| 断层崖演化与古地震研究 |
| |
| 引用本文： | 尤惠川,邓起东,冉勇康.断层崖演化与古地震研究[J].地震地质,2004,26(1):33-45. |
| |
| 作者姓名： | 尤惠川 邓起东 冉勇康 |
| |
| 作者单位： | 中国地震局地球物理研究所,北京,100081;中国地震局地质研究所,北京,100029 |
| |
| 摘 要： | 从断层崖演化模型及其理论分析入手 ,给出了模型的数学分析解 ,导出了一次突发事件和蠕动成因断层崖演化的等时地形 (地层 )线、最大坡度和崖下堆积体截面积的精确表达式 ,据此分析了可能造成的几何与沉积构造特征。根据野外观察、实验分析及理论研究 ,探讨了断层崖演化及其古地震学研究的一些重要问题 ,提出了与断层崖相关的古地震几何形态、沉积结构和实验分析的综合标志 ,并具体研究和确定了与红果子贺兰山东麓断层崖和孟家湾F2 0 1断层崖相关的 8次古地震事件及其近地表特征和复发周期 ,前者为 2 .0～ 3.0ka,平均 2 .4ka ,后者为 3.3～ 4 .0ka ,平均 3.6ka
|
| 关 键 词： | 断层崖 演化 古地震 |
| 文章编号： | 0253-4967(2004)01-0033-13 |
| 修稿时间： | 2002年9月4日 |
DEGRADATION OF FAULT SCARP AND PALEOEARTHQUAKE RESEARCH |
| |
| YOU Hui-chuan DENG Qi-dong RAN Yong-kang Institute of Geophysics,China Earthquake Administration,Beijing ,China Institute of Geology,China Earthquake Administration,Beijing ,China.DEGRADATION OF FAULT SCARP AND PALEOEARTHQUAKE RESEARCH[J].Seismology and Geology,2004,26(1):33-45. |
| |
| Authors: | YOU Hui-chuan DENG Qi-dong RAN Yong-kang Institute of Geophysics China Earthquake Administration Beijing China Institute of Geology China Earthquake Administration Beijing China |
| |
| Institution: | YOU Hui-chuan 1) DENG Qi-dong 2) RAN Yong-kang 2)1) Institute of Geophysics,China Earthquake Administration,Beijing 100081,China 2) Institute of Geology,China Earthquake Administration,Beijing 100029,China |
| |
| Abstract: | This paper deals with the degradation of fault scarp and the identification of paleo-earthquake in the light of theoretical and mathematical analysis of scarp development processes. We propose some models for fault scarp degradation in unstable and diffusion stages, and give out their mathematical solutions. From these solutions, the quantitative relation between geometrical features and/or sedimentary structures of fault scarp is analyzed. Furthermore, the precise expressions of the isochronous form-line o |
| |
| Keywords: | fault scarp degradation paleoearthquake |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
|
