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Volumn 36, Issue 1-3, 2009, Pages 25-51

The Miocene Gangdese porphyry copper belt generated during post-collisional extension in the Tibetan Orogen

Author keywords

Porphyry Cu deposits; Post collisional extensional setting; Tibetan orogen

Indexed keywords

ADAKITES; BASALTIC CRUST; CENOZOIC; COLLISION ZONE; CONTINENTAL COLLISIONS; CONTINUOUS SPECTRUM; FIELD WORKS; FLUID INCLUSION; GEOCHEMICAL AFFINITY; GEOPHYSICAL DATA; HIGH PRESSURE; HIGH SALINITY; HIGH TEMPERATURE; HYDRO-FRACTURING; HYDROTHERMAL FLUIDS; ISOCHRON AGE; LHASA TERRANE; MAGMATIC SYSTEMS; MAGMATISMS; MESOZOIC; MIOCENE; NORMAL FAULT SYSTEM; NORMAL FAULTS; OLIGOCENE; OROGENIC BELTS; PALEOCENE; PORPHYRY COPPERS; PORPHYRY CU DEPOSITS; POST-COLLISIONAL EXTENSIONAL SETTING; SMALL-DIAMETER; SOUTHERN TIBET; SPATIAL LOCALIZATION; THRUST ZONE; TIBETAN OROGEN; TIBETANS; TRIASSIC; VOLCANO-SEDIMENTARY SEQUENCES;

EID: 70350555526     PISSN: 01691368     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.oregeorev.2008.09.006     Document Type: Article
Times cited : (386)

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