| 热水塘断层活动性研究 |
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| 引用本文： | 常祖峰,张艳凤,安晓文,王晋南.热水塘断层活动性研究[J].地震研究,2006,29(2):147-150. |
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| 作者姓名： | 常祖峰 张艳凤 安晓文 王晋南 |
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| 作者单位： | 云南省地震局,昆明,650224 |
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| 摘 要： | 通过野外考察，证实了热水塘断层的存在，对断层的规模、展布特征及其最新活动时代进行了认真地论证。认为该断层为中更新世活动断层，规模较小，晚更新世以来无活动迹象。
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| 关 键 词： | 热水塘断层 活动时代 地貌特征 水平右旋走滑 |
| 文章编号： | 1000-0666-(2006)02-0147-04 |
| 收稿时间： | 2005-07-22 |
| 修稿时间： | 2005年7月22日 |
Study on Reshuitang Fault and Its Activity |
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| CHANG Zu-feng,ZHANG Yan-feng,AN Xiao-wen,WANG Jin-nan.Study on Reshuitang Fault and Its Activity[J].Journal of Seismological Research,2006,29(2):147-150. |
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| Authors: | CHANG Zu-feng ZHANG Yan-feng AN Xiao-wen WANG Jin-nan |
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| Institution: | Earthquake Administration of Yunnan Province, Kunming 650224, China |
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| Abstract: | The field investigation proves the existence of the Reshuitang fault. We study its morphological features, extending features and latest active time, determine the fault to be a Middle Pleistocene active fault with small scale and without activity since Late Pleistocene. This shows that the Reshuitang fault is safe, will not affect the Wudongde key water control project that is planned to build. |
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| Keywords: | Reshuitang fault basic character active time morphological features |
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