Generation of Early Indosinian enriched mantle-derived granitoid pluton in the Sanjiang Orogen (SW China) in response to closure of the Paleo-Tethys

Lithos

Volumn 140-141, Issue , 2012, Pages 166-182

  Zi, Jian Wei ^a,b   Cawood, Peter A ^a,c   Fan, Wei Ming ^b   Tohver, Eric ^a   Wang, Yue Jun ^b   McCuaig, T Campbell ^a  

^a UNIVERSITY OF WESTERN AUSTRALIA   (Australia)

^b GUANGZHOU INSTITUTE OF GEOCHEMISTRY   (China)

^c UNIVERSITY OF ST ANDREWS   (United Kingdom)

Author keywords

Closure of the Paleo Tethys; I type calc alkaline granitoids; Mafic magmatic enclaves (MMEs); Sanjiang Orogen; Subduction enrichment; Zircon Hf O isotopes

Indexed keywords

BATHOLITH; CALC ALKALINE ROCK; CRYSTALLIZATION; EMPLACEMENT; ENCLAVE; ENRICHMENT; FELSIC ROCK; FRACTIONAL CRYSTALLIZATION; GRANITOID; HAFNIUM; HOST ROCK; I-TYPE ROCK; ISOTOPIC RATIO; MAFIC ROCK; MAGMA; MANTLE STRUCTURE; OROGENY; OXYGEN ISOTOPE; PLUTON; SHRIMP DATING; SUBDUCTION; TETHYS; TRIASSIC; URANIUM-LEAD DATING; ZIRCON;

EID: 84859043048     PISSN: 00244937     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.lithos.2012.02.006     Document Type: Article

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