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Supply Chain Disruptions: Evidence from the Great East Japan Earthquake∗
Supply Chain Disruptions: Evidence from the Great East Japan Earthquake∗ Vasco M. Carvalhoy Makoto Nireiz Yukiko U. Saitox Alireza Tahbaz-Salehi{ June 2020 Abstract Exploiting the exogenous and regional nature of the Great East Japan Earthquake of 2011, this paper provides a quantification of the role of input-output linkages as a mechanism for the prop- agation and amplification of shocks. We document that the disruption caused by the disaster propagated upstream and downstream supply chains, affecting the direct and indirect suppliers and customers of disaster-stricken firms. Using a general equilibrium model of production net- works, we then obtain an estimate for the overall macroeconomic impact of the disaster by taking these propagation effects into account. We find that the earthquake and its aftermaths resulted in a 0:47 percentage point decline in Japan’s real GDP growth in the year following the disaster. ∗We thank the co-editor and four anonymous referees for helpful comments and suggestions. We thank Hirofumi Okoshi and Francisco Vargas for excellent research assistance. We are also grateful to Daron Acemoglu, Pol Antras,` David Baqaee, Paula Bustos, Lorenzo Caliendo, Arun Chandrasekhar, Ryan Chahrour, Giancarlo Corsetti, Ian Dew-Becker, Masahisa Fujita, Julian di Giovanni, Sanjeev Goyal, Adam Guren, Matt Jackson, Jennifer La’O, Glenn Magerman, Isabelle Mejean,´ Ameet Morjaria, Kaivan Munshi, Michael Peters, Aureo de Paula, Jacopo Ponticelli, Farzad Saidi, Adam Szeidl, Edoardo Teso, Yasuyuki Todo, Aleh Tsyvinski, Liliana Varela, Andrea Vedolin, Jaume Ventura, Jose Zubizarreta, and numerous seminar and conference participants for useful feedback and suggestions. We also thank the Center for Spatial Information Science, University of Tokyo for providing us with the geocoding service. -
Constraints on the Moho in Japan and Kamchatka
Tectonophysics 609 (2013) 184–201 Contents lists available at ScienceDirect Tectonophysics journal homepage: www.elsevier.com/locate/tecto Review Article Constraints on the Moho in Japan and Kamchatka Takaya Iwasaki a, Vadim Levin b,⁎, Alex Nikulin b, Takashi Iidaka a a Earthquake Research Institute, University of Tokyo, Japan b Rutgers University, NJ, USA article info abstract Article history: This review collects and systematizes in one place a variety of results which offer constraints on the depth Received 1 July 2012 and the nature of the Moho beneath the Kamchatka peninsula and the islands of Japan. We also include stud- Received in revised form 12 November 2012 ies of the Izu–Bonin volcanic arc. All results have already been published separately in a variety of venues, and Accepted 22 November 2012 the primary goal of the present review is to describe them in the same language and in comparable terms. Available online 3 December 2012 For both regions we include studies using artificial and natural seismic sources, such as refraction and reflec- tion profiling, detection and interpretation of converted-mode body waves (receiver functions), surface wave Keywords: Kamchatka dispersion studies (in Kamchatka) and tomographic imaging (in Japan). The amount of work done in Japan is Japan significantly larger than in Kamchatka, and resulting constraints on the properties of the crust and the upper- Crustal structure most mantle are more detailed. Upper-mantle structure Japan and Kamchatka display a number of similarities in their crustal structure, most notably the average Moho crustal thickness in excess of 30 km (typical of continental regions), and the generally gradational nature of the crust–mantle transition where volcanic arcs are presently active. -
Table S1. Summary of Kayen Et Al
Table S1. Summary of Kayen et al. (2013) Vs liquefaction case history data Data Crit. Depth Depth to γ (kN/m3) site ID LOCATION Liquefied? total CSR MSF ϕ (°) ORIGINAL SITE REFERENCE Mw GWT (m) σvo (kPa) σ'vo (kPa) amax (g) rd VS1 (m/sec) VS (m/sec) CRRPL=15% Gmax (kPa) Ko σ' mo (kPa) Point Range (m) Above gwt Below gwt 1906 San Francisco Earthquake, California, USA 5 9001 Coyote Valley 7.7 ± 0.10 YES 3.5 - 6 2.4 77.08 ± 8.53 54.03 ± 5.41 15.10 17.30 0.36 ± 0.09 0.89 ± 0.09 0.30 ± 0.09 0.97 171.98 ± 2.00 146.97 0.13 38093 30 0.500 36.02 Barrow, 1983 6 9002 Salinas River North 7.7 ± 0.10 NO 9.1 - 10.6 6.0 155.24 ± 8.31 117.47 ± 6.09 14.00 18.50 0.32 ± 0.08 0.68 ± 0.16 0.19 ± 0.07 0.97 172.05 ± 5.84 178.54 0.13 60113 34 0.441 73.68 Barrow, 1983 1948 Fukui Earthquake, Japan 9 118 HINO GAWA EAST BANK, FUKUI PREF. EQUESTRIAN CENTER, 7.1 ± 0.12 YES 6.0 - 10 1.0 143.50 ± 14.15 74.83 ± 8.10 17.30 18.00 0.50 ± 0.13 0.64 ± 0.14 0.40 ± 0.14 1.08 142.28 ± 17.04 131.91 0.10 31926 30 0.500 49.89 Office of the Engineer (1949); Hamada et al. (1992); This study 10 103 MORITA-CHO GAKKU, HAMADA ET AL. -
Large and Repeating Slow Slip Events in the Izu-Bonin Arc from Space
LARGE AND REPEATING SLOW SLIP EVENTS IN THE IZU-BONIN ARC FROM SPACE GEODETIC DATA (伊豆小笠原弧における巨大スロー地震および繰り返し スロー地震の宇宙測地学的研究) by Deasy Arisa Department of Natural History Sciences Graduate School of Science, Hokkaido University September, 2016 Abstract The Izu-Bonin arc lies along the convergent boundary where the Pacific Plate subducts beneath the Philippine Sea Plate. In the first half of my three-year doctoral course, I focused on the slow deformation on the Izu Islands, and later in the second half, I focused on the slow deformation on the Bonin Islands. The first half of the study, described in Chapter V, is published as a paper, "Transient crustal movement in the northern Izu–Bonin arc starting in 2004: A large slow slip event or a slow back-arc rifting event?". Horizontal velocities of continuous Global Navigation Satellite System (GNSS) stations on the Izu Islands move eastward by up to ~1 cm/year relative to the stable part of the Philippine Sea Plate suggesting active back-arc rifting behind the northern part of the arc. We confirmed the eastward movement of the Izu Islands explained by Nishimura (2011), and later discussed the sudden accelerated movement in the Izu Islands detected to have occurred in the middle of 2004. I mainly discussed this acceleration and make further analysis to find out the possible cause of this acceleration. Here I report that such transient eastward acceleration, starting in the middle of 2004, resulted in ~3 cm extra movements in three years. I compare three different mechanisms possibly responsible for this transient movement, i.e. (1) postseismic movement of the 2004 September earthquake sequence off the Kii Peninsula far to the west, (2) a temporary activation of the back-arc rifting to the west dynamically triggered by seismic waves from a nearby earthquake, and (3) a large slow slip event in the Izu-Bonin Trench to the east. -
Philippine Sea Plate Inception, Evolution, and Consumption with Special Emphasis on the Early Stages of Izu-Bonin-Mariana Subduction Lallemand
Progress in Earth and Planetary Science Philippine Sea Plate inception, evolution, and consumption with special emphasis on the early stages of Izu-Bonin-Mariana subduction Lallemand Lallemand Progress in Earth and Planetary Science (2016) 3:15 DOI 10.1186/s40645-016-0085-6 Lallemand Progress in Earth and Planetary Science (2016) 3:15 Progress in Earth and DOI 10.1186/s40645-016-0085-6 Planetary Science REVIEW Open Access Philippine Sea Plate inception, evolution, and consumption with special emphasis on the early stages of Izu-Bonin-Mariana subduction Serge Lallemand1,2 Abstract We compiled the most relevant data acquired throughout the Philippine Sea Plate (PSP) from the early expeditions to the most recent. We also analyzed the various explanatory models in light of this updated dataset. The following main conclusions are discussed in this study. (1) The Izanagi slab detachment beneath the East Asia margin around 60–55 Ma likely triggered the Oki-Daito plume occurrence, Mesozoic proto-PSP splitting, shortening and then failure across the paleo-transform boundary between the proto-PSP and the Pacific Plate, Izu-Bonin-Mariana subduction initiation and ultimately PSP inception. (2) The initial splitting phase of the composite proto-PSP under the plume influence at ∼54–48 Ma led to the formation of the long-lived West Philippine Basin and short-lived oceanic basins, part of whose crust has been ambiguously called “fore-arc basalts” (FABs). (3) Shortening across the paleo-transform boundary evolved into thrusting within the Pacific Plate at ∼52–50 Ma, allowing it to subduct beneath the newly formed PSP, which was composed of an alternance of thick Mesozoic terranes and thin oceanic lithosphere. -
Temporal Evolution of Fault Coupling Associated with the Occurrence of Slow Slip Events in Central Japan
Temporal evolution of fault coupling associated with the occurrence of slow slip events in central Japan Lucile Bruhat∗y1 and Junichi Fukuda2 1Laboratoire de G´eologiede l'ENS { CNRS : UMR8538 { France 2Earthquake Research Institute { Japan Abstract Although interseismic coupling has often been considered to be stationary in time, there is increasing evidence that fault locking can vary both spatially and temporally during the interseismic period. The detection of transient slip behavior in the proximity of locked regions, such as slow slip events or decadal-scale uncoupling events, suggest in fact that the notion of a characteristic interseismic coupling distribution might not be appropriate. This study focuses on interseismic deformation rates in the southeastern part of the Kant¯o area in Japan. This region lies at junction of two subduction zones, leading to a particularly complicated tectonic setting. On the Eastern side, the Pacific plate subducts under the Okhotsk Plate at the Japan Trench, while the Sagami Trough to the south evidences the subduction of the Philippine Sea Plate under the Okhotsk Plate. The Philippine Sea Plate interface has hosted M8 megathrust earthquakes in the vicinity of Tokyo metropolitan area, such as the 1923 Great Kant¯oearthquake. Studies of interseismic deformation rates [Sagiya, (2004); Nishimura et al. (2007)] have shown that these megathrust events are consistent with the presence of a strongly locked asperity on the western extent of the Philippine Sea Plate interface at depths above 15-20km. Meanwhile, offshore the B¯os¯oPeninsula, i.e. on the eastern side of the interface, recurrent slow slip events have been detected in 1996, 2002, 2007, 2011, 2013-2014, and 2018. -
Tsunami Deposits and Earthquake Recurrence Along the Nankai
Tsunami deposits and earthquake recurrence along the Nankai, Suruga and Sagami Troughs OSAMU FUJIWARA1 and JUNKO KOMATSUBARA1 1: Active Fault Research Center, AIST, C7, 1-1-1 Higashi, Tsukuba, Ibaraki 305-8567, Japan ([email protected]) INTRODUCTION Histories of great (M~8) subduction-zone earthquakes inferred from tsunami deposits span 3000 years for the Nankai and Suruga Troughs and nearly 10,000 years for the Sagami Trough. The inferred histories contain variable recurrence intervals. The shortest recurrence intervals, 100-200 years for the Nankai Trough and 150-300 years for the Sagami Trough, are similar to those known from written earthquake and tsunami records in the last 1300 years. Longer intervals inferred from the tsunami deposits probably reflect variability in rupture mode, incompleteness of geologic records, and insufficient research. 130E 140E GEOLOGICAL SETTING The Nankai, Suruga and Sagami Troughs comprising the northeastern subduction margin of the Philippine Sea plate are 40N seismically active areas in the world. The Philippine Sea plate converges with overriding plates at a rate of 49-42 mm/year along the Nankai Trough and 27 mm/year around the Sagami Trough (Seno et al., 1993, 1994). Several source areas (segments) 35N Japan are located along these troughs, each of which are 100 - 150 km long along the trough axis and potentially excites M8-class Trench earthquake accompanied by large tsunami and coastal uplift or subsidence. Earthquakes and tsunamis occurred from these areas have repeatedly damaged the Pacific coast of Japan, including Tokyo Nankai Trough and Osaka metropolitan areas. Trench Trench Izu-Ogasawara Izu-Ogasawara Fig. -
Seismotectonic Modeling of the Repeating M 7-Class Disastrous Odawara Earthquake in the Izu Collision Zone, Central Japan
Earth Planets Space, 56, 843–858, 2004 Seismotectonic modeling of the repeating M 7-class disastrous Odawara earthquake in the Izu collision zone, central Japan Katsuhiko Ishibashi Research Center for Urban Safety and Security/Department of Earth and Planetary Sciences, Kobe University, Kobe 657-8501, Japan (Received February 16, 2004; Revised July 15, 2004; Accepted July 21, 2004) Odawara City in central Japan, in the northernmost margin of the Philippine Sea (PHS) plate, suffered from severe earthquake disasters five times during the last 400 years with a mean repeat time of 73 years; in 1633, 1703, 1782, 1853 and 1923. In this region, non-volcanic Izu outer arc (IOA), the easternmost part of the PHS plate, has been subducted beneath Honshu (Japanese main island), and volcanic Izu inner arc (IIA) on the west of IOA has made multiple collision against Honshu. I hypothesize ‘West-Sagami-Bay Fracture’ (WSBF) beneath Odawara, a north-south striking tear fault within the PHS plate that has separated the descending IOA crust from the buoyant IIA crust, through examinations of multiple collision process and the PHS plate configuration. WSBF is considered a blind causative fault of the 1633, 1782 and 1853 M 7 Odawara earthquakes, and is inferred to have ruptured also during the 1703 and 1923 great Kanto earthquakes simultaneously with the interplate main fault. A presumable asperity on WSBF just beneath Odawara seems to control the temporal regularity of earthquake occurrence. Though WSBF has not yet been detected directly, it is considered an essential tectonic element in this region, which might be a fracture zone with a few or several kilometer thickness actually. -
Earthquake Protection in Buildings Through Base Isolation
fECH RLC N4TL INST- OF STAND 4 NIST Special Publication 832, Volume 1 A111D3 7aTm7 Earthquake Resistant Construction Using Base Isolation NIST I PUBLICATIONS [Shin kenchiku kozo gijutsu kenkyu iin-kai hokokusho ] Earthquake Protection in Buildings Through Base Isolation United States Department of Commerce Z Technology Administration 832 National Institute of Standards and Technology V.1 1992 7he National Institute of Standards and Technology was established in 1988 by Congress to "assist industry in the development of technology . needed to improve product quality, to modernize manufacturing processes, to ensure product reliability . and to facilitate rapid commercialization ... of products based on new scientific discoveries." NIST, originally founded as the National Bureau of Standards in 1901, works to strengthen U.S. industry's competitiveness; advance science and engineering; and improve public health, safety, and the environment. One of the agency's basic functions is to develop, maintain, and retain custody of the national standards of measurement, and provide the means and methods for comparing standards used in science, engineering, manufacturing, commerce, industry, and education with the standards adopted or recognized by the Federal Government. As an agency of the U.S. Commerce Department's Technology Administration, NIST conducts basic and applied research in the physical sciences and engineering and performs related services. The Institute does generic and precompetitive work on new and advanced technologies. NIST's research -
Paleoseismicity Along the Southern Kuril Trench Deduced From
Paleoseismicity along the southern Kuril Trench deduced from submarine-fan turbidites ∗ , Atsushi Noda a, Taqumi TuZino a Yutaka Kanai a Ryuta Furukawa a Jun-ichi Uchida b 1 aGeological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST), Central 7, Higashi 1–1–1, Tsukuba, Ibaraki 305–8567, Japan bDepartment of Earth Science, Faculty of Science, Kumamoto University, 39-1, Kurokami 2-chome, Kumamoto 860-8555, Japan Received 24 August 2007; revised 22 May 2008; accepted 27 May 2008 Abstract Large (> M 8), damaging interplate earthquakes occur frequently in the eastern Hokkaido region, northern Japan, where the Pacific Plate is subducting rapidly beneath the Okhotsk (North American) Plate at approximately 8 cm yr−1. With the aim of estimating the long-term recurrence intervals of earthquakes in this region, seven sediment cores were obtained from a submarine fan located on the forearc slope along the southern Kuril Trench, Japan. The cores contain a number of turbidites, some of which can be correlated among the cores on the basis of the analysis of lithology, chronology, and the composition of sand grains. Foraminiferal assemblages and the composition of sand grains indicate that the upper–middle slope (> 1,000 m water depth) is the source of the turbidites. The deep-sea origin of the turbidites is consistent with the hypothesis that they were derived from slope failures initiated by strong shaking associated with earthquake events. The recurrence intervals of turbidite deposition are 113–439 years for events that occurred over the past 7 kyrs; the short intervals are recorded in the cores obtained from levees on the middle fan. -
Resilient Industries in Japan
Public Disclosure Authorized Public Disclosure Authorized Public Disclosure Authorized Public Disclosure Authorized ©2020 The World Bank International Bank for Reconstruction and Development The World Bank Group 1818 H Street NW, Washington, DC 20433 USA October 2020 RIGHTS AND PERMISSIONS The material in this work is subject to copyright. Because The World Bank encourages dissemination of its knowledge, this work may be reproduced, in whole or in part, for noncommercial purposes as long as full attribution to this work is given. Any queries on rights and licenses, including subsidiary rights, should be addressed to World Bank Publications, The World Bank Group, 1818 H Street NW, Washington, DC 20433, USA; e-mail: [email protected]. CITATION Please cite this report as follows: World Bank. 2020. “Resilient Industries in Japan: Lessons Learned in Japan on Enhancing Competitive Industries in the Face of Disasters Caused by Natural Hazards.” World Bank, Washington, D.C. ii Resilient Industries in Japan Resilient Industries in Japan iii DISCLAIMER This work is a product of the staff of The World Bank with external contributions. The findings, interpretations, and conclusions expressed in this work do not necessarily reflect the views of The World Bank, its Board of Executive Directors, or the governments they represent. The World Bank does not guarantee the accuracy of the data included in this work. The boundaries, colors, denominations, and other information shown on any map in this work do not imply any judgment on the part of The World Bank concerning the legal status of any territory or the endorsement or acceptance of such boundaries. -
The J-SHIS Fault Code
Japan Seismic Hazard Information Station (J-SHIS) File format specification June 2021 National Research Institute for Earth Science and Disaster Resilience -Table of contents- Probabilistic Seismic Hazard Maps: Guide for file "Seismic Hazard Map" ......................... 4 Probabilistic Seismic Hazard Maps: Guide for file "Hazard curve" ............................... 7 Probabilistic Seismic Hazard Maps: Guide for file "Hazard curve for Active fault" ............. 10 Probabilistic Seismic Hazard Maps: Guide for file "Fault shape (rectangle)" ................... 13 Probabilistic Seismic Hazard Maps: Guide for file "Fault shape (non-rectangle)" ............... 17 Probabilistic Seismic Hazard Maps: Guide for file "Fault shape (non-rectangle, Large Earthquakes along the Nankai Trough)" ........................................................................... 21 Probabilistic Seismic Hazard Maps: Guide for file "Fault shape (discretized rectangular source faults)" .............................................................................................. 24 Probabilistic Seismic Hazard Maps: Guide for file "Fault shape (discretized rectangular without specified source faults)" ..................................................................... 29 Probabilistic Seismic Hazard Maps: Guide for file "Fault shape (discretized non-rectangular source faults) ....................................................................................... 34 Probabilistic Seismic Hazard Maps: Guide for file "Parameters for seismic activity evaluation