Increase of juvenal mantle-derived composition from syn-orogenic to post-orogenic granites of the east part of the erstern Tianshan (China) and implications for continental vertical growth: Sr and Nd isotopic evidence;东天山东段同造山到后造山花岗岩幔源组分的递增及 陆壳垂向生长意义-Sr,Nd同位素证据

Yanshi Xuebao/Acta Petrologica Sinica

Volumn 24, Issue 4, 2008, Pages 762-771

  Wang, Tao ^a   Li, WuPing ^b   Li, JinBao ^c   Hong, DaWei ^a   Tong, Ying ^a   Li, Shan ^a  

^a INSTITUTE OF GEOLOGY   (China)

^b GUANGZHOU UNIVERSITY   (China)

^c CHANG'AN UNIVERSITY   (China)

Author keywords

Central Asian Orogenic Belt; Granite; Isotopic evolution; Mafic vein; Phanerozoic vertical continental growth

Indexed keywords

EID: 85168629107     PISSN: 10000569     EISSN: 20958927     Source Type: Journal    
DOI: None     Document Type: Article

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