Ag isotopic and chalcophile element evolution of the terrestrial and martian mantles during accretion: New constraints from Bi and Ag metal-silicate partitioning-Reference-Cited by-同舟云学术

Ag isotopic and chalcophile element evolution of the terrestrial and martian mantles during accretion: New constraints from Bi and Ag metal-silicate partitioning

Published:2020-12 Issue: Volume:552 Page:116590
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Righter K.^ORCID,Schönbächler M.,Pando K.,Rowland R.^ORCID,Righter M.,Lapen T.

Funder

NASA

Publisher

Elsevier BV

Subject

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

Reference81 articles.

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4. The great sulfur depletion of Earth's mantle is not a signature of mantle–core equilibration;Ballhaus;Contrib. Mineral. Petrol.,2017

5. Highly siderophile element composition of the Earth's primitive upper mantle: constraints from new data on peridotite massifs and xenoliths;Becker;Geochim. Cosmochim. Acta,2006

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