On the iron isotope composition of Mars and volatile depletion in the terrestrial planets-Reference-Cited by-同舟云学术

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On the iron isotope composition of Mars and volatile depletion in the terrestrial planets

Published:2016-09 Issue: Volume:449 Page:360-371
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Sossi Paolo A.^ORCID,Nebel Oliver,Anand Mahesh,Poitrasson Franck

Funder

Australian Postgraduate Award

ANU

Australian Research Council

Science and Technology Facilities Council

CNRS-INSU PNP

Publisher

Elsevier BV

Subject

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

Reference109 articles.

1. Searching for signatures of life on Mars: an Fe-isotope perspective;Anand;Philos. Trans. R. Soc. Lond. B, Biol. Sci.,2006

2. Melting relations of ultramafic lavas (komatiites) at 1 atm and high pressure;Arndt;Year B. - Carnegie Inst. Wash.,1976

3. The differentiation of eucrites: the role of in situ crystallization;Barrat;Meteoritics,2000

4. Early stages of core segregation recorded by Fe isotopes in an asteroidal mantle;Barrat;Earth Planet. Sci. Lett.,2015

5. Petrogenesis of olivine-phyric shergottite Larkman Nunatak 06319: implications for enriched components in martian basalts;Basu Sarbadhikari;Geochim. Cosmochim. Acta,2009

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