| 1902年吉林汪清6.6级地震与图们江流域地震地质特征 |
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| 引用本文： | 金东淳,崔钟燮,许相希,李华,安在律,姜炳植.1902年吉林汪清6.6级地震与图们江流域地震地质特征[J].东北地震研究,2000,16(3):31-37. |
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| 作者姓名： | 金东淳 崔钟燮 许相希 李华 安在律 姜炳植 |
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| 作者单位： | 吉林省延边朝鲜族自治州地震局吉林!延边 123456，吉林省延边朝鲜族自治州地震局吉林!延边 123456，吉林省延边朝鲜族自治州地震局吉林!延边 123456，吉林省延边朝鲜族自治州地震局吉林!延边 123456，吉林省延边朝鲜族自治州地震局吉林!延边 123456，吉林省延边朝鲜族自治州地震局吉 |
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| 摘 要： | 本文通过地质地貌、氡射气测量等手段，对 1902 年汪清 6.6 级地震事件和图们江。流域新构造运动进行调查研究，重新认定了 1902 年汪清 6.6 级地震的宏观震中位置 ( 东经 129 ° 24， 北纬 43 ° 26 )； 确定了东阳穹房沟 NW 向压剪性断裂为活动性断裂，是发生 1902 年 7 月 3 日 6.6 级地震的发震构造。该断裂附近的主压应力方向为近东西向。
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| 关 键 词： | 汪清地震 宏现震中 图们江流域 地震地质 |
RALATION BETWEEN THE WANGQING 6.6 EARTHQUAKE IN 1902AND THE SEISMOGEOLOGICAL FEATURES IN THE TUMENJIANG VALLEY |
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| JIN Dong-chun CUI Zhong-xie XU Xiang-xi LI Hua AN Zai-lu JIANG Bing-zhi.RALATION BETWEEN THE WANGQING 6.6 EARTHQUAKE IN 1902AND THE SEISMOGEOLOGICAL FEATURES IN THE TUMENJIANG VALLEY[J].Seismological Research of Northeast China,2000,16(3):31-37. |
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| Authors: | JIN Dong-chun CUI Zhong-xie XU Xiang-xi LI Hua AN Zai-lu JIANG Bing-zhi |
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| Abstract: | Features of the Wangqing 6.6 earthquake occurred in 1902 and the tectonic activity in the Tumenjiang valley are studied in this paper by means of geology, geomorphology and Rn radiation. The macroscopic epicentre is determined to be at 12924E,4326N. The NW fault in Qiongfanggou is determined active and to be the seismogenic structure for the 6.6 earthquake. The principal compressional direction in the fault area and nearby is E-W. |
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| Keywords: | The Wangqing earthquake Macroscopic epicentre The Tumengjiang valley Seismogeology |
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