Compre online Spatial Economic Modelling of Megathrust Earthquake in Japan: Impacts, Reconstruction, and Regional Revitalization: 11, de Tokunaga, Suminori, Resosudarmo, Budy P. na Amazon. Geol Soc Am Bull 93:829â846, Wessel P, Smith WHF (1998) New, improved version of the generic mapping tools released. J Geophys Res 117:B01404. Analyzes the impacts of the Great East Japan and Nankai megathrust earthquakes using a new economic geography model and shows the predicted labor distribution Analyzes the economic impact of the Indian Ocean tsunami generated by the SumatraâAndaman earthquake of 2004 and assesses the subsequent disaster management process In Northeast Japan, it remains a puzzle to reconcile the mismatch between long-term (geological) uplift and late-interseismic and coseismic subsidence associated with the 2011 Tohoku earthquake. A Hikurangi megathrust quake the same strength as the one that hit Japan would release more than 11,000 times the energy of the 2011 Christchurch quake. Anyone who has experienced an earthquake in Japan knows that most are barely noticeable and last only a few seconds.There are approximately 5,000 minor earthquakes recorded in Japan per year, with more than half measured between 3.0 and 3.9.Thus, most go unnoticed by people. Baba AK, Matsuda T, Itaya T, Wada Y, Hori N, Yokoyama M, Eto N, Kamei R, Zaman H, Kidane T, Otofuji Y (2007) New age constraints on counter-clockwise rotation of NE Japan. Frete GRÁTIS em milhares de produtos com o Amazon Prime. Tectonophysics 97:183â200, Koike K, Machida H (2001) Atlas of Quaternary marine terraces in the Japanese Islands (in Japanese). doi:10.1029/2011GL048701, Yamagiwa S, Miyazaki S, Hirahara K, Fukahata Y (2015) Afterslip and viscoelastic relaxation following the 2011 Tohoku-oki earthquake (Mw9.0) inferred from inland GPS and seafloor GPS/Acoustic data. "What Have Religious Groups Done After 3.11? https://doi.org/10.1186/s40623-017-0606-6, DOI: https://doi.org/10.1186/s40623-017-0606-6. (duration of tectonic erosion), this effect can explain about half of the observed data. In northeastern Japan, aseismic slip occurs in the form of decelerating afterslip after large interplate earthquakes and as relatively steady slip on uncoupled areas of the subduction thrust. Earth Planets Space 63:631â636. PhD Thesis, Univ Tokyo, Suito H, Nishimura T, Tobita M, Imakiire T, Ozawa S (2011) Interplate fault slip along the Japan Trench before the occurrence of the 2011 off the Pacific coast of Tohoku Earthquake as inferred from GPS data. It was one of the largest in earthâs hâ¦ Numerical Investigation of Controls on Megathrust Earthquakes Along the Japan Trench Subduction Zone. J Geophys Res 118:6183â6202. Chikyu Monthly 25:125â129, Ikeda Y (2014) Strain buildup in the Northeast Japan orogen with implications for gigantic subduction earthquakes. Earthquake Research Institute, University of Tokyo, Yayoi 1-1-1, Bunkyo-ku, Tokyo, 113-0032, Japan, Department of Earth Sciences, Graduate School of Science, Chiba University, Chiba, 263-8522, Japan, You can also search for this author in As shown in Fig. Offshore observations obtained by both geodetic and geological methods could be important constraints on our earthquake cycle model. We hear a lot about the next Megathrust Earthquake, or âBig Oneâ that BC is due to experience. Science 313:1281â1284, Shibazaki B, Garatani K, Iwasaki T, Tanaka A, Ito Y (2008) Faulting processes controlled by the nonuniform thermal structure of the crust and uppermost mantle beneath the northeastern Japanese island arc. To access whether these earthquakes might trigger the eruption, we calculated the stress and â¦ Crustal deformation by the M w 9.0 megathrust Tohoku earthquake causes the extension over a wide region of the Japanese mainland. Shibusawa, Hiroyuki. A megathrust earthquake occurs at subduction zones at destructive convergent plate boundaries, where one tectonic plate is forced underneath another. Metadata AH performed the computations and prepared the manuscript. doi:10.1002/2015GL064167, Sharp WD, Clague DA (2006) 50-Ma initiation of Hawaiian-Emperor bend records major change in Pacific plate motion. We are grateful to Anne D. Van Horne for her constructive comments and grammatical correction. Here we report on a previously unrecognized quasi-periodic slow-slip behavior that is widespread in the megathrust zone. By using this website, you agree to our These interplate earthquakes are the planet's most powerful, with moment magnitudes (M w) that can exceed 9.0.Since 1900, all earthquakes of magnitude 9.0 or greater have been megathrust earthquakesâ¦ The Kobe earthquake was right beneath the city and the megathrust earthquake will be about 150 kilometres from Vancouver. 2010 Mw 8.8 Chile Earthquake Zisin (J Seismol Soc Japan) 36:541â550, Muto J, Shibazaki B, Iinuma T, Ito Y, Ohta Y, Miura S, Nakai Y (2016) Heterogeneous rheology controlled postseismic deformation of the 2011 Tohoku-Oki earthquake. Geol Soc Am Bull 102:704â720, von Huene R, Langseth M, Nasu N, Okuda H (1982) A summary of Cenozoic tectonic history along the IPOD Japan Trench transect. Part 1: A Brief Survey of Religious Mobilization after the Great East Japan Earthquake Disasters". "-Did you hear the 2011 earthquake? Earth Planet Sci Lett 459:279â290. Spatial Economic Modelling Of Megathrust Earthquake In Japan è un libro di Tokunaga Suminori (Curatore), Resosudarmo Budy P. (Curatore) edito da Springer a gennaio 2018 - EAN 9789811064920: puoi acquistarlo sul sito HOEPLI.it, la â¦ Pages 289-311. Evidence from the Great East Japan Earthquake", "Energy and resilience: The effects of endogenous interdependencies on trade network formation across space among major Japanese firms", Fault that Caused Japan's 2011 Earthquake is Thin and Slippery. PubMedÂ Google Scholar. With spaceborne interferometric synthetic aperture radar (InSAR) analysis, we found that two recent megathrust earthquakes, the 2011 Mw 9.0 Tohoku earthquake in Japan (March 11, 2011) and the 2010 Mw 8.8 Maule earthquake in Chile (February 27, 2010), have triggered unprecedented subsidence of multiple volcanoes. Int Assoc Geod Symp 145:73â78. Quat Res 71:227â238, Mavrommatis AP, Segall P, Johnson KJ (2014) A decadal-scale deformation transient prior to the 2011 Mw 9.0 Tohoku-oki earthquake. doi:10.1029/2011JB008355, Otofuji Y, Matsuda T, Nohda S (1985) Opening mode of the Japan Sea inferred from the palaeomagnetism of the Japan Arc. Slow-slip events occurred every 1 to 6 years and frequently were correlated with large earthquakes, including the great 2011 Tohoku-oki earthquake. J Disaster Res 9:294â302, Nishimura T, Hirasawa T, Miyazaki S, Sagiya T, Tada T, Miura S, Tanaka K (2004) Temporal change of interplate coupling in northeastern Japan during 1995â2002 estimated from continuous GPS observations. Megathrust earthquakes occur at subduction zones at destructive convergent plate boundaries, where one tectonic plate is forced underneath another. e The study constructs three models of these megathrust earthquakes and the associated tsunami. Around the Pacific Ocean is a horseshoe shaped area that contains subduction zones that create megathrust earthquakes and generate tsunamis. Geophys Res Lett 38:L19307. show that very large (M 8.5+) earthquakes preferentially rupture planar, or flat (low-curvature) megathrust interfaces; they do this highlighting a spatial correlation between the rupture areas of such earthquakes, with the gradient of subduction zone dip (âflatnessâ, or âplanarityâ) calculated from the Slab1.0 subduction zone â¦ A study reported in 2016 found that the largest megathrust quakes are associated with downgoing slabs with the shallowest dip, so-called "flat slab subduction". This page was last edited on 3 January 2021, at 23:20. Large interplate megathrust earthquakes occurred in the Nankai subduction zone off Southwest Japan with an interval of ~100 to 150 years. The size of circles and stars is scaled with the earthquake â¦ An NEG Analysis of Megathrust Earthquakes in Japan. doi:10.1029/2007JB005361, Shibazaki B, Okada T, Muto J, Matsumoto T, Yoshida T, Yoshida K (2016) Heterogeneous stress state of island arc crust in northeastern Japan affected by hot mantle fingers. All authors read and approved the final manuscript. e Read "Spatial Economic Modelling of Megathrust Earthquake in Japan Impacts, Reconstruction, and Regional Revitalization" by available from Rakuten Kobo. 2016).