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东濮凹陷沙三段正常三角洲沉积中遗迹化石及意义

常龙, 王长征, 胡斌, 陈传浩

常龙, 王长征, 胡斌, 陈传浩. 东濮凹陷沙三段正常三角洲沉积中遗迹化石及意义[J]. 沉积与特提斯地质, 2017, 37(3): 66-73.
引用本文: 常龙, 王长征, 胡斌, 陈传浩. 东濮凹陷沙三段正常三角洲沉积中遗迹化石及意义[J]. 沉积与特提斯地质, 2017, 37(3): 66-73.
CHANG Long, WANG Chang-zheng, HU Bin, CHEN Chuan-hao. Trace fossils from the normal delta deposits in the third member of the Shahejie Formation in the Dongpu depression and their significance[J]. Sedimentary Geology and Tethyan Geology, 2017, 37(3): 66-73.
Citation: CHANG Long, WANG Chang-zheng, HU Bin, CHEN Chuan-hao. Trace fossils from the normal delta deposits in the third member of the Shahejie Formation in the Dongpu depression and their significance[J]. Sedimentary Geology and Tethyan Geology, 2017, 37(3): 66-73.

东濮凹陷沙三段正常三角洲沉积中遗迹化石及意义

基金项目: 

国家自然科学基金项目(41272117)

河南理工大学博士基金(B2016-71)

详细信息
    作者简介:

    常龙(1988-),男,硕士研究生,从事沉积学和遗迹学研究。E-mail:455467633@qq.com

    通讯作者:

    王长征(1979-),男,博士,讲师,沉积学和陆相遗迹学研究。E-mail:wangchangzheng@hpu.edu.cn

  • 中图分类号: P512.2;Q911.28

Trace fossils from the normal delta deposits in the third member of the Shahejie Formation in the Dongpu depression and their significance

  • 摘要: 通过对钻井岩心的观察和遗迹化石的鉴定,在东濮凹陷古近纪沙河街组沙三段发现遗迹化石10属15种,包括:Skolithos vertivalis,Skolithos linearis,Skolithos isp.,Palaeophycus tubularis,Palaeophycus isp.,Planolites montanus,Planolites beverlegensis,Planolites isp.,Mermoides isp.,Taenidium isp.,Teichichnus isp.,Helminthoidichnites tenuis,Helminthopsis isp.,Beaconites isp.和Thalassinoides isp.。根据岩性特征、沉积构造和遗迹化石的组成、分布特征,研究区沙三段主要发育正常三角洲前缘亚相、前三角洲亚相,并划分了反映不同沉积环境和水体深度的2种遗迹组合,分别为Palaeophycus-Planolites遗迹组合和Planolites-Helminthoidichnites遗迹组合。
    Abstract: The trace fossils from the third member of the Palaeogene Shahejie Formation in the Dongpu depression are divided, on the basis of core observation and trace fossil identification, into 10 genera and 15 species, including Skolithos vertivalis, Skolithos linearis, Skolithos isp. and Palaeophycus tubularis, Palaeophycus isp., Planolites montanus, Planolites beverlegensis, Planolites isp., Mermoides isp., Taenidium isp., Teichichnus isp., Helminthoidichnites tenuis, Helminthopsis isp., Beaconites isp., and Thalassinoides isp. According to lithology, sedimentary structures, and the types and distribution of the trace fossils, the normal delta front subfacies and prodelta subfacies are separated in the third member of the Palaeogene Shahejie Formation. Two trace fossil assemblages are also recognized, including the Palaeophycus-Planolites and Planolites-Helminthoidichnites trace fossil assemblages which have reflected different sedimentary environments and water depths in the study area.
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出版历程
  • 收稿日期:  2017-03-08
  • 修回日期:  2017-04-10
  • 发布日期:  2017-09-29

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