Hydrous melting of the martian mantle produced both depleted and enriched shergottites

Geology

Volumn 40, Issue 8, 2012, Pages 683-686

  McCubbin, Francis M ^a   Hauri, Erik H ^b   Elardo, Stephen M ^a   Vander Kaaden, Kathleen E ^a   Wang, Jianhua ^b   Shearer, Charles K ^a  

^a UNIVERSITY OF NEW MEXICO   (United States)

^b GEOPHYSICAL LABORATORY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

APATITE; ASTEROIDS; HYDROGEN STORAGE; ICE; MELTING; METEORITES; MOON; TECTONICS;

ALEXANDRIA; DRIVING FORCES; GEOLOGIC PROCESS; GEOMORPHOLOGIC FEATURES; MARTIAN MANTLE; MARTIAN METEORITES; MARTIAN SURFACE; PARENT MAGMAS; PLANETARY EXPLORATION; PLANETARY SCIENCE;

DIGITAL STORAGE;

APATITE; MAGMA; MANTLE STRUCTURE; MARS; MELTING; SHERGOTTITE; SOLAR SYSTEM; WATER CONTENT;

EID: 84866146213     PISSN: 00917613     EISSN: 19432682     Source Type: Journal    
DOI: 10.1130/G33242.1     Document Type: Article

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