地震地质 ›› 2003, Vol. 25 ›› Issue (2): 203-210.

• 研究论文 • 上一篇    下一篇

珠江三角洲部分断裂晚第四纪垂直位移速率

宋方敏1, 汪一鹏1, 李传友1, 陈伟光2, 黄日恒2, 赵红梅2   

  1. 1. 中国地震局地质研究所, 北京, 100029;
    2. 广东省地震局, 广州, 510070
  • 收稿日期:2001-12-24 修回日期:2002-03-10 出版日期:2003-06-04 发布日期:2009-10-26
  • 作者简介:宋方敏,男,1948年生,1975年毕业于南京大学地质系综合找矿专业,副研究员,现主要从事活动构造研究,电话:010-62009029.
  • 基金资助:
    中国地震局"九五"重点项目(95041004)资助.中国地震局地质研究所论著2003B0016.

LATE QUATERNARY VERTICAL DISLOCATION RATE ON SEVERAL FAULTS IN THE ZHUJIANG DELTA AREA

SONG Fang-min1, WANG Yi-peng1, LI Chuan-you1, CHEN Wei-guang2, HUANG Ri-heng2, ZHAO Hong-mei2   

  1. 1. Institute of Geology, China Seismological Bureau, Beijing 100029, China;
    2. Seismological Bureau of Guangdong Province, Guangzhou 510070, China
  • Received:2001-12-24 Revised:2002-03-10 Online:2003-06-04 Published:2009-10-26

摘要: 珠江三角洲地区断裂比较发育,晚第四纪以来的活动方式皆具有垂直差异运动特征,且大多数都呈隐伏状态。文中在对三角洲发育阶段分析的基础上,利用已有钻孔资料,沿断裂两侧寻找位置相互靠近、且能揭露出时代和堆积环境相同的地层层位的一对或多对钻孔进行对比。根据断裂两侧相同层位现今所处海拔高度的差异确定它们沉积以来的垂直位移量,再根据该层位的测年数据计算断裂的垂直位移速率。共计算了5条断裂晚第四纪以来的垂直位移速率,位移速率值为0.14~0.47mm/a。

关键词: 活动断裂, 位移量, 位移速率, 珠江三角洲

Abstract: Fault structures are well developed in the Zhujiang Delta area. They can be classified into NW-, NE- and E-W-trending groups, most of which display distinct features of vertical differential movement. Since most of the faults are buried and their activities are relatively weak, the evidence of vertical dislocation are difficult to be identified directly in the field, and hence the amount of displacement along the faults can not be measured. Fortunately, a large number of drill holes have been drilled during the construction of the Zhujiang Delta, and a lot of data concerning the present altitudes above sea level of late Quaternary deposits and their ages have been measured and determined. Basing on the analysis of the formation and evolution of the Zhujiang Delta, we have selected a pair or some pairs of bore holes, which are close in position and may reveal the deposition time and environment of the same strata for comparative analysis. Then the vertical displacements along the faults can be determined according to the differences between the present altitudes above sea level of the same strata on both sides of the faults, and hence the dislocation rates can be calculated based upon the age data. We have calculated the late Quaternary vertical dislocation rates for 5 faults. The results show that the dislocation rates are within the range of 0.14~0.47mm/a. Among them, the vertical dislocation rate of the Xijiang Fault in the past 29,400 years is 0.44mm/a. The vertical dislocation rate of the Baini-Shawan Fault in the past 15,000 years is 0.39mm/a, while that in the past 11,400 years is 0.38mm/a. The vertical dislocation rate of the Gulao-Conghua Fault in the past 29,530 years is 0.47mm/a. The vertical dislocation rate of the Wuguishan north piedmont fault in the past 6,390 years is 0.19mm/a. The vertical dislocation rate of the Shougouling Fault in the past 29,800 years is 0.14mm/a, and that in the past 17,480 years is 0.19~0.21mm/a. All these results are of great importance to the project of detecting the active faults in major cities that will be carried out in the near future.

Key words: active fault, dislocation, dislocation rate, Zhujiang Delta

中图分类号: