Paleoproterozoic metamorphism of high-grade granulite facies rocks in the North China Craton: Study advances, questions and new issues

doi:10.1016/j.precamres.2017.06.025

	Paleoproterozoic metamorphism of high-grade granulite facies rocks in the North China Craton: Study advances, questions and new issues
	Zhou, Li-Gang 1; Zhai, Ming-Guo 1,2; Lu, Jun-Sheng 1,2; Zhao, Lei 3; Wang, Hao-Zheng 4; Wu, Jia-Lin 5; Liu, Bo 3; Zou, Yi 3; Shan, Hou-Xiang 3; Cui, Xia-Hong 3
刊名	PRECAMBRIAN RESEARCH
	2017-12-01
卷号	303 页码:520-547
关键词	The Ncc Paleoproterozoic High-grade Granulites Geothermal Gradient Uplift Rate Tectonic Mechanism
ISSN号	0301-9268
DOI	10.1016/j.precamres.2017.06.025
文献子类	Article
英文摘要	High-grade granulite facies rocks (one of extreme granulites) refer in particular to a part with high metamorphic temperature (HT) and high metamorphic pressure (HP) within granulite facies. A part of basement rocks of the North China Craton (NCC) experiences high-grade metamorphisms up to HP-HT granulite-facies or granuite-eclogite transition facies in Paleoproterozoic, which offers ideal natural laboratories to probe into early Precambrian tectonic evolution of the Earth. The studies of Precambrian high-grade metamorphic rocks have made steady progresses on distributions and occurrences of high-grade granulite facies rocks, their mineral interactions (including micro-inclusion mineral), metamorphic conditions, metamorphic chronologies, and metamorphic processes and P-T paths in recent decades. The concept of Incipient Plate Tectonics was proposed by Zhai (1997,2004,2012,2014) and Zhai and Santosh (2011). However, some intractable and controversial scientific problems still exist, which are challenging and significant issues to understand early tectonic evolution of continent crust and the Earth. This paper reviews study advances of Paleoproterozoic high-grade granulite terranes in the NCC and overviews its prospect. Three fundamental characteristics are distinct: 1) Paleoproterozoic high-grade metamorphic rocks seemingly occur in area or broad pan-belt, which widely spread in the northwest NCC, middle NCC, south NCC, eastern NCC and Korean peninsula, in almost all outcrops of Precambrian basements of the NCC (Sino-Korean Craton) except for some coverage districts of Phanerozoic rocks; Three kinds of high-grade rocks have been distinguished, which are HP mafic granulite, HT pelitic granulite and ultramafic granulite. As their country rocks, some tonalite-trondhjemite-granodiorite gneisses (TTGs) could have undergone metamorphism under the same P-T conditions. 2) The HP mafic granulites and HT pelitic granulites are commonly spatially-associated with concordant occurrences, showing the both underwent contemporaneous deformation and metamorphism since peak metamorphic stage.
WOS关键词	U-PB GEOCHRONOLOGY ; HIGH-PRESSURE GRANULITES ; LIAO-JI BELT ; T-T PATHS ; CONTINENTAL LOWER CRUST ; LU-HF ISOTOPES ; KHONDALITE BELT ; TECTONIC IMPLICATIONS ; PELITIC GRANULITES ; PLATE-TECTONICS
WOS研究方向	Geology
语种	英语
出版者	ELSEVIER SCIENCE BV
WOS记录号	WOS:000423004300027
资助机构	National Natural Science Foundation of China(41530208 ; National Natural Science Foundation of China(41530208 ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; QYZDY-SSW-DQc017 ; QYZDY-SSW-DQc017 ; 41602203 ; 41602203 ; XDB18030205) ; XDB18030205) ; National Natural Science Foundation of China(41530208 ; National Natural Science Foundation of China(41530208 ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; QYZDY-SSW-DQc017 ; QYZDY-SSW-DQc017 ; 41602203 ; 41602203 ; XDB18030205) ; XDB18030205) ; National Natural Science Foundation of China(41530208 ; National Natural Science Foundation of China(41530208 ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; QYZDY-SSW-DQc017 ; QYZDY-SSW-DQc017 ; 41602203 ; 41602203 ; XDB18030205) ; XDB18030205) ; National Natural Science Foundation of China(41530208 ; National Natural Science Foundation of China(41530208 ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; QYZDY-SSW-DQc017 ; QYZDY-SSW-DQc017 ; 41602203 ; 41602203 ; XDB18030205) ; XDB18030205)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/82588]
专题	中国科学院地质与地球物理研究所
通讯作者	Zhai, Ming-Guo
作者单位	1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China 2.Northwest Univ, Key Lab Continental Dynam, Xian, Shaanxi, Peoples R China 3.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 4.Southwest Petr Univ, Sch Geosci & Technol, Chengdu 610500, Sichuan, Peoples R China 5.Changan Univ, Sch Earth Sci & Resources, Xian 710054, Shaanxi, Peoples R China
推荐引用方式 GB/T 7714	Zhou, Li-Gang,Zhai, Ming-Guo,Lu, Jun-Sheng,et al. Paleoproterozoic metamorphism of high-grade granulite facies rocks in the North China Craton: Study advances, questions and new issues[J]. PRECAMBRIAN RESEARCH,2017,303:520-547.
APA	Zhou, Li-Gang.,Zhai, Ming-Guo.,Lu, Jun-Sheng.,Zhao, Lei.,Wang, Hao-Zheng.,...&Cui, Xia-Hong.(2017).Paleoproterozoic metamorphism of high-grade granulite facies rocks in the North China Craton: Study advances, questions and new issues.PRECAMBRIAN RESEARCH,303,520-547.
MLA	Zhou, Li-Gang,et al."Paleoproterozoic metamorphism of high-grade granulite facies rocks in the North China Craton: Study advances, questions and new issues".PRECAMBRIAN RESEARCH 303(2017):520-547.