Sulfide-metal-oxide phase assemblages in the D'Orbigny angrite: Implications for element diffusion paths involving Fe–Ni–S–O system and redox conditions-Reference-Cited by-同舟云学术

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Sulfide-metal-oxide phase assemblages in the D'Orbigny angrite: Implications for element diffusion paths involving Fe–Ni–S–O system and redox conditions

Published:2023-11 Issue: Volume:237 Page:105770
ISSN:0032-0633
Container-title:Planetary and Space Science
language:en
Short-container-title:Planetary and Space Science

Author:

Varela M.E.^ORCID,Hwang S.-L.,Shen P.,Garcia L.N.,Magnabosco R.

Funder

Consejo Nacional de Investigaciones Científicas y Técnicas

National Science Council

Publisher

Elsevier BV

Subject

Space and Planetary Science,Astronomy and Astrophysics

Reference42 articles.

1. Raman FTIR and Mossbauer spectroscopy of olivines from the D'Orbigny meteorite;Abdu;Meteorit. Planet. Sci.,2011

2. Northwest Africa 8535: Unique Dunitic Angrites. Lunar Planet. Sci. XLVI;Agee,2015

3. Thermo-Calc and DICTRA, Computational tools for materials science;Andersson;Calphad,2002

4. Redox in Magmas: comment on a Recent Treatment of the Kaiserstuhl Volcanics (Braunger et al;Anenburg;J. Petrol.,2019

5. U-Pb ages of angrites;Amelin;Geochem. Cosmochim. Acta,2008

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