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| 两郧断裂构造解析与第四纪滑动速率研究 | |
| 引用本文： | 陈蜀俊,刘锁旺,姚运生,李先福,祝启坤.两郧断裂构造解析与第四纪滑动速率研究[J].大地测量与地球动力学,2004,24(3):60-66. |
| 作者姓名： | 陈蜀俊 刘锁旺 姚运生 李先福 祝启坤 |
| 作者单位： | 1. 中国地质大学地球科学学院,武汉,430074;中国地震局地震研究所,武汉,430071 2. 中国地震局地震研究所,武汉,430071 3. 武汉化工学院,武汉,430077 |
| 摘 要： | 根据现场调查、大比例尺地质填图和第四纪年代学测定，利用构造解析法分析总结了两郧断裂的基本构造样式、构造变形序次和离散走滑(拉分)型盆地、汇聚挤压型剪切弯曲等相关构造特征；定量估算出两郧断裂中西段第四纪的滑动速率。 |
| 关 键 词： | 断裂构造 第四纪 滑动速率 地质填图 构造形变 |
| 文章编号： | 1671-5942(2004)03-0060-07 |
| 修稿时间： | 2004年3月9日 |
RESEARCH ON STRUCTURAL ANALYSIS AND QUATERNARY SLIP RATE OF LIANGYUN FAULT |
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| Chen Shujun,Liu Suowang Yao YunshengLi Xianfu and Zhu Qikun China University of Geosciences,Wuhan Institute of Seismology,CEA,Wuhan Wuhan Institute of Chemical Technology,Wuhan\.RESEARCH ON STRUCTURAL ANALYSIS AND QUATERNARY SLIP RATE OF LIANGYUN FAULT[J].Journal of Geodesy and Geodynamics,2004,24(3):60-66. | |
| Authors: | Chen Shujun Liu Suowang Yao YunshengLi Xianfu and Zhu Qikun China University of Geosciences Wuhan Institute of Seismology CEA Wuhan Wuhan Institute of Chemical Technology Wuhan\ |
| Institution: | Chen Shujun+1,2),Liu Suowang2) Yao Yunsheng2)Li Xianfu3) and Zhu Qikun3) 1) China University of Geosciences,Wuhan 430074 2) Institute of Seismology,CEA,Wuhan 430071 3) Wuhan Institute of Chemical Technology,Wuhan\ 430077 |
| Abstract: | On the basis of field investigation, large scale(1:50000) geologically mapping, Quaternary age determination, and by use of structural analytic method, we have analysised and compreheserded the basic structural type of the Liangyun fault, structural deformation sequence and dispersed strike slip(pull apart)pattern basin, concentrated pressure shear pattern bend and its relative structures. Quaternary slip rate of the middle western segment of the Liangyun fault is quantitavely estimated. |
| Keywords: | Liangyun fault geologically mapping structural analysis Quaternary slip rate structural deformation |
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