Metamorphic patterns and SHRIMP zircon ages of medium-to-high grade rocks from the Tongbai orogen, central China: Implications for multiple accretion/collision processes prior to terminal continental collision

Journal of Metamorphic Geology

Volumn 29, Issue 9, 2011, Pages 979-1002

  Liu, X C ^a,b   Jahn, B M ^b,c   Hu, J ^a   Li, S Z ^d   Liu, X ^d   Song, B ^e  

^a INSTITUTE OF MINERAL RESOURCES   (China)

^b INSTITUTE OF EARTH SCIENCES   (Taiwan)

^c NATIONAL TAIWAN UNIVERSITY   (Taiwan)

^d OCEAN UNIVERSITY OF CHINA   (China)

^e INSTITUTE OF GEOLOGY   (China)

Author keywords

Accretion collision; Clockwise anticlockwise P T path; Metamorphic patterns; Palaeozoic; Qinling Tongbai Dabie Sulu orogenic belt; U Pb dating

Indexed keywords

ACCRETION/COLLISION; METAMORPHIC PATTERNS; P-T PATH; PALAEOZOIC; QINLING-TONGBAI-DABIE-SULU OROGENIC BELT; U-PB DATING;

GEOCHRONOLOGY; ROCKS; ZIRCON;

METAMORPHIC ROCKS;

ACCRETION; AMPHIBOLITE FACIES; CONTINENTAL ARC; CONTINENTAL COLLISION; DIORITE; ECLOGITE; EMPLACEMENT; GARNET; GEOCHRONOLOGY; GRANULITE FACIES; METAMORPHIC ROCK; OROGENIC BELT; P-T CONDITIONS; PALEOZOIC; PETROLOGY; SHRIMP DATING; SUBDUCTION; ULTRAHIGH PRESSURE METAMORPHISM; URANIUM-LEAD DATING; ZIRCON;

CHINA; HENAN; QINLING MOUNTAINS; SULU BELT; TONGBAI;

EID: 80054027340     PISSN: 02634929     EISSN: 15251314     Source Type: Journal    
DOI: 10.1111/j.1525-1314.2011.00952.x     Document Type: Article

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