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Continuous Observation of Groundwater and Crustal Deformation for Forecasting Tonankai and Nankai Earthquakes in Japan

机译:连续观测地下水和地壳变形以预测日本的Tonankai和Nankai地震

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摘要

In 2006, we started construction of an observation network of 12 stations in and around Shikoku and the Kii Peninsula to conduct research for forecasting Tonankai and Nankai earthquakes. The purpose of the network is to clarify the mechanism of past preseismic groundwater changes and crustal deformation related to Tonankai and Nankai earthquakes. Construction of the network of 12 stations was completed in January 2009. Work on two stations, Hongu-Mikoshi (HGM) and Ichiura (ICU), was finished earlier and they began observations in 2007. These two stations detected strain changes caused by the slow-slip events on the plate boundary in June 2008, although related changes in groundwater levels were not clearly recognized.
机译:2006年,我们开始在四国和纪伊半岛及其周边地区建立一个由12个站点组成的观测网络,以进行预测Tonankai和Nankai地震的研究。该网络的目的是弄清与Tonankai和Nankai地震有关的过去地震前地下水变化和地壳变形的机制。由12个站点组成的网络的建设于2009年1月完成。Hongu-Mikoshi(HGM)和Ichiura(ICU)这两个站点的工作较早完成,并于2007年开始观测。这两个站点检测到由慢速引起的应变变化。尽管尚未明确认识到地下水位的相关变化,但在2008年6月发生了板块边界滑移事件。

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