地球科学进展 ›› 2012, Vol. 27 ›› Issue (9): 947 -956. doi: 10.11867/j.issn.1001-8166.2012.09.0947

综述与评述 上一篇    下一篇

生长断层活动强度定量研究的主要方法评述
雷宝华   
  1. 1.国土资源部 海洋油气资源与环境地质重点实验室,山东 青岛 266071;2.青岛海洋地质研究所,山东 青岛 266071
  • 收稿日期:2012-04-02 修回日期:2012-07-23 出版日期:2012-09-10
  • 通讯作者: 雷宝华(1984-),男,湖北武汉人,研究实习员,主要从事石油构造分析和天然气水合物成藏研究.E-mail:manoil@163.com
  • 基金资助:

    国家自然科学基金项目“千里岩隆起的构造形态及其地质意义”(编号:41106060)资助.

Review of Methods with Quantitative Studies of Activity Intensity of the Growth Fault

Lei Baohua   

  1. 1.Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Ministry of Land and Resources, Qingdao 266071, China;2.Qingdao Institute of Marine Geology, Qingdao 266071, China
  • Received:2012-04-02 Revised:2012-07-23 Online:2012-09-10 Published:2012-09-10

目前,定量研究生长断层活动强度的主要方法有生长指数法、古落差法、断层活动速率法、(古)滑距法和断层位移—长度关系分析法等。在前人研究的基础上,对这些方法进行系统的补充和总结。从不同方法的提出、判别、前提假设、优缺点和关系对比等方面,进行介绍和评述。并通过实例分析,用生长指数法、古落差法、断层活动速率法和断层位移—长度关系分析法计算大张坨断层的活动强度,指出不同方法的优缺点。最后对生长断层活动定量研究方法的发展趋势进行了预测,认为生长断层活动定量研究向精度不断提高、多种方法综合运用、对断层活动演化研究更全面、揭示更多的地质和油气信息等方面发展。

At present, the methods with quantitative studies of activity intensity of growth fault include growth index, ancient fault throw, fault activity rate, (ancient) sliding distance and the normal fault displacementlength relationship analysis. On the basis of previous research, this paper complements and summarizes these methods systemically. There methods are introduced and reviewed from the perspectives of proposing and distinguishing, the presuppositions and assumptions, the advantages and disadvantages, the comparison of different methods and their relationships. Through case studies, activity intensity of the Dazhangtuo fault with the methods of growth index, the ancient fault throw, fault activity rate and the normal fault displacementlength relationship analysis are calculated and the advantages and disadvantages of these methods are pointed out. Finally, the development trend of growth fault activity in quantitative research is forecasted. It is believed that the accuracy will be improved continuously, a variety of methods will be used, the evolution of fault will be more comprehensively studied, more geological and petroleum information will be revealed.

中图分类号: 

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