ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
据牙形石论鄂西茅口组顶部古岩溶不整合面形成时代
  
关键词:Permian  Maokou Formation  Paleokarst unconformity  conodont  Hubei
基金项目:1∶5万《巫山县幅》(H49E006008)、《官渡河幅》(H49E007008)区调联测
作者单位
李志宏 宜昌地质矿产研究所 
牛志军 宜昌地质矿产研究所 
陈立德 宜昌地质矿产研究所 
黄照先 宜昌地质矿产研究所 
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摘要:
The Age of Paleokarst Unconformity at the Top of Maokou Formation in Western Hubei Inferred from Conodonts
      The conodonts illustrated in this paper were collected from paleokarst unconformity at the top of the Permian Maokou Formation,western Hubei.The conodonts are products of redeposition,as shown by color,luster and worn out character of samples.Based on the evolutionary characteristics,geological time limits and modes of occurrenceofconnodonts,thepaleokarstunconformityisconsideredtobeofLateWordian—Early Capitanian in Permian.(i.e., upper part of M.aserrata zone—M.postserrta zone).
LI Zhi-hong,NIU Zhi-jun,CHEN Li-de,HUANG Zhao-xian.2001.The Age of Paleokarst Unconformity at the Top of Maokou Formation in Western Hubei Inferred from Conodonts[J].Acta Geoscientica Sinica,22(2):157-158.
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