Metamorphic evolution of (ultra)-high-pressure subduction-related transient crust in the South Tianshan Orogen (Central Asian Orogenic Belt): Geodynamic implications

doi:10.1016/j.gr.2014.11.008

CORC > 地质与地球物理研究所 > 中国科学院地质与地球物理研究所 > 中国科学院矿产资源研究重点实验室

	Metamorphic evolution of (ultra)-high-pressure subduction-related transient crust in the South Tianshan Orogen (Central Asian Orogenic Belt): Geodynamic implications
	Klemd, Reiner 1; Gao, Jun 2; Li, Ji-Lei 1,2; Meyer, Melanie 1
刊名	GONDWANA RESEARCH
	2015-08-01
卷号	28 期号:1 页码:1-25
关键词	South Tianshan Orogen (Ultra-)high-pressure metamorphism Geochronology Accretionary- and continental-type subductions Channel flow exhumation
DOI	10.1016/j.gr.2014.11.008
文献子类	Review
英文摘要	The study of subduction-related high-pressure- and ultra-high-pressure metamorphic rocks exposed in orogenic belts is critical for unraveling the tectonothermal evolution of an orogen. The South Tianshan Orogen of the southwestern Central Asian Orogenic Belt, one of the world's largest accretionary orogens, contains several Paleozoic (ultra-)high-pressure ((U)HP) metamorphic terranes. (U)HP eclogites, blueschists and associated (U)HP metasedimentary rocks of continental and oceanic origin were reported from two localities in the Northern Tianshan (NTS) of Kazakhstan and Kyrgyzstan, namely from the Ordovician Aktyuz and Makbal metamorphic terranes. Furthermore Lower Carboniferous (U)HP eclogites and blueschists of oceanic origin are located in the Southern Tianshan Accretionary Complex (STAC) of southern Kyrgyzstan (Atbashi) and northwestern China (Akeyazi).
WOS关键词	NORTHERN TIEN-SHAN ; P-T PATH ; ULTRAHIGH-PRESSURE METAMORPHISM ; PALEOZOIC TECTONIC EVOLUTION ; FLUID-ROCK INTERACTION ; HP-UHP ROCKS ; ZIRCON U-PB ; TRACE-ELEMENT MOBILIZATION ; CONVERGENT PLATE MARGINS ; MUNCHBERG GNEISS COMPLEX
WOS研究方向	Geology
语种	英语
WOS记录号	WOS:000356743000001
资助机构	Deutsche Forschungsgemeinschaft(KL692/17-3) ; Deutsche Forschungsgemeinschaft(KL692/17-3) ; National Natural Science Foundation(41390445 ; National Natural Science Foundation(41390445 ; IGCP Project(592) ; IGCP Project(592) ; 41025008) ; 41025008) ; Deutsche Forschungsgemeinschaft(KL692/17-3) ; Deutsche Forschungsgemeinschaft(KL692/17-3) ; National Natural Science Foundation(41390445 ; National Natural Science Foundation(41390445 ; IGCP Project(592) ; IGCP Project(592) ; 41025008) ; 41025008)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/62351]
专题	地质与地球物理研究所_中国科学院矿产资源研究重点实验室
作者单位	1.Univ Erlangen Nurnberg, GeoZentrum Nordbayern, D-91054 Erlangen, Germany 2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
推荐引用方式 GB/T 7714	Klemd, Reiner,Gao, Jun,Li, Ji-Lei,et al. Metamorphic evolution of (ultra)-high-pressure subduction-related transient crust in the South Tianshan Orogen (Central Asian Orogenic Belt): Geodynamic implications[J]. GONDWANA RESEARCH,2015,28(1):1-25.
APA	Klemd, Reiner,Gao, Jun,Li, Ji-Lei,&Meyer, Melanie.(2015).Metamorphic evolution of (ultra)-high-pressure subduction-related transient crust in the South Tianshan Orogen (Central Asian Orogenic Belt): Geodynamic implications.GONDWANA RESEARCH,28(1),1-25.
MLA	Klemd, Reiner,et al."Metamorphic evolution of (ultra)-high-pressure subduction-related transient crust in the South Tianshan Orogen (Central Asian Orogenic Belt): Geodynamic implications".GONDWANA RESEARCH 28.1(2015):1-25.