乌溪江水库地震的地震地质背景

地震地质 ›› 1986, Vol. 8 ›› Issue (3): 33-43.

乌溪江水库地震的地震地质背景

夏其发¹, 汪雍熙¹, 李敏¹, 许任德², 沈光伟², 陈元栋²

1. 水利水电科学研究院;
2. 水利电力部华东勘测设计院

收稿日期:1984-09-30 出版日期:1986-09-03 发布日期:2009-11-25

THE SEISMOGEOLOGICAL BACKGROUND OF THE WUXIJIANG RESERVOIR-INDUCED SEISMICITY

Xia Qifa¹, Wang Yongxi¹, Li Min¹, Xu Rende², Shen Guangwei², Chen Yuandong²

1. Institute of Water Conservancy and Hydroelectric Power;
2. Institute of East China Hydroelectric Power Reconnaissance

Received:1984-09-30 Online:1986-09-03 Published:2009-11-25

摘要/Abstract

摘要： 乌溪江水库区原被认为是一稳定地区,但蓄水后库区中段发生了频繁的小震。本文根据现场地质调查和测震资料,对区域地震地质背景,库区地质环境、震中区地质条件和水库地震特征等,进行了分析论证,并与新丰江水库的诱震条件作了对比,运用地震地质类比法,对水库诱发地震的发展趋势作出了评价。1983年汛期该库首次蓄至正常高水位,地震的发展没有超出本文的估计。

Abstract: The Wuxijiang reservoir area has been considered to be geologically and seismologi-tally stable,but frequent microearthquakes were observed in the middle part of the reservoir area after impounding.On the basis of geologic field-work and seismic data,we have described and analysed the seismogeological background of this area,the geological environment of the reservoir,the geological conditions of the epicentral area and the features of the reservoir-induced seismicity.The conditions which induced earthquakes during impounding of the reservoir were compared with those in the Xinfengjiang reservoir.And the trending reservoir-induced seismicity was appraised by using seismogeological anlogic method.During the flood season in 1983,the water level of the reservoir was first over the normal one and the seimicity did not exceed our appraisals.

夏其发, 汪雍熙, 李敏, 许任德, 沈光伟, 陈元栋. 乌溪江水库地震的地震地质背景[J]. 地震地质, 1986, 8(3): 33-43.

Xia Qifa, Wang Yongxi, Li Min, Xu Rende, Shen Guangwei, Chen Yuandong. THE SEISMOGEOLOGICAL BACKGROUND OF THE WUXIJIANG RESERVOIR-INDUCED SEISMICITY[J]. SEISMOLOGY AND EGOLOGY, 1986, 8(3): 33-43.