Strength models of the terrestrial planets and implications for their lithospheric structure and evolution
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DOI[10.1186/s40645-020-00388-2]のデータに遷移します
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- 資料種別
- 記事
- 著者・編者
- Ikuo Katayama
- 出版年月日等
- 2021-01-04
- 出版年（W3CDTF）
- 2021-01-04
- タイトル（掲載誌）
- Progress in earth and planetary science
- 巻号年月日等（掲載誌）
- 8(1)
- 掲載巻
- 8(1)
- ISSN（掲載誌）
- 2197-4284
- ISSN-L（掲載誌）
- 2197-4284
- 本文の言語コード
- eng
- DOI
- 10.1186/s40645-020-00388-2
- 国立国会図書館永続的識別子
- info:ndljp/pid/11667980
- 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）
- 2021-04-28T11:35:34+09:00
- 保存日（W3CDTF）
- 2021-04-28
- 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/11667979
- 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/s40645-020-00388-2
- 関連情報（URI）
- 参照
- Effects of rheological stratification and elasticity of lithosphere on subduction initiationElastic Properties of Thermally Treated Diabase and Peridotite: Implications Toward the Elastic Properties of Oceanic Lithosphere
- 参照
- Low-temperature, high-stress deformation of olivine under water-saturated conditionsSystematic changes in the incoming plate structure at the Kuril trenchRheology of the upper mantle and the mantle wedge: A view from the experimentalistsThe crust and mantle of MarsSerpentine in active subduction zonesCrustal structure of Mars from gravity and topographyHigh-Pressure Creep of Serpentine, Interseismic Deformation, and Initiation of SubductionGrain boundary sliding in San Carlos olivine: Flow law parameters and crystallographic-preferred orientationLithospheric strength and its relationship to the elastic and seismogenic layer thicknessVolatiles on Earth and Mars: A comparisonRheological decoupling at the Moho and implication to Venusian tectonicsSeismic velocity structure and its implications for oceanic mantle hydration in the trench–outer rise of the Japan TrenchWhat is the origin of macroscopic friction?Heterogeneities in the thickness of the elastic lithosphere of Mars: Constraints on heat flow and internal dynamicsClues to the lithospheric structure of Mars from wrinkle ridge sets and localization instabilityDeformation of antigorite serpentinite at high temperature and pressureRheology and thermal structure of the lithosphere beneath the Hawaiian Ridge inferred from gravity data and models of plate flexureEpisodic tremor and slow slip potentially linked to permeability contrasts at the MohoWater in the oceanic upper mantle: implications for rheology, melt extraction and the evolution of the lithosphereDeformation of Earth MaterialsUpper limits of power law creep of rocksDislocation and diffusion creep of synthetic anorthite aggregatesThe thermal evolution of Mars as constrained by paleo-heat flowsStrength of the lithosphere: Constraints imposed by laboratory experimentsMartian plate tectonicsRheology of the Lower Crust and Upper Mantle: Evidence from Rock Mechanics, Geodesy, and Field ObservationsFabric development in (Mg,Fe)O during large strain, shear deformation: implications for seismic anisotropy in Earth’s lower mantle11. Friction of the Smectite Clay MontmorilloniteLong-Term Evolution of the Martian Crust-Mantle SystemElastic Thickness Estimates for Venus Using Line of Sight Accelerations from Magellan Cycle 5Effects of pressure on high-temperature dislocation creep in olivineDynamics of fault motion and the origin of contrasting tectonic style between Earth and VenusDeformation of clinopyroxenite: Evidence for a transition in flow mechanisms and semibrittle behaviorMars North Polar Deposits: Stratigraphy, Age, and Geodynamical ResponseWater Management Challenges Associated with the Production of Shale Gas by Hydraulic FracturingTessera deformation and the contemporaneous thermal state of the plateau highlands, VenusThe effective elastic thickness (<i>T</i><sub><i>e</i></sub>) of continental lithosphere: What does it really mean?Differences between Archean and Proterozoic lithospheres: Assessment of the possible major role of thermal conductivityPlanetary TectonicsLithospheric flexure and thermal anomaliesFormation of fold-and-thrust belts on Venus by thick-skinned deformationObservations of flexure and the state of stress in the oceanic lithosphereHigh‐temperature deformation of dry diabase with application to tectonics on VenusThermal structure of oceanic and continental lithosphereGeological Evolution of Venus: Rises, Plains, Plumes, and PlateausThe evolution of the martian elastic lithosphere and implications for crustal and mantle rheologyVOLCANISM AND TECTONICS ON VENUSLithospheric flexure on VenusVenus: Volcanism and Rift Formation in Beta RegioSolubility of water in the α, β and γ phases of (Mg,Fe) 2 SiO 4Depth of faulting on Mercury: Implications for heat flux and crustal and effective elastic thicknessImplications of the high D/H ratio for the sources of water in Venus' atmosphereObservations of flexure and the rheology of the oceanic lithosphereSubsurface water and clay mineral formation during the early history of MarsFriction of rocksThe mechanical and thermal structure of Mercury's early lithosphereImplications of fault-valve behaviour for rupture nucleation and recurrenceStress and temperature in the bending lithosphere as constrained by experimental rock mechanicsThe seismicity of MarsThe effect of mineralogy and effective normal stress on frictional strength of sheet silicatesCorrection to “Localized gravity/topography admittance and correlation spectra on Mars: Implications for regional and global evolution”岩石の変形特性に対する水の効果と大陸・海洋プレートのレオロジー構造蛇紋岩の力学的性質とそのテクトニックな意義Effects of humidity and interlayer cations on the frictional strength of montmorilloniteSensitivity of elastic thickness to water in the Martian lithosphereCan clay minerals account for the behavior of non-asperity on the subducting plate interface？Evolution of the rheological structure of Mars
- 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CrossrefCrossref
- 書誌ID（NDLBibID）
- 11667980