Hydrogen partitioning between nominally anhydrous upper mantle minerals and melt between 3 and 5 GPa and applications to hydrous peridotite partial melting

Chemical Geology

Volumn 262, Issue 1-2, 2009, Pages 42-56

  Tenner, Travis J ^a   Hirschmann, Marc M ^a   Withers, Anthony C ^a   Hervig, Richard L ^b  

^a UNIVERSITY OF MINNESOTA   (United States)

^b ARIZONA STATE UNIVERSITY   (United States)

Author keywords

Experimental petrology; Hydrogen partitioning; Mantle melting

Indexed keywords

ALUMINUM; GARNETS; GLASS; HYDROGEN; MELTING; MINERALS; OLIVINE; SILICATE MINERALS; STRUCTURAL GEOLOGY;

ANHYDROUS MANTLE; ELECTRON MICROPROBES; EXPERIMENTAL PETROLOGY; GARNET-LHERZOLITE; HYDROGEN PARTITIONS; MANTLE MELTING; MID OCEAN RIDGE BASALTS; TETRAHEDRAL SITES;

DATA HANDLING;

CLINOPYROXENE; EXPERIMENTAL MINERALOGY; GARNET; HIGH PRESSURE; HIGH TEMPERATURE; HYDROGEN; MELT; MID-OCEAN RIDGE BASALT; OLIVINE; ORTHOPYROXENE; PARTIAL MELTING; PARTITION COEFFICIENT; PARTITIONING; PERIDOTITE; PETROLOGY; PRESSURE EFFECT; PYROXENE; TEMPERATURE EFFECT; UPPER MANTLE;

EID: 68549141018     PISSN: 00092541     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.chemgeo.2008.12.006     Document Type: Article

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