Proto-Tehtys Ocean in East Asia (I) Northern and southern border faults and subduction polarity
文献类型:期刊论文
作者 | Li SanZhong1,2; Zhao ShuJuan1,2; Li XiYao1,2; Cao HuaHua1,2; Liu Xin1,2; Guo XiaoYu3; Xiao WenJiao4; Lai ShaoCong5; Yan Zhen3; Li ZongHui6 |
刊名 | ACTA PETROLOGICA SINICA
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出版日期 | 2016-09-01 |
卷号 | 32期号:9页码:2609-2627 |
关键词 | Proto-Tethys Ocean Border faults Early Paleozoic East Asia Subduction polarity |
文献子类 | Article |
英文摘要 | The Proto-Tethys Ocean is a complicately-originated oceanic basin originated from Supercontinent Rodinia breakup and existed from Neoproterozoic to the end of the Early Paleozoic. It was located in the range of north of the Yunnan-Burma-Thailand/Baoshan (Sibumasu) micro-continental blocks and south of the Tarim-North China Block. There is still controversy for a long time on the southern and northern border faults and the late Early Paleozoic subduction polarity of the Proto-Tethys Ocean. It is important for understanding tectonic background, restoration and reconstruction of Supercontinent Pangea assembly. Therefore, this paper used the integrated methods for the latest results of field geology, tectonics, magmatism, sedimentology, geochemistry and tectonic chronology and tomographic imaging, to identify the positions of the southern and northern border faults of the Proto-Tethyan Tectonic Domain, and determine the subduction polarity of the Proto-Tethys Ocean. Integrated analysis results show that to the north is bounded by the paleoLuonan-Luanchuan Suture (or Kuanping Suture) and its extension to West Kunlun; the southern boundary is the Longmu CoShuanghu-Changning-Menglian Suture. The Tarim-Alax-North China Block in the north of the Proto-Tethys Ocean had a southward subduction polarity and collided with the Gondwana along the northern margin of the Gondwana in the Early Devonian, forming a giant orocline now preserved in the Qilian-Altyn Tagh-Qaidam segment of the Central China Orogen. The south branch of the Proto-Tethys Ocean may be closed, making the Greater South China Block including the North Qiangtang, Ruoergai, Yangtze and Cathaysia, Bureya-Jiamusi and Indochina blocks a southward subduction and accretion to the northern margin of the Gondwana in Devonian. |
WOS关键词 | QINLING OROGENIC BELT ; QAIDAM UHPM BELT ; U-PB GEOCHRONOLOGY ; TECTONIC EVOLUTION ; NW CHINA ; GEOCHEMICAL CONSTRAINTS ; ACCRETIONARY TECTONICS ; VOLCANIC-ROCKS ; KUNLUN OROGEN ; TIBET PLATEAU |
WOS研究方向 | Geology |
语种 | 英语 |
WOS记录号 | WOS:000385210900002 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/53281] ![]() |
专题 | 地质与地球物理研究所_岩石圈演化国家重点实验室 |
作者单位 | 1.Ocean Univ China, Coll Marine Geosci, MOE Key Lab Submarine Geosci & Prospecting Tech, Qingdao 266100, Peoples R China 2.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266061, Peoples R China 3.Chinese Acad Geol Sci, Inst Geol, Beijing 100037, Peoples R China 4.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China 5.Northwest Univ, Dept Geol, Xian 710069, Peoples R China 6.China Geol Survey, Xian Geol Survey Ctr, Xian 710054, Peoples R China |
推荐引用方式 GB/T 7714 | Li SanZhong,Zhao ShuJuan,Li XiYao,et al. Proto-Tehtys Ocean in East Asia (I) Northern and southern border faults and subduction polarity[J]. ACTA PETROLOGICA SINICA,2016,32(9):2609-2627. |
APA | Li SanZhong.,Zhao ShuJuan.,Li XiYao.,Cao HuaHua.,Liu Xin.,...&Lan HaoYuan.(2016).Proto-Tehtys Ocean in East Asia (I) Northern and southern border faults and subduction polarity.ACTA PETROLOGICA SINICA,32(9),2609-2627. |
MLA | Li SanZhong,et al."Proto-Tehtys Ocean in East Asia (I) Northern and southern border faults and subduction polarity".ACTA PETROLOGICA SINICA 32.9(2016):2609-2627. |
入库方式: OAI收割
来源:地质与地球物理研究所
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