Importance of rheological heterogeneity for interpreting viscoelastic relaxation caused by the 2011 Tohoku-Oki earthquake
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DOI[10.1186/s40623-017-0611-9]to the data of the same series
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- Material Type
- 記事
- Author/Editor
- Hisashi Suito
- Publication, Distribution, etc.
- Publication Date
- 2017-01-31
- Publication Date (W3CDTF)
- 2017-01-31
- Periodical title
- EPS : Earth, Planets and Space
- No. or year of volume/issue
- 69(21)
- Volume
- 69(21)
- ISSN (Periodical Title)
- 1880-5981
- ISSN-L (Periodical Title)
- 1343-8832
- Text Language Code
- eng
- DOI
- 10.1186/s40623-017-0611-9
- Persistent ID (NDL)
- info:ndljp/pid/10319672
- 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)
- 2017-04-04T20:19:14+09:00
- Date Captured (W3CDTF)
- 2017-03-24
- 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/10319651
- 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.
- コレクション : 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
- DOI
- 10.1186/s40623-017-0611-9
- Access Restrictions
- インターネット公開
- Related Material (URI)
- Is Referenced By
- Omori-like slow decay (p < 1) of postseismic displacement rates following the 2011 Tohoku megathrust earthquakeAzimuthal differences and changes in strain rate and stress of the Japanese Islands deduced from geophysical dataInfluence of the 2011 Tohoku-oki earthquake on the strain-rate field around the Noto PeninsulaExtremely early recurrence of intraplate fault rupture following the Tohoku-Oki earthquakeSpatiotemporal distributions of afterslip and locking on the plate interface associated with the 2011 Tohoku-Oki earthquake using a 3-D temperature and strain rate-dependent heterogeneous viscosity modelProgress in modeling the Tohoku-oki megathrust earthquake cycle and associated crustal deformation processesAn adjoint-based simultaneous estimation method of the asthenosphere's viscosity and afterslip using a fast and scalable finite-element adjoint solverRapid mantle flow with power-law creep explains deformation after the 2011 Tohoku mega-quakePresence of interplate channel layer controls of slip during and after the 2011 Tohoku-Oki earthquake through the frictional characteristicsFunction Model Based on Nonlinear Transient Rheology of Rocks: An Analysis of Decadal GNSS Time Series After the 2011 Tohoku‐oki EarthquakePostseismic gravity changes after the 2011 Tohoku earthquake observed by superconducting gravimeters at Mizusawa, JapanInterpretation of Offshore Crustal Movements Following the 2011 Tohoku-Oki Earthquake by the Combined Effect of Afterslip and Viscoelastic Stress RelaxationInterplate Slip Following the 2003 Tokachi‐oki Earthquake From Ocean Bottom Pressure Gauge and Land GNSS DataInvestigating a tsunamigenic megathrust earthquake in the Japan TrenchNew Megathrust Locking Model for the Southern Kurile Subduction Zone Incorporating Viscoelastic Relaxation and Non‐Uniform Compliance of Upper PlateAlong-arc heterogeneous rheology inferred from post-seismic deformation of the 2011 Tohoku-oki earthquake2004年紀伊半島南東沖の地震の粘性緩和による変動上部マントルの粘性構造を反映した深発地震の余効変動Detection of Seafloor Movement in Subduction Zones Around Japan Using a GNSS-A Seafloor Geodetic Observation System from 2013 to 2016ベイズ推定によるすべりインバージョン研究の高度化東北沖地震の余効変動から知る東北日本弧地殻マントルのレオロジー特性Potential for crustal deformation monitoring using a dense cell phone carrier Global Navigation Satellite System networkHeterogeneous rheology of Japan subduction zone revealed by postseismic deformation of the 2011 Tohoku-oki earthquakeImprovement on spatial resolution of a coseismic slip distribution using postseismic geodetic data through a viscoelastic inversion
- Data Provider (Database)
- 国立情報学研究所 : CiNii Research
- Original Data Provider (Database)
- 雑誌記事索引データベースCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 10319672