterogeneous mantle and crustal structure formed during the early differentiation of Mars;Science Advances;2024-05-31

2. Evidence and significance of wehrlitization within continental lithospheric mantle;Acta Petrologica Sinica;2023

3. Melt inclusions in chassignite NWA 2737: A link between processes recorded in Martian meteorites and rocks at Gale crater;Meteoritics & Planetary Science;2021-07

4. Olivines in main-group pallasites: magma-ocean cumulates or partial melting residues?;Geochemical Perspectives Letters;2021-01

5. Layered gabbros and peridotites from Piton des Neiges volcano, La Réunion Island;Journal of Volcanology and Geothermal Research;2020-11

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