Oxygen and hydrogen isotopic compositions of coexistent minerals of the Tasigake alkali granite pluton, northern Xinjiang: Constraints upon the cause of 18O-D depletion and the 18O/16O exchange kinetics

Chinese Science Bulletin

Volumn 44, Issue 12, 1999, Pages 1086-1093

  Liu, Wei ^a   Zhao, Zhenhua ^b   Zhang, Fuqin ^a  

^a INSTITUTE OF GEOLOGY AND GEOPHYSICS   (China)

^b GUANGZHOU INSTITUTE OF GEOCHEMISTRY   (China)

Author keywords

18O D depletion; Alkali granite; Isotopic exchange kinetics; Ulungur

Indexed keywords

EID: 0001441265     PISSN: 10016538     EISSN: None     Source Type: Journal    
DOI: 10.1007/BF02886131     Document Type: Article

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