Silica-rich spinel harzburgite residues formed by fractional hybridization-melting of the intra-oceanic supra-subduction zone mantle: New evidence from TUBAF seamount peridotites-Reference-Cited by-同舟云学术

Silica-rich spinel harzburgite residues formed by fractional hybridization-melting of the intra-oceanic supra-subduction zone mantle: New evidence from TUBAF seamount peridotites

Published:2021-01 Issue: Volume:293 Page:477-506
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Bénard A.,Müntener O.,Pilet S.,Arculus R.J.,Nebel O.

Funder

Australian Research Council

Swiss National Science Foundation

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference116 articles.

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3. Determining the composition of high-pressure mantle melts using diamond aggregates;Baker;Geochim. Cosmochim. Acta,1994

4. High pressure experimental calibration of the olivine orthopyroxene-spinel oxygen geobarometer: implications for the oxidation state of the upper mantle;Ballhaus;Contrib. Mineral. Petrol.,1991

5. Diapirs as the source of the sediment signature in arc lavas;Behn;Nat. Geosci.,2011

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