珠江三角洲部分断裂晚第四纪垂直位移速率  

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

作　　者：宋方敏[1] 汪一鹏[1] 李传友[1] 陈伟光[2] 黄日恒[2] 赵红梅[2] 

机构地区：[1]中国地震局地质研究所,北京100029 [2]广东省地震局,广州510070

出　　处：《地震地质》2003年第2期203-210,共8页Seismology and Geology

基　　金：中国地震局"九五"重点项目 (95 0 4 10 0 4 )资助。

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 4 7mm/a。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

关 键 词：珠江三角洲 晚第四纪 活动方式 活动断裂 位移量 位移速率 计算方法 

分 类 号：P542.3[天文地球—构造地质学]