Crustal anatexis and formation of two types of granitic magmas in the Kontum massif, central Vietnam: Implications for magma processes in collision zones

Gondwana Research

Volumn 12, Issue 4, 2007, Pages 428-437

  Owada, M ^a   Osanai, Y ^b   Nakano, N ^b   Matsushita, T ^a   Tran Ngoc Nam, ^c   Tsunogae, T ^d   Toyoshima, T ^e   Binh, Pham ^f   Kagami, H ^e  

^a YAMAGUCHI UNIVERSITY   (Japan)

^b KYUSHU UNIVERSITY   (Japan)

^c HUE UNIVERSITY   (Viet Nam)

^d UNIVERSITY OF TSUKUBA   (Japan)

^e NIIGATA UNIVERSITY   (Japan)

^f Research Institute of Geology and Mineral Resources   (Viet Nam)

Author keywords

Adakite; Central Vietnam; Collision zone; The Kontum massif; The Late Permian

Indexed keywords

ANATEXIS; COLLISION ZONE; CRUST; FORMATION MECHANISM; GRANITE; MAGMA; PERMIAN; ULTRAHIGH TEMPERATURE METAMORPHISM;

KONTUM MASSIF; VIET NAM;

EID: 35548978580     PISSN: 1342937X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.gr.2006.11.001     Document Type: Article

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