Zircons in the Shenglikou ultrahigh-pressure garnet peridotite massif and its country rocks from the North Qaidam terrane (western China): Meso-Neoproterozoic crust-mantle coupling and early Paleozoic convergent plate-margin processes

Precambrian Research

Volumn 187, Issue 1-2, 2011, Pages 33-57

  Xiong, Qing ^a   Zheng, Jianping ^a,b   Griffin, William L ^b   O'Reilly, Suzanne Y ^b   Zhao, Junhong ^a  

^a CHINA UNIVERSITY OF GEOSCIENCES   (China)

^b MACQUARIE UNIVERSITY   (Australia)

Author keywords

Early Paleozoic convergent plate margin processes; Garnet peridotite massif; Geochronology; Meso Neoproterozoic crust mantle coupling; North Qaidam; Zircon composition

Indexed keywords

CONVERGENT MARGIN; CRUST-MANTLE BOUNDARY; GARNET; GEOCHRONOLOGY; GNEISS; HAFNIUM; ISOTOPIC COMPOSITION; METAMORPHISM; OROGENY; PALEOZOIC; PERIDOTITE; PLATE CONVERGENCE; PROTEROZOIC; PROTOLITH; SUBDUCTION; TECTONIC EVOLUTION; TERRANE; TRACE ELEMENT; ULTRAMAFIC ROCK; URANIUM-LEAD DATING; ZIRCON;

CHINA; QAIDAM MOUNTAINS; QILIAN MOUNTAINS; QINGHAI;

EID: 79954956673     PISSN: 03019268     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.precamres.2011.02.003     Document Type: Article

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