Erratum to: H2O storage capacity of olivine and low-Ca pyroxene from 10 to 13 GPa: Consequences for dehydration melting above the transition zone (Contrib Mineral Petrol, 10.1007/s00410-011-0675-7);H2O storage capacity of olivine and low-Ca pyroxene from 10 to 13 GPa: Consequences for dehydration melting above the transition zone

Contributions to Mineralogy and Petrology

Volumn 163, Issue 2, 2012, Pages 297-316

  Tenner, Travis J ^a   Hirschmann, Marc M ^a   Withers, Anthony C ^a   Ardia, Paola ^a  

^a UNIVERSITY OF MINNESOTA   (United States)

Author keywords

410 km discontinuity; Hydrous partial melting; Peridotite

Indexed keywords

CONCENTRATION (COMPOSITION); DEHYDRATION; MID-OCEAN RIDGE BASALT; OLIVINE; P-T CONDITIONS; PARTIAL MELTING; PERIDOTITE; PRESSURE EFFECT; PYROXENE; TRANSITION ZONE; TRANSPORT PROCESS; UPPER MANTLE; VISCOSITY; WATER STORAGE;

EID: 84856215282     PISSN: 00107999     EISSN: None     Source Type: Journal    
DOI: 10.1007/s00410-011-0684-6     Document Type: Erratum

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