ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
The Carboniferous and Permian sequences in north and south of the Longmucuo-Shuanghu suture zone in Tibet
  
关键词:Carboniferous  Permian  Tibet  Qiangtang  Palaeo-tethys
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作者单位E-mail
ZHANG Yi-chun Nanjing institute of Geology and Palaeontology, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing, 210008, China
 
geozyc@yahoo.com 
YUAN Dong-xun Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China  
ZHAI Qing-guo Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China  
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摘要:
The Carboniferous and Permian sequences in north and south of the Longmucuo-Shuanghu suture zone in Tibet
      The location of the Palaeo-tethys suture in Tibet has been in great dispute for past two decades. The Longmucuo-Shuanghu suture has long been considered as the Palaeo-tethys in Tibet. Restudy of the Carboniferous and Permian sequences in the north and south of this suture reveal that: (1) the Carboniferous and Permian se-quence of the North Qiangtang Block is characterized by containing compound corals and intact fusulinids zones from Moscovian Fusulinella, Fusulina to Changhsingian Palaeofusulina zones; (2) the Early Permian of the South Qiangtang Block is dominated by diamictites and the Middle Permian carbonates found there may deposit on the oceanic seamount.
ZHANG Yi-chun,YUAN Dong-xun,ZHAI Qing-guo.2009.The Carboniferous and Permian sequences in north and south of the Longmucuo-Shuanghu suture zone in Tibet[J].Acta Geoscientica Sinica,30(S1):94-96.
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