Post-collisional granitoids from the Dabie orogen: New evidence for partial melting of a thickened continental crust

Geochimica et Cosmochimica Acta

Volumn 75, Issue 13, 2011, Pages 3815-3838

  He, Yongsheng ^a,b   Li, Shuguang ^a   Hoefs, Jochen ^b   Huang, Fang ^a,c   Liu, Sheng Ao ^a   Hou, Zhenhui ^a  

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

^b UNIVERSITY OF GÖTTINGEN   (Germany)

^c ETH ZURICH   (Switzerland)

Author keywords

[No Author keywords available]

Indexed keywords

CHEMICAL COMPOSITION; CONTINENTAL CRUST; GRANITOID; ISOTOPIC COMPOSITION; ISOTOPIC FRACTIONATION; MAGMA; PARTIAL MELTING; RARE EARTH ELEMENT; SHRIMP DATING; URANIUM-LEAD DATING; ZIRCON;

EID: 79957830820     PISSN: 00167037     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.gca.2011.04.011     Document Type: Article

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