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Suruga Bay earthquake 2009

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Journal Article
Published: 01 December 2012
Bulletin of the Seismological Society of America (2012) 102 (6): 2420–2435.
... topographies, a seawater layer, and a fluid–solid boundary condition to an aftershock ( M w 5.8) of the 2009 Suruga Bay earthquake. We attempt to reproduce observations at seismic stations near the coast and then simulate waveforms in the ocean‐bottom stations. Our results show that a large difference between...
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Journal Article
Published: 01 April 2011
Bulletin of the Seismological Society of America (2011) 101 (2): 688–700.
... of the large event. Finally, an inverse Fourier transform is conducted to obtain the time history of strong ground motions at the site of interest during the large event. The method is applied to strong-motion records during the 11 August 2009 Suruga Bay, Japan, earthquake ( M w 6.2) to confirm its...
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The estimated Fourier amplitude spectra at SGR for the <span class="search-highlight">2009</span> <span class="search-highlight">Suruga</span> <span class="search-highlight">Bay</span> eart...
Published: 01 April 2011
Figure 11. The estimated Fourier amplitude spectra at SGR for the 2009 Suruga Bay earthquake. The horizontal component (gray trace) is the composition of two components. These spectra were computed by multiplying the Fourier amplitude spectra at MKN (Fig.  10 ) with the average spectral ratios
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The observed Fourier amplitude spectra at MKN for the <span class="search-highlight">2009</span> <span class="search-highlight">Suruga</span> <span class="search-highlight">Bay</span> earth...
Published: 01 April 2011
Figure 10. The observed Fourier amplitude spectra at MKN for the 2009 Suruga Bay earthquake. The spectra are smoothed with a Parzen window with a bandwidth of 0.05 Hz. The horizontal component (gray trace) is the composition of two components. The spectra are already corrected for the path
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(a) An overall view of Japan with the main plate boundaries ( Bird, 2003 )....
Published: 01 December 2012
star) simulated with the FDM . The F‐net CMT solution from NIED is also shown. A solid star shows the M w  6.2 mainshock event, the 2009 Suruga Bay earthquake, which occurred two years before the M w  5.8 event. Black contour lines indicate topography every 500 m around the source area. The K
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The observation results of strong ground motions during the <span class="search-highlight">2009</span> <span class="search-highlight">Suruga</span> <span class="search-highlight">Bay</span>...
Published: 01 April 2011
Figure 3. The observation results of strong ground motions during the 2009 Suruga Bay earthquake. (a) Strong-motion stations (solid circles) around the damaged embankment (solid triangle). (b) Distribution of JMA seismic intensity, calculated from the composition of three components. (c
Journal Article
Published: 01 April 2011
Bulletin of the Seismological Society of America (2011) 101 (2): 919–924.
... S. Enescu B. Suzuki W. Asano Y Obara K. Kunugi T. Shiomi K. ( 2010 ). Stress transfer in the Tokai subduction zone from the 2009 Suruga Bay earthquake in Japan , Nat. Geosci. 3 , 496 - 500 . Aoi S. Sekiguchi H. Morikawa N. Kunugi T. ( 2008...
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Journal Article
Published: 12 January 2016
Bulletin of the Seismological Society of America (2016) 106 (1): 54–72.
... a subducting plate and have focal depths>50  km, with the exception of the 2009 Suruga Bay earthquake ( M w  6.2), which had a focal depth of 23 km. Based on this classification, our data set consists of eight crustal, seven interplate, and five intraplate earthquakes (Table  1 ). Here we developed...
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Journal Article
Published: 01 November 2012
Seismological Research Letters (2012) 83 (6): 1104–1105.
... Generation of Nonstationary Artificial Ground Motion Based on Hilbert Transform Yushan Zhang, Fengxin Zhao, and Caihong Yang FDM Simulation of Seismic‐Wave Propagation for an Aftershock of the 2009 Suruga Bay Earthquake: Effects of Ocean‐Bottom Topography and Seawater Layer Takeshi Nakamura, Hiroshi...
Journal Article
Journal: Geosphere
Published: 26 July 2018
Geosphere (2018) 14 (5): 2009–2043.
... traces correlate with clusters of low-frequency tremor, very low frequency earthquakes, and co-seismic slip during great earthquakes ( Cummins and Kaneda, 2000 ; Cummins et al., 2001 ; Ito and Obara, 2006 ; Obana and Kodaira, 2009 ). The seaward edges of several forearc basins (e.g., Kumano Basin...
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Journal Article
Published: 30 January 2018
Bulletin of the Seismological Society of America (2018) 108 (2): 836–856.
... subduction zone from the 2009 Suruga Bay earthquake in Japan , Nature Geosci. 3 , 496 – 500 , doi: 10.1038/NGEO885 . Asano K. , and Iwata T. 2006 . Source process and near‐source ground motions of the 2005 West Off Fukuoka Prefecture earthquake , Earth Planets Space 58 , 93 – 98...
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Journal Article
Journal: Geosphere
Published: 16 February 2018
Geosphere (2018) 14 (2): 535–551.
... site velocities at all the GNSS stations by fitting a function with linear, annual, and semiannual terms for the period from April 2005 to December 2009; we chose this period because it spans only a few tectonic events, including the 2006 earthquake swarm off the eastern coast of the Izu Peninsula...
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The <span class="search-highlight">earthquakes</span> with a rupture model in the literature                Event...
Published: 01 February 2021
, 00:26 6.8 KiK-net 17 Suruga bay 11 Aug 2009, 05:07 6.5 KiK-net 18 Offshore Honshu (Sanriku-Oki) 9 Mar 2011, 11:45 7.3 Hayes (NEIC, Offshore Honshu 2011) 19 Tohoku 11 Mar 2011, 14:46 9 Yue and Lay (2013) 20 Fukushima Hamadori 11 Apr 2011, 17:16 6.68 Kakehi (2004
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Standard Deviation     after Second‐Stage Regression Analyses Calculated fo...
Published: 12 January 2016
Bay 2009/08/11 05:07 6.2 0.21 0.32 0.17 0.22 15 Tohoku 2011/03/11 14:46 9.1 0.35 0.34 0.45 0.43 16 Iwate‐Oki 2011/03/11 15:09 7.4 0.15 0.24 0.14 0.14 17 Ibaraki‐Oki 2011/03/15 15:15 7.9 0.25 0.18 0.26 0.19 18 Northern Nagano 2011/03/12 03:59 6.3 0.18 0.21
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Standard Deviation     after Second‐Stage Regression Analyses Calculated fo...
Published: 12 January 2016
Bay 2009/08/11 05:07 6.2 0.21 0.32 0.17 0.22 15 Tohoku 2011/03/11 14:46 9.1 0.35 0.34 0.45 0.43 16 Iwate‐Oki 2011/03/11 15:09 7.4 0.15 0.24 0.14 0.14 17 Ibaraki‐Oki 2011/03/15 15:15 7.9 0.25 0.18 0.26 0.19 18 Northern Nagano 2011/03/12 03:59 6.3 0.18 0.21
Journal Article
Published: 01 August 2012
Bulletin of the Seismological Society of America (2012) 102 (4): 1462–1476.
..., and the acceleration data is recorded at a sampling frequency of 100 or 200 Hz. Figure  2 demonstrates an example of the variation of ground motions due to the site amplification effect by comparing the ground acceleration records at two adjacent stations from the 11 August 2009 M w  6.2 earthquake in Suruga Bay...
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Journal Article
Published: 01 February 2021
Earthquake Spectra (2021) 37 (1): 505–522.
..., 00:26 6.8 KiK-net 17 Suruga bay 11 Aug 2009, 05:07 6.5 KiK-net 18 Offshore Honshu (Sanriku-Oki) 9 Mar 2011, 11:45 7.3 Hayes (NEIC, Offshore Honshu 2011) 19 Tohoku 11 Mar 2011, 14:46 9 Yue and Lay (2013) 20 Fukushima Hamadori 11 Apr 2011, 17:16 6.68 Kakehi (2004...
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Journal Article
Published: 16 June 2020
Bulletin of the Seismological Society of America (2020) 110 (5): 2577–2597.
... earthquakes recorded by the Kyoshin network (K‐NET) to analyze the horizontal normalized response spectra and the V/H response spectral ratios, using 36 offshore records from six offshore stations throughout the Sagami Bay and 31 onshore records from eight onshore stations adjacent to those offshore stations...
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Journal Article
Journal: Geosphere
Published: 01 August 2011
Geosphere (2011) 7 (4): 868–876.
... transducers at any moment. Lagrangian velocities can then be calculated from the instantaneous positions. Piper and Normark (2009) summarized the initiation processes for turbidity currents into three categories: sediment failure due to earthquake and other submarine landslide processes, direct...
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Journal Article
Journal: Geosphere
Published: 18 December 2020
Geosphere (2021) 17 (1): 171–200.
... earthquakes at tens of sites along the subduction zone ( Atwater et al., 1995 ; Nelson and Personius, 1996 ; Clague, 1997 ; Shennan et al., 1998 ; Kelsey et al., 2002 ; Witter et al., 2003 ; Nelson et al., 2004 ; Schlichting and Peterson, 2006 ; McCalpin and Carver, 2009 ; Valentine et al., 2012...
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