地震地质 ›› 1999, Vol. 21 ›› Issue (4): 346-350.

• 构造地质 • 上一篇    下一篇

沂沭断裂带大水场剖面断层泥的ESR年代学研究

孙瑛杰, 卢演俦, 尹功明   

  1. 中国地震局地质研究所 北京 100029
  • 收稿日期:1998-12-31 修回日期:1999-02-28 出版日期:1999-12-08 发布日期:2009-11-25
  • 基金资助:
    国家自然科学基金资助(4972062);中国地震局地质研究所论著99B0053.

A STUDY ON ESR DATING FOR THE DASHUICHANG GOUGE PROFILE OF THE YISHU FAULT ZONE

Sun Yingjie, Lu Yanchou, Yin Gongming   

  1. Institute of Geology, China Seismological Bureau, Beijing 100029
  • Received:1998-12-31 Revised:1999-02-28 Online:1999-12-08 Published:2009-11-25

摘要: 对山东省沂水县大水场断层剖面的断层泥带进行了野外观测和ESR 测年。断层泥的ESR年龄与由其穿插关系等判断出的断层活动次序相符。各断层泥的ESR 年龄显示出大水场断层经历了两个活动较频繁的时段,即0.25~0.28Ma B.P. 和0.45~0.55Ma B.P

关键词: 断层泥, 地质年代学, 断层活动

Abstract: Along the Dashuichang gouge profile of the Yishu fault zone, there are ten divided gouge stripes based on colors and textures of the gouge Thirteen samples for ESR dating have been collected from the various gouge stripes ESR dates of these samples range from 240ka to 530ka B P, and concentrated on two time intervals of 240~310ka and 410~530ka, respectively It means that there might be two major active episodes on the fault during the Quaternary period. The ESR dates of gouge quartz samples are consistent with geological evidence and intersection relationship on outcrop section.

Key words: Fault gouge, Geochronology, Faulting