Martian Dunite NWA 2737: Petrographic constraints on geological history, shock events, and olivine color

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Metal-saturated sulfide assemblages in NWA 2737: Evidence for impact-related sulfur devolatilization in Martian meteorites

NWA 2737, a Martian meteorite from the Chassignite subclass, contains minute amounts (0.010 ± 0.005 vol%) of metal-saturated Fe-Ni sulfides. These latter bear evidence of the strong shock effects documented by abundant Fe nanoparticles and planar defects in Northwest Africa (NWA) 2737 olivine. A Ni-poor troilite (Fe ⁄S = 1.0 ± 0.01), sometimes Cr-bearing (up to 1 wt%), coexists with micrometer-...

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Xenon Isotopic Components in Nwa 2737– a Chassignite from the Hot Desert

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Petrographic Constraints on Shock Induced P/t Conditions in Shergottites

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PYROXENE CRYSTAL CHEMISTRY AND THE LATE COOLING HISTORY OF NWA 2737. B. Re- ynard,

ynard, P. Beck, J-A. Barrat and M. Bohn, Laboratoire des Sciences de la Terre, CNRS UMR 5570, Ecole Normale Supérieure de Lyon, 46 allée d’Italie, 69364 Lyon Cedex 7, France. E-mail : [email protected], Geophysical Laboratory, Carnegie Institution of Washington, 5251 Broad Ranch road NW, DC20015. Email:[email protected]. U.B.O.-I.U.E.M., place Nicolas Copernic, F-29280 Plouzané Cedex, France....

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Heterogeneous Noble Gas Distribution in the Nwa 2737

Introduction: NWA 2737 is the second chassignite, whose brown colored appearance different from Chassigny would be due to shock metamorphism. Noble gas compositions so far reported for the NWA 2737 [1, 2] are largely different from those of Chassigny. High Xe/Xe up to ~2 observed in NWA 2737 might be shock-implanted Martian atmospheric Xe. Common ejection event at ∼11 Myr was suggested for NWA ...

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ژورنال

عنوان ژورنال: Journal of Geophysical Research

سال: 2007

ISSN: 0148-0227

DOI: 10.1029/2006je002777