Shear strain concentration mechanism in the lower crust below an intraplate strike-slip fault based on rheological laws of rocks
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- 資料種別
- 記事
- 著者・編者
- Xuelei ZhangTakeshi Sagiya
- 出版年月日等
- 2017-06-19
- 出版年(W3CDTF)
- 2017-06-19
- タイトル(掲載誌)
- EPS : Earth, Planets and Space
- 巻号年月日等(掲載誌)
- 69(82)
- 掲載巻
- 69(82)
- ISSN(掲載誌)
- 1880-5981
- ISSN-L(掲載誌)
- 1343-8832
- 本文の言語コード
- eng
- DOI
- 10.1186/s40623-017-0668-5
- 国立国会図書館永続的識別子
- info:ndljp/pid/10369109
- 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)
- 2017-06-22T22:40:19+09:00
- 保存日(W3CDTF)
- 2017-06-22
- 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)
- 可
- 掲載誌(国立国会図書館永続的識別子)
- info:ndljp/pid/10319651
- 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
- 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
- DOI
- 10.1186/s40623-017-0668-5
- オンライン閲覧公開範囲
- インターネット公開
- 関連情報(URI)
- 参照
- Intraplate Strike‐Slip Faulting, Stress Accumulation, and Shear Localization of a Crust‐Upper Mantle System With Nonlinear Viscoelastic MaterialCrustal dynamics: unified understanding of geodynamic processes at different time and length scales不均質レオロジー構造を考慮した島弧地殻における変形と応力場のモデル化
- 参照
- Grain size reduction due to fracturing and subsequent grain-size-sensitive creep in a lower crustal shear zone in the presence of a CO2-bearing fluidGrain size reduction by dynamic recrystallization: can it result in major rheological weakening?Scaling of viscous shear zones with depth-dependent viscosity and power-law stress–strain-rate dependenceInhibition of grain growth by second-phase particlesGeodetic determination of relative plate motion in central CaliforniaDeep crustal structure along the Niigata-Kobe Tectonic Zone, Japan: Its origin and segmentationRheology of the Lower Crust and Upper Mantle: Evidence from Rock Mechanics, Geodesy, and Field ObservationsOn the effects of thermally weakened ductile shear zones on postseismic deformationNetworking of shear zones at the brittle-to-viscous transition (Cap de Creus, NE Spain)High‐temperature fracturing and subsequent grain‐size‐sensitive creep in lower crustal gabbros: Evidence for coseismic loading followed by creep during decaying stress in the lower crust?On the relationship between the formation of shear zones and the form of the flow law for rocks undergoing dynamic recrystallizationOn dynamic recrystallization during solid state flow: Effects of stress and temperatureShear heating in continental strike-slip shear zones:model and field examplesGrain Growth Kinetics of Quartz and Calcite AggregatesWater-weakened lower crust and its role in the concentrated deformation in the Japanese IslandsGeotectonic evolution of the Nihonkoku Mylonite Zone of north central Japan based on geology, geochemistry, and radiometric ages of the Nihonkoku MylonitesGrain-size-sensitive flow and shear-stress enhancement at the brittle–ductile transition of the continental crustTomographic Evidence for Localized Lithospheric Shear Along the Altyn Tagh FaultOn mylonites in ductile shear zonesThermal and mechanical evolution of shear zonesGrain size evolution and the rheology of ductile shear zones: from laboratory experiments to postseismic creepHeat flow and energetics of the San Andreas Fault ZoneFar‐reaching transient motions after Mojave earthquakes require broad mantle flow beneath a strong crustDynamic models of interseismic deformation and stress transfer from plate motion to continental transform faultsInfluence of water fugacity and activation volume on the flow properties of fine‐grained anorthite aggregatesSP-Mylonites: Origin of some mylonites by superplastic flowMagnetotelluric transect across the Niigata‐Kobe Tectonic Zone, central Japan: A clear correlation between strain accumulation and resistivity structureFriction of rocksStrain accumulation process around the Atotsugawa fault system in the Niigata-Kobe Tectonic Zone, central JapanFrictional coefficient on faults in a seismogenic region inferred from earthquake mechanism solutions“Introduction to Grains, Phases, and Interfaces—an Interpretation of Microstructure,” Trans. AIME, 1948, vol. 175, pp. 15–51, by C.S. SmithDuctile shear zones beneath strike‐slip faults: Implications for the thermomechanics of the San Andreas Fault ZoneShear deformation zones along major transform faults and subducting slabsKinematics of oblique collision and ramping inferred from microstructures and strain in middle crustal rocks, central Southern Alps, New ZealandGrain and sub-grain size variations across a mylonite zoneGeothermal gradient and heat flow data in and around Japan (I): apprasial of heat flow from geothermal gradient dataMid-crustal electrical conductors and their correlations to seismicity and deformation at Itoigawa-Shizuoka Tectonic LineOrigin of the concentrated deformation zone in the Japanese Islands and stress accumulation process of intraplate earthquakesOccurrence of mylonite zones and pseudotachylyte veins around the base of the upper crust: An example from the southern Hidaka metamorphic belt, Samani area, Hokkaido, JapanDeep crustal structure around the Atotsugawa fault system, central Japan : a weak zone below the seismogenic zone and its role in earthquake generation
- 連携機関・データベース
- 国立情報学研究所 : CiNii Research
- 提供元機関・データベース
- 雑誌記事索引データベースCrossref科学研究費助成事業データベース科学研究費助成事業データベース科学研究費助成事業データベースCrossrefCrossrefCrossref
- 書誌ID(NDLBibID)
- 10369109