Omori-like slow decay (p < 1) of postseismic displacement rates following the 2011 Tohoku megathrust earthquake
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DOI[10.1186/s40623-020-01162-w]to the data of the same series
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- Material Type
- 記事
- Author/Editor
- Shunsuke MorikamiYuta Mitsui
- Publication, Distribution, etc.
- Publication Date
- 2020-03-16
- Publication Date (W3CDTF)
- 2020-03-16
- Periodical title
- EPS : Earth, Planets and Space
- No. or year of volume/issue
- 72(37)
- Volume
- 72(37)
- ISSN (Periodical Title)
- 1880-5981
- ISSN-L (Periodical Title)
- 1343-8832
- Text Language Code
- eng
- DOI
- 10.1186/s40623-020-01162-w
- Persistent ID (NDL)
- info:ndljp/pid/11520491
- Collection
- Collection (Materials For Handicapped People:1)
- Collection (particular)
- 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
- Acquisition Basis
- オンライン資料収集制度
- Date Accepted (W3CDTF)
- 2020-08-03T12:00:21+09:00
- Date Captured (W3CDTF)
- 2020-08-03
- Format (IMT)
- application/pdf
- Access Restrictions
- 国立国会図書館内限定公開
- Service for the Digitized Contents Transmission Service
- 図書館・個人送信対象外
- Availability of remote photoduplication service
- 可
- Periodical Title (URI)
- Periodical Title (Persistent ID (NDL))
- info:ndljp/pid/11467692
- Data Provider (Database)
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- Summary, etc.
- application/pdf
- DOI
- 10.1186/s40623-020-01162-w
- Access Restrictions
- インターネット公開
- Rights (production)
- © The Author(s) 2020.This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.
- Related Material
- Additional file 1 of Omori-like slow decay (p
- Related Material (URI)
- Is Referenced By
- Azimuthal differences and changes in strain rate and stress of the Japanese Islands deduced from geophysical dataOn the performance of position-domain sidereal filter for 30-s kinematic GPS to mitigate multipath errorsHeterogeneous rheology of Japan subduction zone revealed by postseismic deformation of the 2011 Tohoku-oki earthquake
- References
- Scaling of early afterslip velocity and possible detection of tsunami-induced subsidence by GPS measurements immediately after the 2011 Tohoku-Oki earthquakeAfterslip and viscoelastic relaxation following the 2011 Tohoku earthquake (Mw9.0) inferred from inland GPS and seafloor GPS/Acoustic dataAccelerated pacific plate subduction following interplate thrust earthquakes at the Japan trenchMachine Learning Approach to Characterize the Postseismic Deformation of the 2011 Tohoku‐Oki Earthquake Based on Recurrent Neural NetworkStress‐driven relaxation of heterogeneous upper mantle and time‐dependent afterslip following the 2011 Tohoku earthquakePrevalence of viscoelastic relaxation after the 2011 Tohoku-oki earthquakeSeafloor observations indicate spatial separation of coseismic and postseismic slips in the 2011 Tohoku earthquakeModeling Seismic Cycles of Great Megathrust Earthquakes Across the Scales With Focus at Postseismic PhaseHeterogeneous rheology controlled postseismic deformation of the 2011 Tohoku‐Oki earthquakeRapid mantle flow with power-law creep explains deformation after the 2011 Tohoku mega-quakeAn updated digital model of plate boundariesPersistent inelastic deformation in central Japan revealed by GPS observation before and after the Tohoku-oki earthquakeComparison of accuracy of GPS techniquesResolving depth-dependent subduction zone viscosity and afterslip from postseismic displacements following the 2011 Tohoku-oki, Japan earthquakeEvidence of viscoelastic deformation following the 2011 Tohoku‐Oki earthquake revealed from seafloor geodetic observationDeformation cycles of subduction earthquakes in a viscoelastic EarthAfterslip and aftershocks in the rate‐and‐state friction lawNonlinear strain buildup and the earthquake cycle on the San Andreas FaultPossibility of recovery of slip deficit rate between the North American plate and the Pacific plate off Sanriku, northeast JapanPostseismic Viscoelastic ReboundA constitutive law for rate of earthquake production and its application to earthquake clusteringStochastic synthesis of earthquake catalogsEvidence of power-law flow in the Mojave desert mantleSlab1.0: A three‐dimensional model of global subduction zone geometriesA Variable Span SmootherOmori‐like decay of postseismic velocities following continental earthquakesOn the mechanics of earthquake afterslipFrequency of earthquakes in California*Overlapping post-seismic deformation processes: afterslip and viscoelastic relaxation following the 2011 Mw 9.0 Tohoku (Japan) earthquakePostseismic relaxation driven by brittle creep: A possible mechanism to reconcile geodetic measurements and the decay rate of aftershocks, application to the Chi‐Chi earthquake, TaiwanPreceding, coseismic, and postseismic slips of the 2011 Tohoku earthquake, JapanStatistical Models for Earthquake Occurrences and Residual Analysis for Point ProcessesQuasi-static Motions near the San Andreas Fault ZoneSilent fault slip following an interplate thrust earthquake at the Japan TrenchEarthquake and Volcano DeformationComparison of postseismic afterslip models with aftershock seismicity for three subduction-zone earthquakes: Nias 2005, Maule 2010 and Tohoku 2011Frictional Afterslip Following the 2005 Nias-Simeulue Earthquake, SumatraRepeating earthquakes and quasi-static slip on the plate boundary east off northern Honshu, Japan新潟－神戸ひずみ集中帯を横断する測地観測による越後平野周辺の地殻変動Importance of rheological heterogeneity for interpreting viscoelastic relaxation caused by the 2011 Tohoku-Oki earthquakeThe 2011 off the Pacific coast of Tohoku Earthquake and its aftershocks observed by GEONETInterplate fault slip along the Japan Trench before the occurrence of the 2011 off the Pacific coast of Tohoku Earthquake as inferred from GPS dataContributions of poroelastic rebound and a weak volcanic arc to the postseismic deformation of the 2011 Tohoku earthquake
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- 120006821302