中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Paleoproterozoic metamorphism of high-grade granulite facies rocks in the North China Craton: Study advances, questions and new issues

文献类型:期刊论文

作者Zhou, Li-Gang1; Zhai, Ming-Guo1,2; Lu, Jun-Sheng1,2; Zhao, Lei3; Wang, Hao-Zheng4; Wu, Jia-Lin5; Liu, Bo3; Zou, Yi3; Shan, Hou-Xiang3; Cui, Xia-Hong3
刊名PRECAMBRIAN RESEARCH
出版日期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
DOI10.1016/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
WOS记录号WOS:000423004300027
出版者ELSEVIER SCIENCE BV
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)
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.

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来源:地质与地球物理研究所

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