The Middle–Late Triassic Closure of the East Paleotethys Ocean: Paleomagnetic Evidence from the Baoshan Terrane, China  

作　　者：ZHAO Jie HUANG Baochun YAN Yonggang 

机构地区：[1]State Key Laboratory of Continental Dynamics,Department of Geology,Northwest University,Xi’an 710069,China [2]Key Laboratory of Orogenic Belt and Crust Evolution,Ministry of Education,School of Earth and Space Sciences,Peking University,Beijing 100871,China [3]Guangdong Provincial Key Lab of Geodynamics and Geohazards,School of Earth Sciences and Engineering,Sun Yatsen University,Guangzhou 510275,China

出　　处：《Acta Geologica Sinica(English Edition)》2019年第6期1978-1979,共2页地质学报（英文版）

基　　金：financially supported by the National Natural Science Foundation of China (grants No. 41190071 and 41702229)

摘　　要：Objective It is still controversial about when,where and how the East Paleotethys Ocean closed due to the lack of reliable paleomagnetic data from the blocks or terranes located in both sides of the suture,which prohibits our better understanding of a series of key scientific issues such as how major blocks of East Asia collided together。

关 键 词：Paleo East TRIASSIC 

分 类 号：P53[天文地球—古生物学与地层学]