ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
湖北秭归晚寒武世末期至早奥陶世早期层序地层格架
  
关键词:sequence-stratigraphy framework  end of Late Cambrian early stage of Early Ordovician  Zigui  Hubei
基金项目:
作者单位
胡宁 中国地质科学院宜昌地质矿产研究所 
雷卞军 中国地质科学院宜昌地质矿产研究所 
黄照先 中国地质科学院宜昌地质矿产研究所 
张开明 中国地质科学院宜昌地质矿产研究所 
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摘要:
The Sequence-Stratigraphy Framework at the End of Late Cambrian Early Stage of Early Ordovician, Zigui County,Hubei
      The mega cycle sequence is dominated by transgression sedimention during the late stage of Late Cambrian the early stage of Early Ordovician in Zigui County, Hubei. On the basis of the study of the out crop sequence stratigraphy and 1∶50000 scale regional geological surveys, Two third order sequences are distinguished from top of the Loushanguan Formation to top of the Honghuayuan Formation. The nature of sequence boundaries and the character of system sracts of the two sequence are summed up and the regional stratigraphic framework is established. Furthermore, the authors conside that the formation and distribution of the massive dolostones were controlled by the sea_level descending events.
HU Ning,LEI Bian-jun,HUANG Zhao-xian,ZHANG Kai-ming.1997.The Sequence-Stratigraphy Framework at the End of Late Cambrian Early Stage of Early Ordovician, Zigui County,Hubei[J].Acta Geoscientica Sinica,18(4):421-428.
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