２００７年版 震源断層を特定した地震動予測地図 ポスター

In this research, an earthquake motion is estimated by using the earthquake record and microtremors observation of the ground to presure an earthquake motion in the area of

4) Arai, H. : S-wave velocity profiling by inversion of microtremor H/V spectrum, Bull. : Estimation of deep underground velocity structure by inversion of spectral ratio

Kawabe (2008)：SOURCE MODELING AND STRONG GROUND MOTION SIMULATION OF THE 2007 NIIGATAKEN CHUETSU-OKI EARTHQUAKE (Mj=6.8) IN JAPAN, The 14th World Conference on Earthquake

震動 Ss では 7.0%以上，弾性設計用地震動 Sd では

地震 想定D 8.0 74 75 25000 ポアソン 海域の補正係数を用いる震源 地震規模と活動度から算定した値

活断層の評価 中越沖地震の 知見の反映 地質調査.

Using the CMT analysis for aftershocks (M j ＞3.0) of 2004 Mid Niigata earthquake (M j 6.8) carried out by National Research Institute for Earth Science and Disaster Prevention

In this study, spatial variation of fault mechanism and stress ˆeld are studied by analyzing accumulated CMT data to estimate areas and mechanism of future events in the southern