Episodic Paleoproterozoic (∼2.45, ∼1.95 and ∼1.85Ga) mafic magmatism and associated high temperature metamorphism in the Daqingshan area, North China Craton: SHRIMP zircon U-Pb dating and whole-rock geochemistry

Precambrian Research

Volumn 224, Issue , 2013, Pages 71-93

  Wan, Yusheng ^a   Xu, Zhongyuan ^b   Dong, Chunyan ^a   Nutman, Allen ^c   Ma, Mingzhu ^a   Xie, Hangqiang ^a   Liu, Shoujie ^a   Liu, Dunyi ^a   Wang, Huicu ^d   Cu, Hang ^d  

^a INSTITUTE OF GEOLOGY   (China)

^b JILIN UNIVERSITY   (China)

^c UNIVERSITY OF WOLLONGONG   (Australia)

^d TIANJIN INSTITUTE OF GEOLOGY AND MINERAL RESOURCES   (China)

Author keywords

Daqingshan; Geochemistry; Mafic magmatism; North China Craton; Paleoproterozoic; SHRIMP zircon dating

Indexed keywords

AMPHIBOLITE FACIES; DIABASE; EPISODIC EVENT; EXTENSIONAL TECTONICS; GABBRO; GEOCHEMISTRY; GRANULITE FACIES; IGNEOUS INTRUSION; KHONDALITE; MAFIC ROCK; MAGMATISM; MANTLE STRUCTURE; PROTEROZOIC; SHRIMP DATING; ULTRAHIGH TEMPERATURE METAMORPHISM; URANIUM-LEAD DATING; ZIRCON;

CHINA; DAQING SHAN; NEI MONGGOL; NORTH CHINA BLOCK;

EID: 84867619380     PISSN: 03019268     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.precamres.2012.09.014     Document Type: Article

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