| 用活断层资料分析中国大陆及其邻区晚更新世以来的构造应变特征 |
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| 引用本文： | 荆燕,任金卫,王辉. 用活断层资料分析中国大陆及其邻区晚更新世以来的构造应变特征[J]. 地震研究, 2005, 28(4): 353-358 |
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| 作者姓名： | 荆燕 任金卫 王辉 |
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| 作者单位： | 中国地质大学地球科学与资源学院,北京,100083;中国地震局地壳应力研究所,北京,100085;中国地震局地震预测研究所,北京,100036 |
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| 摘 要： | 根据活断层资料,利用贝塞尔双三次样条模型对中国大陆及其邻区晚更新世以来的平均水平应变率场进行了计算。结果显示,中国大陆的构造膨胀率、构造剪切应变率、构造矩率和旋转角速度的分布都与地震的分布相似,呈条带状,并与活动地块的边界和主要断裂位置一致。另外,中国大陆的地壳变形具有西强东弱的整体特征。
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| 关 键 词： | 活断层 构造应变场 活动地块 晚更新世 中国大陆及其邻区 |
| 文章编号： | 1000-0666-(2005)04-0353-06 |
| 收稿时间： | 2004-10-21 |
| 修稿时间： | 2004-10-21 |
Tectonic Deformation of China Continent and Its Adjacent Regions since Late Pleistocene Inferred from Active Fault Movement Data |
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| JING Yan,REN Jin-wei,WANG Hui. Tectonic Deformation of China Continent and Its Adjacent Regions since Late Pleistocene Inferred from Active Fault Movement Data[J]. Journal of Seismological Research, 2005, 28(4): 353-358 |
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| Authors: | JING Yan REN Jin-wei WANG Hui |
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| Affiliation: | 1. School of the Earth Sciences and Resourses, China University of Geoscience, Beijing 100083, China;2. institute of Crustal Dynamics, CEA, Beijing 100085, China;3. Institute of Earthquake Prediction, CEA, Beifing 100036, China |
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| Abstract: | Using active fault movement data,we calculated the average horizontal strain rate field of China Continent and vicinity since late Pleistocene with Bessel bicubic spline model.The results show that the distribution of the tectonic dilatational strain rate,shear strain rate,tectonic moment rate and rotation rate of China Continent are consistent with that of the earthquake,appearing in the shape of band,and consistent with the locations of active block boundaries and main faults.In addition,the crustal deformation of China Continent is of a whole feature "strong in the west but weak in the east". |
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| Keywords: | active fault tectonic strain field active crustal block Epipleistocene Chinese Continent and vicinity |
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