亞洲的顯生宙大陸增生與特提斯的“基梅里”造山作用

摘要：

Asia that comprises numerous ancient cratonicblocks and young mobile belts isthe largestcomposite continent on Earth.It was enlargedby successive accretion ofdispersed terranesthat,associated with opening and closure of the Paleo-Asian andTethys oceans,had produced avast amount of juvenile continental crust.The CentralAsian orogenic belt(CAOB),for instance,is celebrated for its accretionary tectonicsand production of massive juvenile crust in the Phanerozoic or,most significantly,inthe Paleozoic.The Tethyan domain consisted of two major oceans,i.e.Paleo-Tethysin north and Neo-Tethys in south,separated by a strip of continents/terrains called theCimmerian Continent(Sengor,1984),most of which had begun splitting from thenorthern margin ofGondwanaland during Triassic time.

关键词： 构造地质学 大陆增生 特提斯 造山作用 亚洲板块

作者: Sun-Lin Chung Han-Yi Chiu Hao-Yang Lee Fu-Yuan Wu Mohammad H.Zarrinkoub Avtandil Okrostsvaridze Ghazar Galoyan A. Feyzi Bingol

作者单位: Department of Geosciences,National Taiwan University,Taipei Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing Department of Geology,Birjand University,Birjand,Iran Institute of Earth Sciences,Ilia State University,Tbilisi,Georgia Institute of Geology,Armenian National Academy of Sciences,Yerevan,Armenia Department of Geological Engineering,Firat University,Elazig,Turkey

会议类型: 国内会议

会议名称: 2013年全国岩石学与地球动力学研讨会

会议地点: 广州

会议语种:中文

页码: 456-457

在线出版日期: 2013-10-01（万方平台首次上网日期，不代表论文的发表时间）