Syneruptive incorporation of martian surface sulphur in the nakhlite lava flows revealed by S and Os isotopes and highly siderophile elements: implication for mantle sources in Mars-Reference-Cited by-同舟云学术

Syneruptive incorporation of martian surface sulphur in the nakhlite lava flows revealed by S and Os isotopes and highly siderophile elements: implication for mantle sources in Mars

Published:2019-12 Issue: Volume:266 Page:416-434
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Mari N.^ORCID,Riches A.J.V.,Hallis L.J.,Marrocchi Y.^ORCID,Villeneuve J.,Gleissner P.^ORCID,Becker H.,Lee M.R.^ORCID

Funder

European Union’s Horizon 2020 Research and Innovation Programme

STFC

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference119 articles.

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4. Re–Os isotopic measurements at the femtomole level in natural samples;Birck;Geostand. Newslett.,1997

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