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Towards the understanding of mega-thrust earthquake occurrence system around southwestern Japan -Developing and utilization of the dense ocean floor observatory-

机译:在日本西南部围绕西南地震发生系统的理解 - 开发利用密集的海底天文台 -

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The Nankai Trough in Southwestern Japan is well known as the mega thrust earthquake generating tsunamis, with the interval of 100-150 years. The 1944 Tonankai and the 1946 Nankai earthquakes around the Nankai trough, each hypocenter was located off the Kii peninsula in southwestern Japan. Based on crustal structure and simulation researches, we proposed and have been starting to deploy the dense ocean floor observatory network system around the Tonankai seismogenic zone, to monitor crustal activities using broadband seismometer, accelerometer and precise pressure gauges. The ocean floor network is significant ant important to monitor the crustal activities around mega-thrust earthquakes. Furthermore, this system will contribute to early warning of earthquakes and tsunamis.
机译:日本西南部的南开槽是众所周知的Mega推力地震产生海啸,间隔为100-150岁。 1944年的Tonankai和1946年南开地震周围的南开槽,每个斜视都位于日本西南部的Kii半岛。 基于地壳结构和仿真研究,我们提出并开始在彩色地震区周围部署密集的海底天文台网络系统,以监测使用宽带地震计,加速度计和精确压力表的地壳活动。 海底网络是重要的反对者重要的是,以监测大规模推力地震周围的地壳活动。 此外,该系统将有助于地震和海啸的预警。

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