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《Journal of Jilin University(Earth Science Edition)》 2009-03
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The Closure Time of the Paleo-Asian Ocean and the Paleo-Tethys Ocean:Implication for the Tectonic Cause of the End-Permian Mass Extinction

LI Peng-wu1,2,GAO Rui1,GUAN Ye1,LI Qiu-sheng11.Lithosphere Research Center,Institute of Geology,CAGS,Beijing 100037,China2.Geo-detection Laboratory,Ministry of Education of China,China University of Geosciences,Beijing 100083,China  
A comparative analysis of paleolatitudes and latitudinal displacements was undertaken for the South China,Cimmerian continent(including Baoshan,Shan-Thai and Qiangtang blocks),the North China and Siberian blocks by using available paleomagnetic data to determine the collisional and amalgamation history of these blocks.The results show that(1)the Baoshan block collided with the South China block in the Late Permian and continued to drift rapidly northwards,together with the South China and Shan-Thai blocks,until the Late Triassic;(2)the paleo-Asian ocean separating North China and Siberian blocks closed in the end-Permian,and North China block collided with Siberian block in the end-Permian(ca.250 Ma);(3)the age correlations between the end-Permian mass extinctions,Siberian traps and Emeishan traps large igneous province and the final closure time of paleo-oceans show that the mass extinctions are closely related to the evolution of these ancient oceans,suggesting that the collision of continents are the main tectonic cause of end-Permian mass extinctions.
【Fund】: 国家自然科学基金项目(40774026);; 中国地质大学(北京)地下信息探测技术与仪器教育部重点实验室开放课题项目(GDL0503)
【CateGory Index】: P541
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