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Relevant bibliographies by topics / Tohoku-Oki earthquakes

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Academic literature on the topic 'Tohoku-Oki earthquakes'

Author: Grafiati

Published: 6 September 2023

Last updated: 29 July 2025

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Journal articles on the topic "Tohoku-Oki earthquakes"

1

Nishikawa, T., T. Matsuzawa, K. Ohta, N. Uchida, T. Nishimura, and S. Ide. "The slow earthquake spectrum in the Japan Trench illuminated by the S-net seafloor observatories." Science 365, no. 6455 (2019): 808–13. http://dx.doi.org/10.1126/science.aax5618.

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Investigating slow earthquake activity in subduction zones provides insight into the slip behavior of megathrusts, which can provide important clues about the rupture extent of future great earthquakes. Using the S-net ocean-bottom seismograph network along the Japan Trench, we mapped a detailed distribution of tectonic tremors, which coincided with very-low-frequency earthquakes and a slow slip event. Compiling these and other related observations, including repeating earthquakes and earthquake swarms, we found that the slow earthquake distribution is complementary to the Tohoku-Oki earthquak

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2

Du, Cunpeng, Haitao Yin, Shengwen Yu, Le Yang, and Yuan Jia. "Effects of the 2011 Mw 9.0 Tohoku-Oki Earthquake on the Locking Characteristics and Seismic Risk of the Yishu Fault Zone in China." Sustainability 15, no. 5 (2023): 4321. http://dx.doi.org/10.3390/su15054321.

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To ascertain the 2011 Tohoku-Oki Mw 9.0 earthquake’s impact on the stability of the Yishu fault zone, this study inverts the fault locking degree and slip rate defect distribution of the Yishu fault zone using GPS horizontal velocity field data covering the period from 1999 to 2009 and from April 2011 to 2019. This is based on the block negative dislocation model. Combined with the b value and strain field characteristics, the properties of deformation of the Yishu fault zone before and after the earthquake are comprehensively analyzed. The results show that before the 2011 Tohoku-Oki Mw 9.0 e

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Okawa, Izuru, Toshihide Kashima, Shin Koyama, and Masanori Iiba. "Recorded Responses of Building Structures during the 2011 Tohoku-Oki Earthquake with Some Implications for Design Practice." Earthquake Spectra 29, no. 1_suppl (2013): 245–64. http://dx.doi.org/10.1193/1.4000130.

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During the 2011 Tohoku-oki earthquake, a large number of response records from various types of buildings were obtained. The records give us the actual motions of buildings during the exceptionally large earthquakes that are considered comparable with design earthquakes. Various types of earthquake response records have been collected, and their properties with several buildings that will exhibit implications for structural design are discussed.

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4

Tao, Zheng Ru, Xia Xin Tao, and Wei Jiang. "A Review on Long-Term Evaluation of Occurrence Probability for Subduction-Zone Earthquakes in Eastern Japan." Applied Mechanics and Materials 166-169 (May 2012): 2190–96. http://dx.doi.org/10.4028/www.scientific.net/amm.166-169.2190.

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Evaluation approach of occurrence probability for subduction-zone earthquakes adopted in “National Seismic Hazard Maps for Japan” is reviewed, especially for the area of the 2011 off the Pacific coast of Tohoku Earthquake (2011 Tohoku Earthquake in short). One problem is pointed that the occurrence probability of such a large earthquake cannot be predicted just from seismicity in a region small like Miyagi-ken-Oki area or southern Sanriku-Oki. The whole subduction zone in eastern Japan is suggested to be taken into account with the interaction between the energy released in quakes. Finally, a

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5

Suito, Hisashi. "Current Status of Postseismic Deformation Following the 2011 Tohoku-Oki Earthquake." Journal of Disaster Research 13, no. 3 (2018): 503–10. http://dx.doi.org/10.20965/jdr.2018.p0503.

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Postseismic deformation following the 2011 Tohoku-Oki earthquake has been observed by the Global Navigation Satellite System (GNSS) Earth Observation Network System (GEONET) and the Seafloor Geodetic Observation (SGO) over the past six and half years. Observed deformation at onshore sites exceeds 140 cm horizontally, there is uplift of 50 cm, and deformation tends eastward. However, offshore sites reveal complex patterns ranging from near-zero deformation in the northern part of Iwate-Oki, to westward in the southern part of Iwate-Oki, Miyagi-Oki, and the northern part of Fukushima-Oki regions

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Tong, P., D. Zhao, and D. Yang. "Tomography of the 2011 Iwaki earthquake (M 7.0) and Fukushima nuclear power plant area." Solid Earth Discussions 3, no. 2 (2011): 1021–36. http://dx.doi.org/10.5194/sed-3-1021-2011.

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Abstract. High resolution tomographic images of the crust and upper mantle in and around the area of the 2011 Iwaki earthquake (M 7.0) and the Fukushima nuclear power plant are determined by inverting a large number of high-quality arrival times with both the finite-frequency and ray tomography methods. The Iwaki earthquake and its aftershocks mainly occurred in a boundary zone with strong variations in seismic velocity and Poisson's ratio. Prominent low-velocity and high Poisson's ratio zones are revealed under the Iwaki source area and the Fukushima nuclear power plant, which may reflect flu

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Tong, P., D. Zhao, and D. Yang. "Tomography of the 2011 Iwaki earthquake (M 7.0) and Fukushima nuclear power plant area." Solid Earth 3, no. 1 (2012): 43–51. http://dx.doi.org/10.5194/se-3-43-2012.

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Abstract. High-resolution tomographic images of the crust and upper mantle in and around the area of the 2011 Iwaki earthquake (M 7.0) and the Fukushima nuclear power plant are determined by inverting a large number of high-quality arrival times with both the finite-frequency and ray tomography methods. The Iwaki earthquake and its aftershocks mainly occurred in a boundary zone with strong variations in seismic velocity and Poisson's ratio. Prominent low-velocity and high Poisson's ratio zones are revealed under the Iwaki source area and the Fukushima nuclear power plant, which may reflect flu

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Kasai, Kazuhiko, Akira Mita, Haruyuki Kitamura, Kazuhiro Matsuda, Troy A. Morgan, and Andrew W. Taylor. "Performance of Seismic Protection Technologies during the 2011 Tohoku-Oki Earthquake." Earthquake Spectra 29, no. 1_suppl (2013): 265–93. http://dx.doi.org/10.1193/1.4000131.

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Many buildings in the Tohoku and Kanto area were strongly shaken during the Tohoku-oki earthquake on 11 March 2011. Soon after the earthquake, the Japan Society of Seismic Isolation (JSSI) established committees to investigate the performance of structures where modern seismic protection methods were used. Since response-control technologies are relatively new, few systems had been validated with actual earthquakes. Generally, the various buildings performed well, and there were no failures of superstructures of base-isolated or supplementally damped buildings. Failures of numerous expansion j

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Shibazaki, Bunichiro, and Hiroyuki Noda. "What Caused the 2011 Tohoku-Oki Earthquake? : Effects of Dynamic Weakening." Journal of Disaster Research 9, no. 3 (2014): 252–63. http://dx.doi.org/10.20965/jdr.2014.p0252.

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Some observational studies have suggested that the 2011 great Tohoku-Oki earthquake (Mw9.0) released a large portion of the accumulated elastic strain on the plate interface owing to considerable weakening of the fault. Recent experimental and theoretical studies have shown that considerable dynamic weakening can occur at high slip velocities because of thermal pressurization or thermal weakening processes. This paper reviews severalmodels of the generation of megathrust earthquakes along the Japan Trench subduction zone, that considers thermal pressurization or a friction law that exhibits ve

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Hashimoto, Manabu. "Crustal Deformation Associated with the 2011 Tohoku-Oki Earthquake: An Overview." Earthquake Spectra 29, no. 1_suppl (2013): 81–98. http://dx.doi.org/10.1193/1.4000117.

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The 2011 Tohoku-oki earthquake generated large displacements in and around the Japanese islands that were detected by the nationwide GPS network, sea-floor geodetic surveys, and space-borne radars. The east-west extension exerted on the Japanese islands by this event induced inland events of Mw6 or larger earthquakes. Coseismic subsidence of up to 1 m was observed along the coast where subsidence was found during the interseismic period. This observation contradicts expectations based on the concept of the recurrence of inter-plate earthquakes. Therefore, postseismic motions or other large eve

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Dissertations / Theses on the topic "Tohoku-Oki earthquakes"

1

Kubo, Hisahiko. "Study on rupture processes of large interplate earthquakes estimated by fully Bayesian source inversions using multi period-band strong-motion data －The 2011 Tohoku-oki and the 2011 Ibaraki-oki earthquakes－." 京都大学 (Kyoto University), 2015. http://hdl.handle.net/2433/199110.

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Scala, Antonio <1985&gt. "Rupture Dynamics Along Subduction Zones: Structural and Geometrical Complexities and the Case of Tohoku-Oki Earthquake." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2016. http://amsdottorato.unibo.it/7489/1/Thesis_Antonio_Scala.pdf.

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We aim to characterize the rupture dynamics along the subduction zones. We investigated the shear/normal stress coupling when geometrical discontinuities and/or realistic velocity fields induce normal traction perturbations. The Spectral Element Method (SEM) is shown to be a powerful numerical tool to perform dynamic simulations for subduction earthquakes due to its geometrical flexibility and to the easy implementation of classical seismological boundary conditions. Sharp variations of normal stress are induced when a rupture propagates between dissimilar materials. Performing dynamic simul

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Scala, Antonio <1985&gt. "Rupture Dynamics Along Subduction Zones: Structural and Geometrical Complexities and the Case of Tohoku-Oki Earthquake." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2016. http://amsdottorato.unibo.it/7489/.

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We aim to characterize the rupture dynamics along the subduction zones. We investigated the shear/normal stress coupling when geometrical discontinuities and/or realistic velocity fields induce normal traction perturbations. The Spectral Element Method (SEM) is shown to be a powerful numerical tool to perform dynamic simulations for subduction earthquakes due to its geometrical flexibility and to the easy implementation of classical seismological boundary conditions. Sharp variations of normal stress are induced when a rupture propagates between dissimilar materials. Performing dynamic simul

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4

Hidayat, Panuntun. "Poroelastic rebound following the 2011 Tohoku-oki earthquake (Mw=9.0) as deduced from geodetic data and its application to infer the Poisson's ratio." Kyoto University, 2019. http://hdl.handle.net/2433/242618.

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Shrivastava, Mahesh N. "Estimation of strain distribution of the seismogenic regions of india,from gps measurements: numerical modeling,interpretations and implications." Thesis, 2010. http://localhost:8080/xmlui/handle/123456789/1579.

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Sun, Tianhaozhe. "Crustal deformation associated with great subduction earthquakes." Thesis, 2017. https://dspace.library.uvic.ca//handle/1828/8372.

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The slip behaviour of subduction faults and the viscoelastic rheology of Earth’s mantle govern crustal deformation throughout the subduction earthquake cycle. This Ph.D. dissertation presents research results on two topics: (1) coseismic and postseismic slip of the shallowest segment of subduction faults and (2) postseismic deformation following great subduction earthquakes controlled by mantle viscoelasticity. Topic 1: Slip behaviour of the shallowest subduction faults. By modelling high-resolution cross-trench bathymetry surveys before and after the 2011 Mw 9.0 Tohoku-oki earthquake, we det

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Brown, Lonn. "Strength of Megathrust Faults: Insights from the 2011 M=9 Tohoku-oki Earthquake." Thesis, 2015. http://hdl.handle.net/1828/6581.

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The state of stress in forearc regions depends on the balance of two competing factors: the plate coupling force that generates margin-normal compression, and the gravitational force, that generates margin-normal tension. Widespread reversal of the focal mechanisms of small earthquakes after the 2011 Tohoku-oki earthquake indicate a reversal in the dominant state of stress of the forearc, from compressive before the earthquake to tensional afterwards. This implies that the plate coupling force dominated before the earthquake, and that the coseismic weakening of the fault lowered the amount of

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Zannat, Umma Jamila. "Network Effect in Geocentre Motion." Phd thesis, 2019. http://hdl.handle.net/1885/157069.

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Geocentre motion is the motion of the centre of mass of the Earth system with respect to the geometric centre of figure of the solid Earth surface because of the continual deformation of the Earth by geophysical processes. This motion is important both in theory and in practice to understand and interpret various mass transport phenomena and their consequences, such as sea level rise, postseismic relaxation, polar ice melting, and glacial isostatic adjustment. Global reference frames for space geodetic point positioning are

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Books on the topic "Tohoku-Oki earthquakes"

1

Gakkai, Nihon Kenchiku. Preliminary Reconnaissance Report of the 2011 Tohoku-Chiho Taiheiyo-Oki Earthquake. Springer Japan, 2012.

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2

Japan. Shōbōchō. Shōbō Kenkyū Sentā. Heisei 23-nen (2011-nen) Tohoku chihō Taiheiyō oki jishin no higai oyobi shōbō katsudō ni kansuru chōsa hōkokusho. Shōbōchō Shōbō Kenkyū Sentā, 2011.

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3

Kokudo Gijutsu Seisaku Sōgō Kenkyūjo (Japan). Heisei 23-nen (2011-nen) Tōhoku chihō Taiheiyō oki jishin doboku shisetsu saigai chōsa sokuhō =: Quick report on damage to infrastructures by the 2011 off the Pacific Coast of Tohoku earthquake. Kokudo Gijutsu Seisaku Sōgō Kenkyūjo, 2011.

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4

Hakubutsukan, Iwate Kenritsu. Iwate-ken ni okeru Tōhoku chihō Taiheiyō oki jishin hisai bunkazai tō no saisei e muketa torikumi: Hisai kara 3-nenme ni okeru seika to kadai = Effort to salvage and preserve cultural properties and natural history collections damaged by 2011 Tohoku Earthquake and Tsunami in Iwate Prefecture. Iwate Kenritsu Hakubutsukan, 2014.

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5

Preliminary Reconnaissance Report of the 2011 Tohoku-Chiho Taiheiyo-Oki Earthquake. Springer Japan, 2012. http://dx.doi.org/10.1007/978-4-431-54097-7.

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Japan, Architectural Institute of. Preliminary Reconnaissance Report of the 2011 Tohoku-Chiho Taiheiyo-Oki Earthquake. Springer Japan, 2016.

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Book chapters on the topic "Tohoku-Oki earthquakes"

1

Ohta, Yusaku, Tatsuya Kobayashi, Ryota Hino, Tomotsugu Demachi, and Satoshi Miura. "Rapid Coseismic Fault Determination of Consecutive Large Interplate Earthquakes: The 2011 Tohoku-Oki Sequence." In International Association of Geodesy Symposia. Springer International Publishing, 2015. http://dx.doi.org/10.1007/1345_2015_109.

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2

Gupta, Harsh K., and Vineet K. Gahalaut. "2011 Tohoku-Oki Earthquake and Tsunami." In SpringerBriefs in Earth Sciences. Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-94-007-6576-4_4.

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3

Kawase, Hiroshi, Shinchi Matsushima, Baoyintu, et al. "Earthquake, Geology, and Tsunami." In Preliminary Reconnaissance Report of the 2011 Tohoku-Chiho Taiheiyo-Oki Earthquake. Springer Japan, 2012. http://dx.doi.org/10.1007/978-4-431-54097-7_2.

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4

Chen, Kejie, Rongxin Fang, Min Li, and Chuang Shi. "The Impact of Tohoku-Oki Earthquake on “CMONOC” Stations." In Lecture Notes in Electrical Engineering. Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-29187-6_29.

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Koshihara, Mikio, Reiji Tanaka, Junji Ogawa, Ryota Yamaya, and Yukihiro Take. "Outline of Investigation and Damage." In Preliminary Reconnaissance Report of the 2011 Tohoku-Chiho Taiheiyo-Oki Earthquake. Springer Japan, 2012. http://dx.doi.org/10.1007/978-4-431-54097-7_1.

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Tokimatsu, Kohji, Shuji Tamura, Hiroko Suzuki, and Kota Katsumata. "Damage to Soils and Foundation." In Preliminary Reconnaissance Report of the 2011 Tohoku-Chiho Taiheiyo-Oki Earthquake. Springer Japan, 2012. http://dx.doi.org/10.1007/978-4-431-54097-7_10.

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Hiraishi, Hisahiro. "Summary." In Preliminary Reconnaissance Report of the 2011 Tohoku-Chiho Taiheiyo-Oki Earthquake. Springer Japan, 2012. http://dx.doi.org/10.1007/978-4-431-54097-7_11.

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Kawai, Naohito, Hiroshi Isoda, and Takahiro Tsuchimoto. "Damage to Timber Buildings." In Preliminary Reconnaissance Report of the 2011 Tohoku-Chiho Taiheiyo-Oki Earthquake. Springer Japan, 2012. http://dx.doi.org/10.1007/978-4-431-54097-7_3.

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Kabeyasawa, Toshimi, Yoshiaki Nakano, Masaki Maeda, et al. "Damages to Reinforced Concrete Buildings." In Preliminary Reconnaissance Report of the 2011 Tohoku-Chiho Taiheiyo-Oki Earthquake. Springer Japan, 2012. http://dx.doi.org/10.1007/978-4-431-54097-7_4.

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Kawano, Akihiko, Junichi Sakai, Mareyasu Doi, Hiroshi Kuramoto, Takashi Fujinaga, and Teruhisa Tanaka. "Damage to Steel Reinforced Concrete Buildings." In Preliminary Reconnaissance Report of the 2011 Tohoku-Chiho Taiheiyo-Oki Earthquake. Springer Japan, 2012. http://dx.doi.org/10.1007/978-4-431-54097-7_5.

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Conference papers on the topic "Tohoku-Oki earthquakes"

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Abdolali, A., James T. Kirby, Giorgio Bellotti, S. Grilli, and J. C. Harris. "Hydro-Acoustic Wave Generation during the Tohoku-Oki 2011 Earthquake." In Coastal Structures and Solutions to Coastal Disasters Joint Conference 2015. American Society of Civil Engineers, 2017. http://dx.doi.org/10.1061/9780784480311.003.

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2

Hino, Ryota, Yoshihiro Ito, Yusaku Ohta, Takeshi Iinuma, and Daisuke Inazu. "Ocean bottom pressure records of the 2011 Tohoku-Oki earthquake." In Proceedings of the 11th SEGJ International Symposium, Yokohama, Japan, 18-21 November 2013. Society of Exploration Geophysicists, 2013. http://dx.doi.org/10.1190/segj112013-117.

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Shang, Tao, Zhengru Tao, Baihui Zhu, and Xiaxin Tao. "Validity of Quarter-wavelength Approximation In the case of Tohoku-oki earthquake." In 2015 3rd International Conference on Advances in Energy and Environmental Science. Atlantis Press, 2015. http://dx.doi.org/10.2991/icaees-15.2015.38.

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Yoshida, Keisuke, Akira Hasegawa, Tomomi Okada, et al. "Stress fields in NE Japan before and after the 2011 Tohoku-oki Earthquake." In Proceedings of the 11th SEGJ International Symposium, Yokohama, Japan, 18-21 November 2013. Society of Exploration Geophysicists, 2013. http://dx.doi.org/10.1190/segj112013-126.

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Ito, Takeo, Syota Suzuki, Kachishige Sato, and Mamoru Hyodo. "Spatio-temporal afterslip distribution following the 2011 Tohoku-Oki earthquake using 3D viscoelastic green’s functions." In INTERNATIONAL SYMPOSIUM ON EARTH HAZARD AND DISASTER MITIGATION (ISEDM) 2017: The 7th Annual Symposium on Earthquake and Related Geohazard Research for Disaster Risk Reduction. Author(s), 2018. http://dx.doi.org/10.1063/1.5047341.

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Park, Sang-Hoon, and Seok-Woo Hong. "Coseismic geoid height changes of the 2011 Tohoku-Oki earthquake in GRACE monthly gravity data." In Workshop on Architecture and Civil Engineering 2013 Second. Science & Engineering Research Support soCiety, 2013. http://dx.doi.org/10.14257/astl.2013.32.11.

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Tomita, Fumiaki, Yusaku Ohta, Takeshi Iinuma, Ryota Hino, Motovuki Kido, and Naoki Uchida. "Seafloor Geodetic Observations to Reveal Co- and Post-Seismic Slip Distributions of the 2011 Tohoku-Oki Earthquake." In 2018 OCEANS - MTS/IEEE Kobe Techno-Ocean (OTO). IEEE, 2018. http://dx.doi.org/10.1109/oceanskobe.2018.8559370.

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Ito, Yoshihiro, and Ryota Hino. "Velocity reduction in an offshore region after the 2011 Tohoku-Oki earthquake, revealed from ocean-bottom seismic records." In Proceedings of the 11th SEGJ International Symposium, Yokohama, Japan, 18-21 November 2013. Society of Exploration Geophysicists, 2013. http://dx.doi.org/10.1190/segj112013-131.

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Takagi, Ryota, Tomomi Okada, Toshio Kono, and Akira Hasegawa. "Monitoring of seismic velocity structure before and after the 2011 Tohoku-Oki earthquake using array observation of ambient noise." In Proceedings of the 11th SEGJ International Symposium, Yokohama, Japan, 18-21 November 2013. Society of Exploration Geophysicists, 2013. http://dx.doi.org/10.1190/segj112013-115.

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Fujihara, Satoru, Kaoru Kawaji, Mariko Korenaga, and Shinichi Akiyama. "Source Model of 2011 Tohoku-Oki Earthquake Estimated from Seismic Waveform Inversion Considering 3-D Inhomogeneity of Underground Structure." In Proceedings of the 11th SEGJ International Symposium, Yokohama, Japan, 18-21 November 2013. Society of Exploration Geophysicists, 2013. http://dx.doi.org/10.1190/segj112013-125.

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Reports on the topic "Tohoku-Oki earthquakes"

1

Si, Hongjun, Saburoh Midorikawa, and Tadahiro Kishida. Development of NGA-Sub Ground-Motion Model of 5%-Damped Pseudo-Spectral Acceleration Based on Database for Subduction Earthquakes in Japan. Pacific Earthquake Engineering Research Center, University of California, Berkeley, CA, 2020. http://dx.doi.org/10.55461/lien3652.

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Presented within is an empirical ground-motion model (GMM) for subduction-zone earthquakesin Japan. The model is based on the extensive and comprehensive subduction database of Japanese earthquakes by the Pacific Engineering Research Center (PEER). It considers RotD50 horizontal components of peak ground acceleration (PGA), peak ground velocity (PGV), and 5%-damped elastic pseudo-absolute acceleration response spectral ordinates (PSA) at the selected periods ranging from 0.01 to 10 sec. The model includes terms and predictor variables considering tectonic setting (i.e., interplate and intrasla

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Plourde, A. P., and J. F. Cassidy. Mapping tectonic stress at subduction zones with earthquake focal mechanisms: application to Cascadia, Japan, Nankai, Mexico, and northern Chile. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/330943.

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Earthquake focal mechanisms have contributed substantially to our understanding of modern tectonic stress regimes, perhaps more than any other data source. Studies generally group focal mechanisms by epicentral location to examine variations in stress across a region. However, stress variations with depth have rarely been considered, either due to data limitations or because they were believed to be negligible. This study presents 3D grids of tectonic stress tensors using existing focal mechanism catalogs from several subduction zones, including Cascadia, Japan, Nankai, Mexico, and northern Ch

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