Late Paleoproterozoic-Neoproterozoic multi-rifting events in the North China Craton and their geological significance: A study advance and review

doi:10.1016/j.tecto.2015.01.019

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

	Late Paleoproterozoic-Neoproterozoic multi-rifting events in the North China Craton and their geological significance: A study advance and review
	Zhai, Mingguo 1,2; Hu, Bo 3; Zhao, Taiping 4; Peng, Peng 5; Meng, Qingren 6
刊名	TECTONOPHYSICS
	2015-11-01
卷号	662 页码:153-166
关键词	North China craton Late Paleoproterozoic-Neoproterozoic Magmatic event Multi-stage rifting Long-term stable continent Extensional tectonic environment
DOI	10.1016/j.tecto.2015.01.019
文献子类	Article
英文摘要	An important Paleoproterozoic mobile belt event took place in the North China Craton (NCC), termed the Hutuo Movement. This event has been interpreted to represent cratonic reworking characterized by rifting-subduction-collision processes. The NCC then evolved into a stable platform or para-platform tectonic setting in Earth's middle age period more than similar to 1.0 Ga. Thick Late Paleoproterozoic-Neoproterozoic sedimentary sequences were extensively deposited on the early metamorphic basement. The major sedimentary basins include the Xiong'er aulacogen system in the south-central NCC, the Yan-Liao aulacogen system in the north-central NCC, the Northern marginal rift system in the northwestern NCC and the Eastern marginal rift system in the eastern NCC. The following four stages of magmatic activity are recognized in the Late Paleoproterozoic to Neoproterozoic interval: (1) similar to 1800 to 1780 Ma Xiong'er igneous province (XIP), (2) similar to 1720 to 1620 Ma anorogenic magmatic association, (3) similar to 1350 to 1320 Ma diabase sill swarms, and (4) similar to 900 Ma mafic dyke swarms. These four magmatic events suggest that the NCC was situated in an intra-plate setting for a long time from similar to 1.8 Ga to similar to 0.7 Ga or even younger, and the magmatic events were associated with multi-stage rifting activities. We document that the NCC was in a long-term extensional tectonic setting during Late Paleoproterozoic-Neoproterozoic era. The main ore deposits in this period are magmatic type iron deposits related to anorthosite-gabbro bodies, REE-Nb-Fe and Pb-Zn-Cu-Fe deposits related to Mesoproterozoic-Neoproterozoic rifts. Orogenic metal deposits are absent. There is no evidence indicating that the Grenville or other orogenic events affected the NCC. The reason for the absence of Grenvillian aged events in the NCC is probably because it was far from the edge of the Nuna supercontinent, if such a supercontinent did exist. There is another possibility that the Earth's middle age represented a particular tectonic evolution period, during which the Earth had a stable lithosphere with underlying secular warm mantle that resulted in multi-magmatism and rifting from the Late Paleoproterozoic to Neoproterozoic. (C) 2015 Elsevier B.V. All rights reserved.
WOS关键词	PRE-RODINIA SUPERCONTINENT ; U-PB AGES ; GEOCHEMICAL CONSTRAINTS ; COLUMBIA SUPERCONTINENT ; RAPAKIVI GRANITE ; XIONGER GROUP ; MAFIC DYKES ; HF ISOTOPES ; ROCKS ; COMPLEX
WOS研究方向	Geochemistry & Geophysics
语种	英语
WOS记录号	WOS:000366227400010
资助机构	973 program(2012CB4166006) ; 973 program(2012CB4166006) ; State Ministry of Science and Technology, and research programs(41030316 ; State Ministry of Science and Technology, and research programs(41030316 ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; 41210003) ; 41210003) ; 973 program(2012CB4166006) ; 973 program(2012CB4166006) ; State Ministry of Science and Technology, and research programs(41030316 ; State Ministry of Science and Technology, and research programs(41030316 ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; 41210003) ; 41210003)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/62156]
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.Northwest Univ, State Key Lab Continental Geodynam, Xian, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing, Peoples R China 3.Changan Univ, Coll Earth Sci & Resources, Xian, Peoples R China 4.Chinese Acad Sci, Guangzhou Inst Geochem, Guangzhou, Guangdong, Peoples R China 5.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithosphere Evolut, Beijing, Peoples R China 6.Chinese Acad Sci, Inst Geol & Geophys, Beijing, Peoples R China
推荐引用方式 GB/T 7714	Zhai, Mingguo,Hu, Bo,Zhao, Taiping,et al. Late Paleoproterozoic-Neoproterozoic multi-rifting events in the North China Craton and their geological significance: A study advance and review[J]. TECTONOPHYSICS,2015,662:153-166.
APA	Zhai, Mingguo,Hu, Bo,Zhao, Taiping,Peng, Peng,&Meng, Qingren.(2015).Late Paleoproterozoic-Neoproterozoic multi-rifting events in the North China Craton and their geological significance: A study advance and review.TECTONOPHYSICS,662,153-166.
MLA	Zhai, Mingguo,et al."Late Paleoproterozoic-Neoproterozoic multi-rifting events in the North China Craton and their geological significance: A study advance and review".TECTONOPHYSICS 662(2015):153-166.