Melting of enstatite (MgSiO3) from 10 to 16.5 GPa and the forsterite (Mg2SiO4) - majorite (MgSiO3) eutectic at 16.5 GPa: implications for the origin of the mantle

Journal of Geophysical Research

Volumn 95, Issue B10, 1990, Pages

  Presnall, D C ^a   Gasparik, T ^a  

^a UNIVERSITY OF TEXAS AT DALLAS   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

ENSTATITE; FORSTERITE/MAJORITE EUTECTIC; MANTLE; MELTING CURVE; PHASE RELATION;

EID: 0025638366     PISSN: 01480227     EISSN: None     Source Type: Journal    
DOI: 10.1029/jb095ib10p15771     Document Type: Article

References (0)