Two-stage plume melting: A possible mechanism for the origin of martian magmatism

Earth and Planetary Science Letters

Volumn 235, Issue 3-4, 2005, Pages 469-479

  Shimoda, Gen ^a   Ikeda, Yukio ^b   Kita, Noriko T ^a   Morishita, Yuichi ^a   Imae, Naoya ^c  

^a NATIONAL INSTITUTE OF ADVANCED INDUSTRIAL SCIENCE AND TECHNOLOGY AIST   (Japan)

^b IBARAKI UNIVERSITY   (Japan)

^c NATIONAL INSTITUTE OF POLAR RESEARCH   (Japan)

Author keywords

Geochemical reservoir; Isotope; Magmatism; Mars; Plume; Rare earth element

Indexed keywords

ISOTOPIC COMPOSITION; MARTIAN MAGMATISM; SHERGOTTITE, NAKHLITE AND CHASSIGNITE (SNC);

COMPOSITION; EXTRACTION; ISOTOPES; RARE EARTH ELEMENTS;

MELTING;

GEOCHEMISTRY; ISOTOPIC COMPOSITION; MANTLE PLUME; MARS; RARE EARTH ELEMENT;

EID: 21344435274     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2005.05.005     Document Type: Article

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