The mobility of W and Mo in subduction zone fluids and the Mo-W-Th-U systematics of island arc magmas

Earth and Planetary Science Letters

Volumn 351-352, Issue , 2012, Pages 195-207

  Bali, E ^a,b   Keppler, H ^b   Audetat, A ^b  

^a UNIVERSITY OF GÖTTINGEN   (Germany)

^b UNIVERSITÄT BAYREUTH   (Germany)

Author keywords

Fluid salinity; Mo solubility; Oxygen fugacity; Subduction zones; W solubility

Indexed keywords

AQUEOUS FLUIDS; ARC MAGMAS; CLINOPYROXENES; ECLOGITES; ISLAND ARC; MANTLE MINERALS; MO-SOLUBILITY; MOLALITIES; OXYGEN FUGACITY; PARTITION COEFFICIENT; REDOX CONDITION; REDOX STATE; SENSITIVE INDICATOR; SOURCE REGION; SUBDUCTION ZONE FLUIDS; SUBDUCTION ZONES; W-SOLUBILITY;

COBALT COMPOUNDS; METAMORPHIC ROCKS; OXIDE MINERALS; SALINITY MEASUREMENT; SODIUM CHLORIDE; SOLUBILITY; STRUCTURAL GEOLOGY;

MOLYBDENUM OXIDE;

ELEMENT MOBILITY; FUGACITY; IGNEOUS GEOCHEMISTRY; ISLAND ARC; MAGMATISM; MOLYBDENUM; SUBDUCTION ZONE; THORIUM; TUNGSTEN; URANIUM;

EID: 84865573191     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2012.07.032     Document Type: Article

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