Origin of the Darongshan-Shiwandashan S-type granitoid belt from southeastern Guangxi: geochemical and Sr-Nd-Hf isotopic constraints;桂东南大容山-十万大山Ｓ型花岗岩带的成因： 地球化学及Ｓｒ-Ｎｄ-Ｈｆ同位素制约

Yanshi Xuebao/Acta Petrologica Sinica

Volumn 23, Issue 2, 2007, Pages 403-412

  Qi, Chang Shi ^a,b   Deng, Xi Guang ^c   Li, Xian Hua ^a,d   Li, Wu Xian ^a   Yang, Yue Heng ^b,d   Xie, Lie Wen ^d  

^a GUANGZHOU INSTITUTE OF GEOCHEMISTRY   (China)

^b UNIVERSITY OF CHINESE ACADEMY OF SCIENCES   (China)

^c Guangzhou Marine Geological Survey   (China)

^d BEIJING INSTITUTE OF GEOLOGY FOR MINERAL RESOURCES   (China)

Author keywords

Darongshan Shiwandashan; S type granite; Sr Nd Hf isotope; Zircon

Indexed keywords

EID: 85168642696     PISSN: 10000569     EISSN: 20958927     Source Type: Journal    
DOI: 10.0000/c300c51c64a94d17aefdeb80a7f18fca     Document Type: Article

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