Fe2+-Mg partitioning between olivine and basaltic melts: Applications to genesis of olivine-phyric shergottites and conditions of melting in the Martian interior

Earth and Planetary Science Letters

Volumn 304, Issue 3-4, 2011, Pages 527-537

  Filiberto, Justin ^a   Dasgupta, Rajdeep ^a  

^a RICE UNIVERSITY   (United States)

Author keywords

Basalt genesis; Fe2+ Mg partitioning; Gusev basalts; Mantle melting; Mantle potential temperatures; Olivine phyric shergottites

Indexed keywords

BASALTIC MELTS; BULK COMPOSITIONS; CONTROL LINES; EXCHANGE COEFFICIENTS; EXPERIMENTAL DATA; FE2+-MG PARTITIONING; GUSEV BASALTS; HIGHER TEMPERATURES; MAGMA COMPOSITION; MAGMATIC SYSTEMS; MANTLE MELTING; MANTLE POTENTIAL TEMPERATURES; MARS EXPLORATION ROVER; MARTIAN MANTLE; MARTIAN METEORITES; MELT COMPOSITIONS; MERIDIANI PLANUM; PARAMETERIZED; PETROGENESIS; ROCK COMPOSITION;

BASALT; MARTIAN SURFACE ANALYSIS; MELTING; SILICATE MINERALS;

OLIVINE;

CRATER; MAFIC ROCK; MANTLE PROCESS; MARS; MARTIAN METEORITE; MELTING; OLIVINE; PARTITIONING; POTENTIAL TEMPERATURE; SHERGOTTITE; TERRESTRIAL ENVIRONMENT;

EMMELICHTHYIDAE;

EID: 79953164552     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2011.02.029     Document Type: Article

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