globalchange  > 气候变化与战略
DOI: 10.1016/j.earscirev.2019.102946
论文题名:
Global Meso-Neoproterozoic plate reconstruction and formation mechanism for Precambrian basins: Constraints from three cratons in China
作者: 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.
刊名: Earth Science Reviews
ISSN: 00128252
出版年: 2019
卷: 198
语种: 英语
中文关键词: Mesoproterozoic ; Neoproterozoic ; North China Craton ; Plate reconstruction ; Rift basins ; South China Craton ; Supercontinent ; Tarim Craton
英文关键词: 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
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
Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/165852
Appears in Collections:气候变化与战略

Files in This Item:

There are no files associated with this item.


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

Recommended Citation:
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]. Earth Science Reviews,2019-01-01,198
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Li S.]'s Articles
[Li X.]'s Articles
[Wang G.]'s Articles
百度学术
Similar articles in Baidu Scholar
[Li S.]'s Articles
[Li X.]'s Articles
[Wang G.]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Li S.]‘s Articles
[Li X.]‘s Articles
[Wang G.]‘s Articles
Related Copyright Policies
Null
收藏/分享
所有评论 (0)
暂无评论
 

Items in IR are protected by copyright, with all rights reserved, unless otherwise indicated.