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首页> 外文期刊>Volcanology and Seismology >Water-level changes in the wells of Kamchatka at the time of the M w 7.6, April 20, 2006 Olyutorskii earthquake
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Water-level changes in the wells of Kamchatka at the time of the M w 7.6, April 20, 2006 Olyutorskii earthquake

机译:2006年4月20日奥利托尔斯基大地震造成7.6瓦时堪察加半岛水井中的水位变化

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摘要

The seismic waves excited by the M^sub ^sub w^^ 7.6 Olyutorskii earthquake that occurred on April 20, 2006 in the Koryak Upland gave rise to water-level changes in five wells situated in continental areas of Kamchatka at hypocentral distances of 750-1150 km. We describe the effects due to seismic waves, as well as the water-level anomalies for February-April 2006 before the earthquake. We used an original technique for the processing of water-level records based on the study of barometric and tidal water-level responses in order to estimate the volume strain in water-saturated rocks during synchronous level variations at two wells. We discuss possible mechanisms for producing anomalous water-level changes due to elastic deformation of monitored groundwater reservoirs and to crack dilatancy in the water-saturated rocks.[PUBLICATION ABSTRACT] Show less
机译:2006年4月20日发生在Koryak高地的M ^ sub ^ sub w ^^ w ^ Olyutorskii 7.6地震激发的地震波在位于堪察加半岛大陆区的750-140 km的偏心距离上引起了五口井的水位变化。 1150公里我们描述了地震波引起的影响,以及地震前2006年2月至4月的水位异常。基于对大气压力和潮汐水位响应的研究,我们使用了一种原始技术来处理水位记录,以便估算两口井水位同步变化时水饱和岩石的体积应变。我们讨论了由于监测的地下水库的弹性变形和饱和水岩石中的裂缝膨胀引起的异常水位变化的可能机制。[出版物摘要]显示更少

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