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電子書籍・電子雑誌Progress in earth and planetary science
巻号5
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Variations in precursory slip behavior resulting from frictional heterogeneity

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Variations in precursory slip behavior resulting from frictional heterogeneity

国立国会図書館請求記号
Z14-529
国立国会図書館書誌ID
11190338
国立国会図書館永続的識別子
info:ndljp/pid/11190338
資料種別
記事
著者
Suguru Yabeほか
出版者
Springer Nature
出版年
2018-08-22
資料形態
紙・デジタル
掲載誌名
Progress in earth and planetary science 5(43)
掲載ページ
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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(提供元: CiNii Research)

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デジタル

資料種別
記事
著者・編者
Suguru Yabe
Satoshi Ide
出版年月日等
2018-08-22
出版年(W3CDTF)
2018-08-22
タイトル(掲載誌)
Progress in earth and planetary science
巻号年月日等(掲載誌)
5(43)
掲載巻
5(43)
ISSN(掲載誌)
2197-4284
ISSN-L(掲載誌)
2197-4284
本文の言語コード
eng
国立国会図書館永続的識別子
info:ndljp/pid/11190338
コレクション(共通)
コレクション(障害者向け資料:レベル1)
コレクション(個別)
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
収集根拠
オンライン資料収集制度
受理日(W3CDTF)
2018-11-26T20:20:20+09:00
保存日(W3CDTF)
2018-11-26
記録形式(IMT)
application/pdf
オンライン閲覧公開範囲
国立国会図書館内限定公開
デジタル化資料送信
図書館・個人送信対象外
遠隔複写可否(NDL)
掲載誌(国立国会図書館永続的識別子)
info:ndljp/pid/11018906
連携機関・データベース
国立国会図書館 : 国立国会図書館デジタルコレクション

デジタル

要約等
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
オンライン閲覧公開範囲
インターネット公開
参照
Stress release process along an intraplate fault analogous to the plate boundary: a case study of the 2017 M5.2 Akita-Daisen earthquake, NE Japan
Physical Mechanism for a Temporal Decrease of the Gutenberg‐Richter <i>b</i>‐Value Prior to a Large Earthquake
Slow Stick‐Slip Failure in Halite Gouge Caused by Brittle‐Plastic Fault Heterogeneity
Eight-year catalog of deep short-term slow slip events at the Nankai trough based on objective detection algorithm using strain and tilt records
Segmentation of Shallow Slow Slip Events at the Hikurangi Subduction Zone Explained by Along‐Strike Changes in Fault Geometry and Plate Convergence Rates
Fault‐Valve Behavior Estimated From Intensive Foreshocks and Aftershocks of the 2017 M 5.3 Kagoshima Bay Earthquake Sequence, Kyushu, Southern Japan
Evaluation of Phenomena Preceding Earthquakes and Earthquake Predictability
Fast to Slow Slip Transition in Stick-Slip Friction of Polymer Gels with Artificial Roughness
参照
An explanation for episodic tremor and slow slip constrained by crack-seal veins and viscous shear in subduction mélange
Frictional properties of JFAST core samples and implications for slow earthquakes at the Tohoku subduction zone
Episodic slow slip events in the Japan subduction zone before the 2011 Tohoku-Oki earthquake
Why Do Aftershocks Occur Within the Rupture Area of a Large Earthquake?
Large nucleation before large earthquakes is sometimes skipped due to cascade‐up—Implications from a rate and state simulation of faults with hierarchical asperities
Nucleation of frictional instability caused by fluid pressurization in subducted blueschist
Tidal sensitivity of tectonic tremors in Nankai and Cascadia subduction zones
Historical seismicity and dynamic rupture process of the 2011 Tohoku-Oki earthquake
New, improved version of generic mapping tools released
Nonvolcanic Deep Tremor Associated with Subduction in Southwest Japan
Source mechanisms and tectonic significance of historical earthquakes along the nankai trough, Japan
Repeating earthquakes and interplate aseismic slip in the northeastern Japan subduction zone
Internal structure and permeability of major strike-slip fault zones: the Median Tectonic Line in Mie Prefecture, Southwest Japan
Foreshock sequences and short-term earthquake predictability on East Pacific Rise transform faults
Occurrence patterns of foreshocks to large earthquakes in the western United States
Slip‐behavior transitions of a heterogeneous linear fault
Foreshocks explained by cascades of triggered seismicity
Earthquake nucleation on faults with rate-and state-dependent strength
Extended Nucleation of the 1999 <i>M</i> <sub>w</sub> 7.6 Izmit Earthquake
Propagation of Slow Slip Leading Up to the 2011 <i>M</i> <sub>w</sub> 9.0 Tohoku-Oki Earthquake
Recurring and triggered slow-slip events near the trench at the Nankai Trough subduction megathrust
Foreshock sequence of the 1992 Landers, California, earthquake and its implications for earthquake nucleation
Seismic Consequences of Warm Versus Cool Subduction Metamorphism: Examples from Southwest and Northeast Japan
Interactions and triggering in a 3‐D rate‐and‐state asperity model
The long precursory phase of most large interplate earthquakes
Foreshocks during the nucleation of stick‐slip instability
Earthquake nucleation on (aging) rate and state faults
Intense foreshocks and a slow slip event preceded the 2014 Iquique <i>M</i> <sub>w</sub> 8.1 earthquake
Quasi‐dynamic versus fully dynamic simulations of earthquakes and aseismic slip with and without enhanced coseismic weakening
Spatio‐temporal complexity of slip on a fault
Geologic heterogeneity can produce aseismic slip transients
Båth's law derived from the Gutenberg‐Richter law and from aftershock properties
Mainshocks are aftershocks of conditional foreshocks: How do foreshock statistical properties emerge from aftershock laws
Mélange rheology and seismic style
Modeling of rock friction: 1. Experimental results and constitutive equations
Low friction and fault weakening revealed by rising sensitivity of tremor to tidal stress
Characteristic small‐earthquake sequence off Sanriku, northeastern Honshu, Japan
Mechanism Diversity of the Loma Prieta Aftershocks and the Mechanics of Mainshock-Aftershock Interaction
Statistical Models for Earthquake Occurrences and Residual Analysis for Point Processes
Inferring fault rheology from low‐frequency earthquakes on the San Andreas
Deep low‐frequency tremor that correlates with passing surface waves
Detailed observations of California foreshock sequences: Implications for the earthquake initiation process
Stability of faults with heterogeneous friction properties and effective normal stress
Statistical study of the occurrence of shallow earthquakes
Brittle‐viscous deformation, slow slip, and tremor
Spatial correlation of aftershock locations and on‐fault main shock properties
Some characteristics of foreshocks and their possible relationship to earthquake prediction and premonitory slip on faults
Fault stability inferred from granite sliding experiments at hydrothermal conditions
深部微動が明らかにする潮汐のプレート運動への影響
Possibility of Mw 9.0 mainshock triggered by diffusional propagation of after-slip from Mw 7.3 foreshock
連携機関・データベース
国立情報学研究所 : CiNii Research
書誌ID(NDLBibID)
11190338