Shock-induced transformation of olivine to a new metastable (Mg,Fe)2SiO4 polymorph in Martian meteorites

Earth and Planetary Science Letters

Volumn 261, Issue 3-4, 2007, Pages 469-475

  Van de Moortèle, Bertrand ^a   Reynard, Bruno ^a   McMillan, Paul F ^b,c   Wilson, Mark ^b   Beck, Pierre ^a   Gillet, Philippe ^a   Jahn, Sandro ^d  

^a UNIVERSITÉ DE LYON   (France)

^b Materials Chemistry Centre   (United Kingdom)

^c DAVY FARADAY RESEARCH LABORATORY   (United Kingdom)

^d GFZ GERMAN RESEARCH CENTRE FOR GEOSCIENCES   (Germany)

Author keywords

HRTEM; Molecular Dynamics simulation; olivine; transition phase; zeta phase

Indexed keywords

MARTIAN METEORITES; MOLECULAR DYNAMICS SIMULATION; RINGWOODITE; SHOCK-INDUCED TRANSFORMATION; WADSLEYITE; ZETA PHASE;

HIGH RESOLUTION TRANSMISSION ELECTRON MICROSCOPY; MOLECULAR DYNAMICS; OLIVINE; PHASE TRANSITIONS; POLYMORPHISM; PRESSURE EFFECTS; RAMAN SPECTROSCOPY;

METEORITES;

MARTIAN METEORITE; OLIVINE; P-T CONDITIONS; PHASE TRANSITION; POLYMORPHISM; UPPER MANTLE;

EID: 34548529699     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2007.07.030     Document Type: Article

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