Ahrensite, γ-Fe2SiO4, a new shock-metamorphic mineral from the Tissint meteorite: Implications for the Tissint shock event on Mars

Author:

Ma Chi,Tschauner Oliver,Beckett John R.,Liu Yang,Rossman George R.,Sinogeikin Stanislav V.,Smith Jesse S.,Taylor Lawrence A.

Funder

NSF

U.S. DOE

National Nuclear Security Administration

DOE

NASA

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference68 articles.

1. Shock compression of feldspars;Ahrens;J. Geophys. Res.,1969

2. Dependence of site occupancy and structural and electrical properties on successive replacement of Co by Zn in CoFe2O4;Akram;J. Electron. Mater.,2014

3. Tissint Martian meteorite: a fresh look at the interior, surface, and atmosphere of Mars;Aoudjehane;Science,2012

4. Simulating the thermochemical magmatic and tectonic evolution of Venus’s mantle and lithosphere: two-dimensional models;Armann;J. Geophys. Res.,2012

5. CITZAF: a package of correction programs for the quantitative electron microbeam X-ray analysis of thick polished materials, thin films, and particles;Armstrong;Microbeam Anal.,1995

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