Origin of high-Mg adakitic magmatic enclaves from the Meichuan pluton, southern Dabie orogen (central China): Implications for delamination of the lower continental crust and melt-mantle interaction

Lithos

Volumn 119, Issue 3-4, 2010, Pages 467-484

  Zhang, Chao ^a,b   Ma, Changqian ^a   Holtz, Francois ^a  

^a CHINA UNIVERSITY OF GEOSCIENCES   (China)

^b LEIBNIZ UNIVERSITY HANNOVER   (Germany)

Author keywords

Dabie orogen; Delamination; Eastern China; High Mg adakite; Mafic enclave

Indexed keywords

ADAKITE; CONCENTRATION (COMPOSITION); CONTINENTAL CRUST; CRETACEOUS; CRUSTAL THICKENING; DELAMINATION; IGNEOUS GEOCHEMISTRY; ISOTOPIC COMPOSITION; ISOTOPIC RATIO; LOWER CRUST; MAGNESIUM; NEODYMIUM ISOTOPE; PARTIAL MELTING; PETROGRAPHY; PLUTON; PROTOLITH; STRONTIUM ISOTOPE; ZIRCON;

CHINA; DABIE MOUNTAINS;

EID: 77956903102     PISSN: 00244937     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.lithos.2010.08.001     Document Type: Article

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