亞洲的顯生宙大陸增生與特提斯的“基梅里”造山作用
- 作者：Sun-Lin ChungHan-Yi ChiuHao-Yang LeeFu-Yuan WuMohammad H.ZarrinkoubAvtandil OkrostsvaridzeGhazar GaloyanA. Feyzi Bingol
- 会议时间：2013-10-01
- 关键词：构造地质学 ; 大陆增生 ; 特提斯 ; 造山作用 ; 亚洲板块
- 作者单位：Sun-Lin Chung,Han-Yi Chiu,Hao-Yang Lee(Department of Geosciences,National Taiwan University,Taipei)Fu-Yuan Wu(Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing)Mohammad H.Zarrinkoub(Department of Geology,Birjand University,Birjand,Iran)Avtandil Okrostsvaridze(Institute of Earth Sciences,Ilia State University,Tbilisi,Georgia)Ghazar Galoyan(Institute of Geology,Armenian National Academy of Sciences,Yerevan,Armenia)A. Feyzi Bingol(Department of Geological Engineering,Firat University,Elazig,Turkey)
- 母体文献：2013年全国岩石学与地球动力学研讨会论文集
- 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
- 主办单位：中国地质学会
- 语种：chi
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.