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Carboniferous Fusulinids and Fusulind Zone in Northern Qiangtang, Tibet

CHENG Li-ren1, CHEN Shou-ming1, ZHANG Yi-chun1,2, WU Shui-zhong3   

  1. 1.College of Earth Sciences, Jilin University,Changchun 130061,China;2.Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008,China;3.Qinhuangdao Branch, Northeast University, Qinhuangdao,Hebei 066004,China
  • Received:2006-03-23 Revised:1900-01-01 Online:2007-01-26 Published:2007-01-26
  • Contact: CHENG Li-ren

Abstract: The Carboniferous fusulinids were discovered by the writer and others in 2004 when carrying on a geological investigation in Northern Qiangtang,Tibet. The Walongshan Formation was established then and it is featured by abundant fusulinid. Six fusulinid zones were established as follows:(1)Eostaffella mosquensis zone,(2)Millerella-Eostaffella zone,(3)Pseudostaffella-Eostaffella zone,(4)Profusuliena zone,(5)Fusulina-Fusulinella zone,(6)Protriticites-Triticites zone. The sequence of strata, being rich in fusulinids, could provide some information to the Late Paleozoic tectonic pattern of the studied area and provide some basic materials for studying the Carboniferous strata, its paleontology, palaeogeography and for the classification of the strata.

Key words: fusulinids fauna, Carboniferous, Northern Qiangtang, Walongshan Formation

CLC Number: 

  • Q915.811.1
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