Geochemical characteristics of the La Réunion mantle plume source inferred from olivine-hosted melt inclusions from the adventive cones of Piton de la Fournaise volcano (La Réunion Island)-Reference-Cited by-同舟云学术

Geochemical characteristics of the La Réunion mantle plume source inferred from olivine-hosted melt inclusions from the adventive cones of Piton de la Fournaise volcano (La Réunion Island)

Published:2017-08-18 Issue:9 Volume:172 Page:
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Valer Marina^ORCID,Schiano Pierre,Bachèlery Patrick

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/article/10.1007/s00410-017-1397-2/fulltext.html

Reference116 articles.

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3. Albarède F, Luais B, Fitton G, Semet M, Kaminski E, Upton BGJ, Bachèlery P, Cheminée JL (1997) The geochemical regimes of Piton de la Fournaise volcano (Réunion) during the last 530,000 years. J Petrol 38:171–201

4. Allègre CJ, Hamelin B, Provost A, Dupré B (1987) Topology in isotopic multispace and origin of mantle chemical heterogeneities. Earth Planet Sci Lett 81:319–337

5. Allègre CJ, Schiano P, Lewin E (1995) Differences between oceanic basalts by multitrace element ratio topology. Earth Planet Sci Lett 129(1):1–12

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