气候变化领域集成服务门户(CCPortal): Global Meso-Neoproterozoic plate reconstruction and formation mechanism for Precambrian basins: Constraints from three cratons in China

CCPortal

DOI	10.1016/j.earscirev.2019.102946
	Global Meso-Neoproterozoic plate reconstruction and formation mechanism for Precambrian basins: Constraints from three cratons in China
	Li S.; Li X.; Wang G.; Liu Y.; Wang Z.; Wang T.; Cao X.; Guo X.; Somerville I.; Li Y.; Zhou J.; Dai L.; Jiang S.; Zhao H.; Wang Y.; Wang G.; Yu S.
发表日期	2019
ISSN	0012-8875
卷号	198
英文摘要	The Meso-Neoproterozoic period, sometimes referred to as the ‘boring billion’ or ‘Earth's middle age’, spans the interval between the formation of the Columbia and Rodina supercontinents. It is regarded as a stable era of the Earth. However, from a global perspective, there are many intensive events of mafic volcanism, dyke intrusions and formation of rift basins recorded in different cratons during this period. This paper focuses on rift basins that developed in three cratons in China (North China, South China and Tarim cratons), because large-scale primary gasfields, as one of the deep resources, have been discovered recently in rocks of Meso-Neoproterozoic age. The formation mechanisms and tectonic settings of these rift basins as the targets of Deep Earth are discussed, based on the restoration of global positions of the three cratons by pre-existing paleomagnetic data and plate reconstruction. We recognise that the rift basins of the North China Craton are related to extrusion tectonics in the southwest Ordos Block or are pull-apart basins along the northern and southern sides of the Ordos Block. The rift basins of the South China Craton are derived from mantle lithospheric delamination of the Jiangnan Orogen in the eastern South China Craton or subduction retreat and backarc opening in the western South China Craton, respectively. The rift basins of the Tarim Craton originated from the backarc opening along the margin of the Supercontinent Rodinia. © 2019
英文关键词	Mesoproterozoic; Neoproterozoic; North China Craton; Plate reconstruction; Rift basins; South China Craton; Supercontinent; Tarim Craton
语种	英语
scopus关键词	basin evolution; craton; formation mechanism; plate convergence; Precambrian; Proterozoic; rift zone; Rodinia; supercontinent; tectonic reconstruction; tectonic setting; China; North China Block; South China Block; Tarim Block
来源期刊	EARTH-SCIENCE REVIEWS
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/209804
作者单位	Key Lab of Submarine Geosciences and Prospecting Techniques/Institute for Advanced Ocean Study, Ocean University of China, Qingdao, 266100, China; Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao, 266237, China; Research Institute of Petroleum Exploration and Development, PetroChina, Beijing, 100083, China; School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou, 510275, China; UCD School of Earth Sciences, University College Dublin, Belfield, Dublin 4, Ireland; State Key Laboratory of Continental Dynamics, Northwest University, Xi'an, 710069, China
推荐引用方式 GB/T 7714	Li S.,Li X.,Wang G.,et al. Global Meso-Neoproterozoic plate reconstruction and formation mechanism for Precambrian basins: Constraints from three cratons in China[J],2019,198.
APA	Li S..,Li X..,Wang G..,Liu Y..,Wang Z..,...&Yu S..(2019).Global Meso-Neoproterozoic plate reconstruction and formation mechanism for Precambrian basins: Constraints from three cratons in China.EARTH-SCIENCE REVIEWS,198.
MLA	Li S.,et al."Global Meso-Neoproterozoic plate reconstruction and formation mechanism for Precambrian basins: Constraints from three cratons in China".EARTH-SCIENCE REVIEWS 198(2019).