• 责任者：Liu Junlai (State Key Laboratory of Geological Processes and Mineral Resources ; China University of Geosciences ; Beijing 100083 ; China) ; Tang Yuan
• 刊名：Journal of Jilin University
• 出版年：2011
• 卷期：41(5)
• 关键词：构造带 ; tectonic zones ; 哀牢山 ; Ailao Mountains
• 页码：p.1285-1303
• 图表：4 illus., 85 refs.
• 分类号：0300
• issnNo：ISSN1671-5888
• isbnNo：CN22-1343/P

The Ailaoshan tectonic zone is the most significant lineament in the eastern oft-com:office:smarttags" />Tibet  (Southeast Asia), which separates the Yangtze-South China and the Indochina blocks. Information on multi-stage complex tectonic evolution is preserved in the rocks in the tectonic zone. Late Archean-Neoproterozoic high grade metamorphic rock series, Cenozoic tectono-magmatic assemblages (shearing deformation structures), Late Permian-Early Triassic Jinping-Song Da rifting rock sequences and Early Carboniferous-Early Triassic Ailaoshan tectonic mélange were well developed from east to west along the Ailaoshan tectonic zone. On the whole, it has experienced three important tectonic stages, i.e. Pre-Tethys, Tethys and Cenozoic intracontinental stages.