Petrogenesis of Fushan high-Mg#diorites from the southern Taihang Mts. In the central North China Craton: Resulting from interaction of peridotite-melt derived from partial melting of delaminated lower continental crust.;太行山南段符山高镁闪长岩的成因-拆沉陆壳物质 熔融的熔体与地幔橄榄岩反应的结果

Yanshi Xuebao/Acta Petrologica Sinica

Volumn 25, Issue 8, 2009, Pages 1947-1961

  Xu, Wenliang ^a,b,c   Yang, Debin ^a   Pei, Fuping ^a   Yu, Yang ^a  

^a JILIN UNIVERSITY   (China)

^b Northwest University   (China)

^c CHINA UNIVERSITY OF GEOSCIENCES   (China)

Author keywords

Fushan intrusion; High Mg diorite; Melt peridotite reaction; Mesozoic lithospheric mantle; Petrogenesis; Southern Taihang Mts

Indexed keywords

EID: 85168630796     PISSN: 10000569     EISSN: 20958927     Source Type: Journal    
DOI: 10.0000/17fddb77ef5141e99e0359303e5a175f     Document Type: Article

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