The geochemical comparison between the Tongshankou and Yinzu adakitic intrusive rocks in southeastern Hubei: ( delaminated ) lower crustal melting and the genesis of porphyry copper deposit;鄂东南铜山ᄆ、殷祖埃达克质( adakitk )侵入岩的 地球化学特征对比:( 拆沉 )下地壳溶融与 斑岩铜矿的成因

Yanshi Xuebao/Acta Petrologica Sinica

Volumn 20, Issue 2, 2004, Pages 351-360

  Wang, Qiang ^a   Zhao, Zhen Hua ^a   Xu, Ji Feng ^a   Bai, Zheng Hua ^a   Wang, Jian Xin ^b   Liu, Cheng Xin ^b  

^a GUANGZHOU INSTITUTE OF GEOCHEMISTRY   (China)

^b Hubei Geological Survey   (China)

Author keywords

Adakite; Eastern China; Hot mantle diapiring; Lower crust delamination; Lower crust melting; Porphyry copper deposit; Southeastern Hubei

Indexed keywords

EID: 85168640052     PISSN: 10000569     EISSN: 20958927     Source Type: Journal    
DOI: 10.0000/76efc141d2a6490f9fe5f225af04dfcc     Document Type: Article

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