| 1970年通海地震的地震地质特征 |
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| 引用本文： | 张四昌,刘百篪.1970年通海地震的地震地质特征[J].地质科学,1978,13(4):323-335. |
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| 作者姓名： | 张四昌 刘百篪 |
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| 作者单位： | 1. 云南省地震局;
2. 国家地震局兰州地震研究所 |
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| 摘 要： | 一、前言1970年1月5日云南省通海、峨山、建水三县交界地区的曲江河谷发生了7.7级地震,震中位置是:东经102.6°;北纬24.1°,震源深度约为13公里。震中烈度10度强。
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| 关 键 词： | , |
SEISMIC GEOLOGICAL CHARACTERISTICS OF TONGHAI EARTHQUAKE IN 1970 |
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| Zhang Sichang,Liu Bochi.SEISMIC GEOLOGICAL CHARACTERISTICS OF TONGHAI EARTHQUAKE IN 1970[J].Chinese Journal of Geology,1978,13(4):323-335. |
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| Authors: | Zhang Sichang Liu Bochi |
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| Institution: | Yunnan Seismological Bureau |
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| Abstract: | On January 5, 1970, a strong earthquake of magnitude 7.7 occurred in Tonghai region, Yunnan province. As a result, a 48 km-long seismic fault emerged along the north-west trending Qujiang fault. Taking all the other materials with consideration, the fracture connected with the Tonghai earthquake is shown to be mainly a clockwise dislocation between rock bodies in both sides along the fracture, thus producing in the shallow part an upthrust in the NE wall, and in the deeper part a normal fault in nature for the vertical component of dislocation due to the change in the dip by the fracture plane.The geological conditions of Tonghai earthquake and strong earthquake’s cluster in Tonghai region are: 1. The Qujiang fault that has been highly active ever since the Yanshan period to Holocene has formed a weak plane in the crust; 2. Under the influence of the recent stress field, stress concentration in Tonghai region is due to regional large scale tectonic activities; 3. The Qujiang fault is horizontally dislocated by transverse fault, resulting in discontinuity along strike of the fault and in the bending and confluence of the major structures in Tonghai region, which leads to the lock of seismogenetic structure. |
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