Re-Os pseudo-isochron of disseminated ore from the Kalatongke Cu-Ni sulfide deposit, Xinjiang, Northwest China: Implications for Re-Os dating of magmatic Cu-Ni sulfide deposits

Ore Geology Reviews

Volumn 53, Issue , 2013, Pages 39-49

  Qu, W J ^a   Chen, J F ^a,b   Wang, L B ^a   Li, C ^a   Du, A D ^a  

^a INSTITUTE OF MINERAL RESOURCES   (China)

^b UNIVERSITY OF SCIENCE AND TECHNOLOGY OF CHINA   (China)

Author keywords

Disseminated ore; Kalatongke Cu Ni sulfide deposit; Re Os dating of magmatic deposits; Re Os pseudo isochron

Indexed keywords

ANALYTICAL UNCERTAINTY; NORTHWEST CHINA; ORE-FORMING PROCESS; RE-OS PSEUDO-ISOCHRON; REGRESSION LINES; STRATIGRAPHIC AGE; SULFIDE DEPOSIT; ZIRCON U-PB AGE;

LEAD; NICKEL; NICKEL DEPOSITS; ORES; OSMIUM; STRATIGRAPHY; SULFUR DEPOSITS;

DEPOSITS;

AGE DETERMINATION; COPPER; COUNTRY ROCK; IGNEOUS INTRUSION; MAGMATISM; MASSIVE SULFIDE; MINERAL DEPOSIT; NICKEL; ORE DEPOSIT; RHENIUM-OSMIUM DATING;

CHINA; GANSU; JINCHUAN [GANSU]; XINJIANG UYGUR;

EID: 84876319744     PISSN: 01691368     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.oregeorev.2012.12.007     Document Type: Article

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