地球科学进展 ›› 2002, Vol. 17 ›› Issue (3): 391 -395. doi: 10.11867/j.issn.1001-8166.2002.03.0391

综述与评述 上一篇    下一篇

潮坪风暴沉积特征及其研究意义
胡明毅 1,2,贺萍   
  1. 1.江汉石油学院,湖北 荆州 434102;2.中国地质大学能源系,北京 100083
  • 收稿日期:2001-04-23 修回日期:2001-09-17 出版日期:2002-12-20
  • 通讯作者: 胡明毅(1965-),男,湖北荆门人,副教授,主要从事沉积学和石油地质研究.E-mail:humy9408@sina.com E-mail:humy9408@sina.com
  • 基金资助:

    国家自然科学基金项目“下古生界深水牵引流沉积研究”(编号:49872050)资助

THE STUDY OF TIDAL STORM DEPOSITS AND ITS RESEARCH SIGNIFCIANCE

HU Ming-yi 1,2,HE Ping 1   

  1. 1.Jianghan Petroleum Institute, Jingzhou 434102,China;2.Faculty of Energy Geology, China University of Geosciences, Beijing 100083, China
  • Received:2001-04-23 Revised:2001-09-17 Online:2002-12-20 Published:2002-06-01

风暴沉积是20世纪70年代后期才指提出的一个重要概念,被认为是沉积学理论的一次重大突破。但是以往的研究多集中在对浅海陆棚区风暴沉积的研究,而对近岸地带潮坪风暴沉积的研究则比较薄弱。系统总结了近20年来国内外对现代潮坪风暴沉积研究的成果,同时介绍了在古代地层中首次识别出的潮坪风暴岩沉积特征,最后指出了潮坪风暴沉积的研究意义。

Storm deposit(tempesite) constitute an important conception which was not put forward until the late 1970s, and it was considered as an great  discovery in sedimentology. The research work in the past, however, was mostly focused on the storm deposits in the shallow-sea shelf(between the fair weather wave base and the storm wave base),  the reports of the storm deposits on the seashore easpecially on tidal flat are rarely seen. The present paper systematically introduces the reseach accomplishments of modern storm deposits in  tidal flat environment, meanwhile introduces the tidal flat tempesite identified  in the ancient rock record. The tidal flat storm deposit is composed of dolostone accumulation bodies, whose bottom has pocket mold and channel mold structures and whose top is convex upward in cloud-like form. The psephitic clasts are arranged mainly in radiating pattern and appear macroscopically in bird-foot or in v-shape pattern. Finally the paper points out the significance of studying tidal  flat storm deposits.

中图分类号: 

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