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Fukushima earthquake 2011

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Journal Article
Published: 18 November 2022
Bulletin of the Seismological Society of America (2023) 113 (1): 498.
.... REFERENCES Lin A. Toda S. Rao G. Tsuchihashi S. , and Yan B. 2013 . Structural analysis of coseismic normal fault zones of the 2011 M w 6.6 Fukushima earthquake, northeast Japan , Bull. Seismol. Soc. Am. 103 , 1603 – 1613 , doi: 10.1785/0120120111 . Lin A. Chen...
Journal Article
Published: 07 September 2021
Bulletin of the Seismological Society of America (2021) 111 (5): 2303–2316.
... by a single observation method due to data acquisition constraints. This study constructs a 3D coseismic deformation model of the 2011 Fukushima‐ken Hamadori earthquake by integrating Differential Interferometric Synthetic Aperture Radar (DInSAR), and differential light detection and ranging (Dlidar) analyses...
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Journal Article
Published: 01 May 2013
Bulletin of the Seismological Society of America (2013) 103 (2B): 1603–1613.
...Aiming Lin; Shinji Toda; Gang Rao; Satoru Tsuchihashi; Bing Yan Abstract The 2011 M w 6.6 Fukushima earthquake occurred in Iwaki City, ∼250 km southwest of the epicenter of the 2011 M w 9.0 Tohoku (Japan) earthquake, and produced two subparallel ∼15–23‐km‐long surface rupture zones with distinct...
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Journal Article
Published: 01 October 2012
Bulletin of the Seismological Society of America (2012) 102 (5): 1949–1956.
...Kazuo Mizoguchi; Shin‐ichi Uehara; Keiichi Ueta Abstract The 11 April 2011 Hamadoori, Fukushima prefecture, northeast Japan, earthquake occurred in a seismically active area, one month after the 11 March 2011 Off the Pacific Coast of Tohoku earthquake. The Hamadoori earthquake resulted in a 14‐km...
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Image
Seismometers installed at <span class="search-highlight">Fukushima</span> Daiichi NPP, <span class="search-highlight">2011</span> Tohoku-oki <span class="search-highlight">earthquake</span>...
Published: 01 February 2017
Figure 2. Seismometers installed at Fukushima Daiichi NPP, 2011 Tohoku-oki earthquake: Dense Surface Array (Left) and Unit 6 Reactor Building (right). (Figure reprinted from JAEE 2011c .)
Journal Article
Journal: Geology
Published: 01 May 2016
Geology (2016) 44 (5): 391–394.
...Cecilia M. McHugh; Toshiya Kanamatsu; Leonardo Seeber; Richard Bopp; Marie-H. Cormier; Kazuko Usami Abstract The A.D. 2011 Tohoku-Oki M w 9 earthquake ruptured the megathrust up to the Japan Trench with a large displacement and caused a catastrophic tsunami. This study is the first to use short...
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Series: Geological Society, London, Special Publications
Published: 01 January 2012
DOI: 10.1144/SP361.1
EISBN: 9781862396098
... by the Fukushima nuclear power plant are broadcast to us daily. While it is true that the first reactor was completed there in 1971, an expert panel reviewed the plant's sesimic resistance in 2008 ( Normile 2011 ). By this time Japanese scientists were well aware of the Jogan tsunami of 869AD, an event...
Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 18 April 2018
Lithosphere (2018) 10 (4): 512–522.
... was the most active during the 2011 earthquake); and ( ii ) the Sanriku channel. Here we focus on the Tohoku-oki channel, which encompasses two important volcanic lineaments: ( i ) the Miyagi Volcanic Lineament in its northern extent; and ( ii ) the Fukushima Volcanic Lineament in its southern extent...
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Journal Article
Published: 01 February 2017
Earthquake Spectra (2017) 33 (1): 109–121.
...Figure 2. Seismometers installed at Fukushima Daiichi NPP, 2011 Tohoku-oki earthquake: Dense Surface Array (Left) and Unit 6 Reactor Building (right). (Figure reprinted from JAEE 2011c .) ...
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Journal Article
Published: 01 May 2013
Bulletin of the Seismological Society of America (2013) 103 (2B): 1473–1492.
... cause of this tsunami that made it so much larger than the design heights at the Fukushima and other NPSs ? In this study, we extend the data and method of Fujii et al. (2011) to further investigate the tsunami source of the 2011 Tohoku earthquake. Additional tsunami waveforms recorded at GPS...
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Journal Article
Published: 01 May 2013
Bulletin of the Seismological Society of America (2013) 103 (2B): 1584–1602.
...S. Toda; H. Tsutsumi Abstract The gigantic M w 9.0 11 March 2011 Tohoku‐oki earthquake suddenly changed the overriding inland area to an extensional stress regime and triggered massive seismic swarms in the coastal region. The largest earthquake of M w 6.6 struck southern Fukushima on 11 April 2011...
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Journal Article
Published: 01 May 2013
Bulletin of the Seismological Society of America (2013) 103 (2B): 1572–1583.
...Yo Fukushima; Youichiro Takada; Manabu Hashimoto Abstract After the 11 March 2011 M w 9.0 Tohoku earthquake, Japan, a swarm of shallow normal‐faulting earthquakes was triggered in a localized region beneath the border between Fukushima and Ibaraki prefectures in eastern Honshu. Here we examine...
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Journal Article
Published: 22 July 2020
Seismological Research Letters (2020) 91 (5): 2851–2861.
... coast shows that it successfully detects the tsunami from the 2016 Fukushima earthquake (M 7.4). The method was also applied to the extremely large tsunami from the 2011 Tohoku earthquake (M 9.0) and extremely small tsunami from the 1998 Sanriku earthquake (M 6.4). The algorithm detected the former huge...
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Comparison of long‐period  GMPE s and observed long‐period (a, c)  PGV s an...
Published: 12 January 2016
Figure 14. Comparison of long‐period GMPE s and observed long‐period (a, c) PGV s and (b, d) PGD s of a crustal earthquake (2011 Fukushima Hamadori, M w  6.7) and an interplate earthquake (2011 Iwate‐Oki, M w  6.7).
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Focal mechanisms of large shallow <span class="search-highlight">earthquakes</span> in the southeast <span class="search-highlight">Fukushima</span> an...
Published: 01 May 2013
Figure 1. Focal mechanisms of large shallow earthquakes in the southeast Fukushima and northern Ibaraki areas after the Tohoku‐oki ( M w  9) mainshock (F‐net catalog from NIED, depth ≤20  km, M j ≥4.0, 11 March 2011 to 10 August 2011), including the M w  6.6 11 April 2011 Iwaki earthquake
Journal Article
Published: 01 May 2013
Bulletin of the Seismological Society of America (2013) 103 (2B): 1348–1359.
...Hisashi Nakahara Abstract I study S ‐wave energy radiation in higher frequencies of 1–8 Hz from the 2011 M w 9.0 Off the Pacific Coast of Tohoku, Japan, earthquake (hereafter called the Tohoku‐Oki earthquake) based on a seismogram envelope inversion method. I first evaluate two medium parameters...
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Epicenters (black stars) and focal mechanisms of the <span class="search-highlight">2011</span> <span class="search-highlight">Fukushima</span> Hamador...
Published: 12 January 2016
Figure 13. Epicenters (black stars) and focal mechanisms of the 2011 Fukushima Hamadori ( M w  6.7), 2011 Iwate‐Oki ( M w  6.7), and 2013 Awaji ( M w  5.8) earthquakes. The focal mechanisms were obtained from the Global CMT project.
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Frequency histogram and cumulative frequency (solid line) of normalized ver...
Published: 01 October 2012
Figure 5. Frequency histogram and cumulative frequency (solid line) of normalized vertical displacements on the 11 April 2011 Hamadoori, Fukushima prefecture, northeast Japan, earthquake ruptures.
Journal Article
Published: 01 May 2013
Bulletin of the Seismological Society of America (2013) 103 (2B): 1373–1393.
...Susumu Kurahashi; Kojiro Irikura Abstract We have constructed a short‐period source model for the 2011 M w 9.0 Off the Pacific Coast of Tohoku earthquake using strong‐motion records at stations near the source fault. The observed strong motions contain five wavepackets that correspond to specific...
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Journal Article
Journal: Elements
Published: 01 June 2012
Elements (2012) 8 (3): 195–200.
...Anne Mathieu; Irène Korsakissok; Denis Quélo; Jérôme Groëll; Marilyne Tombette; Damien Didier; Emmanuel Quentric; Olivier Saunier; Jean-Pierre Benoit; Olivier Isnard Abstract On March 11, 2011, an earthquake and tsunami hit the northeast coast of Japan and damaged the Fukushima Daiichi nuclear...
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