Off Ibaraki region is located at the southern end of the focal area of the 2011 off the Pacific coast of Tohoku Earthquake (Tohoku Earthquake). A dense network of 32 ocean bottom seismometers (OBSs) was deployed at this region with a station interval of about 6 km from October 2010 (11 OBSs started from February 2010) to October 2011. A large number (> 10,000) of aftershocks following the 2011 Tohoku earthquake were detected by this network. However, precise determination of these hypocenters and focal mechanisms is challenging due to uncertainties of seismic properties of thick sediment layers beneath the seafloor. The P-wave velocity structure has been reasonably constrained by active-source seismic surveys (Mochizuki et al., 2008), but the S-wave velocity structure is still unrevealed despite its importance.To constrain the S-wave velocity of the shallower portion, we apply the ambient noise interferometry to the short-period OBS data in this study. After dividing the data into ten-minute segments, we deconvolve the data with instrumental response function, remove trends, and discard data dominated by seismic events. Then, we apply a one-bit normalization and spectrum whitening. Finally, we calculate cross-correlations for vertical-vertical, radial-radial, and transverse-transverse components to retrieve Green's functions.We measure average phase velocity in the array using spatial auto-correlation method (Aki, 1957; Nishida et al., 2008). The phase velocities of the fundamental Rayleigh, the first-higher Rayleigh, and the fundamental Love modes are 0.5 to 2.5 km/s (in the frequency range of 0.1 to 0.3 Hz), 0.8 to 1.5 km/s (0.17 to 0.3 Hz), and 0.5 to 2.0 km/s (0.25 to 0.1 Hz), respectively. Next, we infer the 1-D average S-velocity isotropic structure by non-linear inversion, whose sensitivity is mainly ~5 km. The results show ~1000 m thick sediment with S-wave velocity of 300–1000 m/s immediately beneath the seafloor. At last, we apply band-pass filter with frequency range of 0.125 Hz and measure travel-time anomaly of the phase velocity in each frequency range, following Nagaoka et al. (2012). We apply non-linear inversion (Rawlinson & Sambridge, 2003) and find low-velocity anomalies in the deeper of the northern part and in the shallower of the center part.
4 0 0 0 地震波干渉法による茨城沖領域の構造推定
1 0 0 0 OA ガウス過程回帰による海底水圧データからの最大津波高予測
- 著者
- 高橋 光太郎 柏原 健之朗 五十嵐 康彦 馬場 俊孝 堀 高峰 岡田 真人
- 出版者
- 一般社団法人 人工知能学会
- 雑誌
- 人工知能学会全国大会論文集 第33回全国大会(2019)
- 巻号頁・発行日
- pp.4K3J1304, 2019 (Released:2019-06-01)
津波による被害を抑えるために,水圧計を使用した津波高即時予測システムは世界中で使われている. 津波の高さは,基本的に伝播中の地形(海底地形)に依存するため,予測には沿岸付近で観測された圧力計の値と海岸近くの予測点での津波の高さの間の相関関係を利用する. 津波高の予測には,被害を最小限に抑えるために予測精度と過小評価を避けることの両方が重要になっている. 従来の方法は,1506の地震シナリオから観測された水圧計の値に幅を持たせその中で最大の津波高を予測値としている.しかし,過小評価を避けるために実際の津波高に比べて大きく予測され,精度の低い手法となっている. 本研究では,ガウス過程回帰を用いた津波高予測手法を拡張し,過小評価が少なく精度の高い予測手法を提案した.また,従来法と提案法において,南海トラフの震・津波観測監視システム(DONET1)の圧力計データを用いて津波高を予測する検証を行い,予測精度と過小評価率の比較を行なった.
- 著者
- 堀 高峰 尾池 和夫
- 出版者
- 海洋出版
- 雑誌
- 月刊地球 (ISSN:03873498)
- 巻号頁・発行日
- vol.20, no.9, pp.582-586, 1998-09
- 著者
- Phil R. CUMMINS 馬場 俊孝 堀 高峰 金田 義行
- 出版者
- 公益社団法人 東京地学協会
- 雑誌
- 地学雑誌 (ISSN:0022135X)
- 巻号頁・発行日
- vol.110, no.4, pp.498-509, 2001-08-25 (Released:2009-11-12)
- 参考文献数
- 39
- 被引用文献数
- 2 2
By carefully analyzing the source process of the 1946 Nankai earthquake and its correlation with plate boundary structure, we attempt to explain the occurrence pattern of historical earthquakes in the Nankai Trough, in which great earthquakes tend to rupture separately either the western or eastern portions of the Nankai Trough. The source process of the 1946 earthquake consists of two major subevents, each corresponding to segments A and B, defined by Ando (1975), which have long been thought to correspond to units of earthquake rupture in the western Nankai Trough. Furthermore, rupture in each subevent begins near the eastern edge of the respective segment, where there are pronounced contortions of the plate boundary : a subducting seamount chain off Cape Muroto and a rapid change in subduction angle beneath the Kii Peninsula. We suggest that these seismotectonic features of the plate boundary shape control to some extent the pattern of great earthquake occurrence in the Nankai Trough.