SHRIMP U-Pb zircon geochronology of Palaeoproterozoic metasedimentary;rocks in the North China Craton: Evidence for a major Late;Palaeoproterozoic tectonothermal event

doi:10.1016/j.precamres.2006.06.006

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	SHRIMP U-Pb zircon geochronology of Palaeoproterozoic metasedimentary;rocks in the North China Craton: Evidence for a major Late;Palaeoproterozoic tectonothermal event
	Wan, Yusheng 4; Song, Biao ; Liu, Dunyi ; Wilde, Simon A.; Wu, Jiashan ; Shi, Yuruo ; Yin, Xiaoyan ; Zhou, Hongying
刊名	PRECAMBRIAN RESEARCH
	2006
卷号	149 期号:3-4 页码:249-271
关键词	North China Craton Palaeoproterozoic SHRIMP U-Pb dating metasedimentary rocks continental collision Khondalite
ISSN号	0301-9268
DOI	10.1016/j.precamres.2006.06.006
英文摘要	Although metasedimentary successions are widely distributed across the North China Craton, those of Palaeoproterozoic age are restricted to three orogenic belts, namely: the Trans-North China Orogen, the Khondalite Belt and the Jiao-Liao-Ji Belt. Prior to this work, some of those successions were considered to be Archaean in age. The Palaeoproterozoic metasedimentary rocks contain detrital igneous zircon grains with ages ranging from 3.0 to 2.1 Ga, with the majority recording an age between 2.3 and 2.0 Ga. This latter group define a series of magmatic events that occurred between formation of the Archaean basement and deposition of the metasedimentary rock protoliths. The metasedimentary rocks occur as two associations; older volcano-sedimentary units that formed between 2.37 and 2.0 Ma, and younger sedimentary units that formed mainly between 2.0 and 1.88 Ga. All these rock associations were then subjected to metamorphism during the Late Palaeoproterozoic (1.88 and 1.85 Ga) tectonothermal event, named the Luliang Movement in early Chinese literature, which was a continent-continent collision that led to the amalgamation of the North China Craton. (c) 2006 Elsevier B.V. All rights reserved.
学科主题	前寒武纪地质
WOS关键词	HIGH-PRESSURE GRANULITES ; HIGH-GRADE ROCKS ; MESOPROTEROZOIC ; SUPERCONTINENT ; PALEOPROTEROZOIC EVOLUTION ; TECTONIC EVOLUTION ; CRUSTAL ; EVOLUTION ; LIAONING PROVINCE ; DETRITAL ZIRCONS ; GYEONGGI MASSIF ; HENAN ; PROVINCE
WOS研究方向	Geology
语种	英语
出版者	ELSEVIER SCIENCE BV
WOS记录号	WOS:000241073800008
内容类型	期刊论文
源URL	[http://119.78.100.197/handle/2HKVOGP0/38329]
专题	中国地质调查局天津地质调查中心
作者单位	1.Chinese Acad Geol Sci, Inst Geol, Beijing 100037, Peoples R China. 2.Beijing SHRIMP Ctr, Beijing 100037, Peoples R China. 3.Curtin Univ Technol, Dept Appl Geol, Perth, WA 6845, Australia. 4.中国地质科学院地质研究所
推荐引用方式 GB/T 7714	Wan, Yusheng,Song, Biao,Liu, Dunyi,et al. SHRIMP U-Pb zircon geochronology of Palaeoproterozoic metasedimentary;rocks in the North China Craton: Evidence for a major Late;Palaeoproterozoic tectonothermal event[J]. PRECAMBRIAN RESEARCH,2006,149(3-4):249-271.
APA	Wan, Yusheng.,Song, Biao.,Liu, Dunyi.,Wilde, Simon A..,Wu, Jiashan.,...&Zhou, Hongying.(2006).SHRIMP U-Pb zircon geochronology of Palaeoproterozoic metasedimentary;rocks in the North China Craton: Evidence for a major Late;Palaeoproterozoic tectonothermal event.PRECAMBRIAN RESEARCH,149(3-4),249-271.
MLA	Wan, Yusheng,et al."SHRIMP U-Pb zircon geochronology of Palaeoproterozoic metasedimentary;rocks in the North China Craton: Evidence for a major Late;Palaeoproterozoic tectonothermal event".PRECAMBRIAN RESEARCH 149.3-4(2006):249-271.