Depleted-mantle source for the Ulungur River A-type g-ranites from North Xinjiang, China: Geochemistry and Nd-Sr isotopic evidence, and implications for Phanerozoic crustal growth

Chemical Geology

Volumn 138, Issue 3-4, 1997, Pages 135-159

  Han, Bao Fu ^a   Wang, Shi Guang ^a   Jahn, Bor Ming ^b   Hong, Da Wei ^c   Kagami, Hiroo ^d   Sun, Yuan Lin ^a  

^a PEKING UNIVERSITY   (China)

^b UNIVERSITÉ DE RENNES 1   (France)

^c INSTITUTE OF MINERAL RESOURCES   (China)

^d OKAYAMA UNIVERSITY   (Japan)

Author keywords

A type granite; Altai mountains; Central Asian Orogenic Belt; Nd isotope geochemistry; Rb Sr dating

Indexed keywords

CRUSTAL GROWTH; DEPLETED MANTLE; GRANITE; IGNEOUS GEOCHEMISTRY; ISOTOPIC ANALYSIS; NEODYMIUM/STRONTIUM;

CHINA, XINJIANG, ULUNGUR RIVER;

EID: 0030783340     PISSN: 00092541     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0009-2541(97)00003-X     Document Type: Article

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