Dehydration and melting experiments constrain the fate of subducted sediments

Geochemistry, Geophysics, Geosystems

Volumn 1, Issue 12, 2000, Pages

  Johnson, Marie C ^a   Plank, Terry ^b,c  

^a UNITED STATES MILITARY ACADEMY   (United States)

^b UNIVERSITY OF KANSAS   (United States)

^c BOSTON UNIVERSITY   (United States)

Author keywords

island arc magmatism; mineral fluid partitioning; partition coefficients; subduction zone magmatism

Indexed keywords

ATOMIC EMISSION SPECTROSCOPY; BERYLLIUM; DEHYDRATION; INDUCTIVELY COUPLED PLASMA; INDUCTIVELY COUPLED PLASMA MASS SPECTROMETRY; MASS SPECTROMETRY; MELTING; MICA; PHASE EQUILIBRIA; PHOSPHATE MINERALS; RUBIDIUM; SILICATE MINERALS; SPECTROMETRY; TECTONICS; TRACE ELEMENTS;

INDUCTIVELY COUPLED PLASMA MASS SPECTROMETRIES (ICPMS); INDUCTIVELY COUPLED PLASMA-ATOMIC EMISSION SPECTROMETRY; ISLAND ARC; MAGMATISMS; PARTITION COEFFICIENT; SEDIMENT COMPOSITION; TRACE ELEMENT PARTITIONING; TRANSFER MECHANISMS;

SEDIMENTS;

EID: 84957594966     PISSN: None     EISSN: 15252027     Source Type: Journal    
DOI: 10.1029/1999GC000014     Document Type: Article

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