J4

• 基础地质·矿床·盆地 •    下一篇

西藏羌北地区石炭纪蜓类动物群及其分带

程立人1,陈寿铭1,张以春1,2,吴水忠3   

  1. 1.吉林大学 地球科学学院,长春 130061;2.中国科学院 南京地质古生物研究所,南京 210008;3.东北大学 秦皇岛分校,河北 秦皇岛 066004
  • 收稿日期:2006-03-23 修回日期:1900-01-01 出版日期:2007-01-26 发布日期:2007-01-26
  • 通讯作者: 程立人

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

摘要: 西藏羌北地区石炭纪蜓类动物群是笔者等于2004年首次发现的,并将动物群所在层位建立了瓦垄山组,该套地层中产大量的蜓类化石,种属多,分布连续。经研究,自下而上建立6个蜓类化石带:(1)Eostaffella mosquensis带,(2)Millerella-Eostaffella带,(3)Pseudostaffella-Eostaffella带,(4)Profusuliena带,(5)Fusulina-Fusulinella带,(6)Protriticites-Triticites带。该套含蜓类化石地层的发现,为研究羌北地区晚古生代构造活动提供了信息,也为研究该区石炭纪地层、古生物、生物古地理、区域性地层划分和对比提供了依据。

关键词: 蜓类动物群, 石炭系, 羌北地区, 瓦垄山组

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

中图分类号: 

  • Q915.811.1
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