Magmatic to hydrothermal metal fluxes in convergent and collided margins

Ore Geology Reviews

Volumn 40, Issue 1, 2011, Pages 1-26

  Richards, Jeremy P ^a  

^a UNIVERSITY OF ALBERTA   (Canada)

Author keywords

Epithermal deposit; Magmatic hydrothermal fluid; Ore formation; Porphyry deposit; Post subduction; Subduction

Indexed keywords

EPITHERMAL DEPOSITS; MAGMATIC-HYDROTHERMAL FLUID; ORE FORMATION; PORPHYRY DEPOSITS; POST-SUBDUCTION; SUBDUCTION;

ANOXIC SEDIMENTS; BASALT; BIOLOGY; BRITTLE FRACTURE; CHLORINE; CUPOLAS; DEHYDRATION; DEPOSITS; DEWATERING; DOMES; DUCTILE FRACTURE; EFFLUENT TREATMENT; GOLD; GOLD DEPOSITS; LEACHING; LIQUIDS; MELTING; METALS; MINERAL RESOURCES; MOLYBDENUM; MOLYBDENUM DEPOSITS; ORE DEPOSIT GEOLOGY; ORES; OXIDATION; PLATES (STRUCTURAL COMPONENTS); SEDIMENTOLOGY; SILICA; SILICATE MINERALS; SODIUM CHLORIDE; SOLUBILITY; STRUCTURAL GEOLOGY; SULFUR; SULFUR DIOXIDE; SUPERCRITICAL FLUIDS; TECTONICS; TIN; TUNGSTEN; TUNGSTEN DEPOSITS; VAPORS;

FLOW OF FLUIDS;

CONTINENTAL COLLISION; CONVERGENT MARGIN; EMPLACEMENT; EPITHERMAL DEPOSIT; HEAVY METAL; HYDROTHERMAL ALTERATION; HYDROTHERMAL FLUID; MAGMATISM; OCEANIC CRUST; ORE DEPOSIT; ORE-FORMING FLUID; PARTIAL MELTING; PARTITIONING; PORPHYRY; SUBDUCTION ZONE; TECTONIC SETTING;

EID: 79960592786     PISSN: 01691368     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.oregeorev.2011.05.006     Document Type: Review

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