Evolution of the rheological structure of Mars

• 資料種別: 記事
• タイトル: Evolution of the rheological structure of Mars
• 著者・編者: Shintaro Azuma; Ikuo Katayama
• 出版事項: 日本 : Springer Nature
• 出版年月日等: 2017-01-03
• 出版年（W3CDTF）: 2017-01-03
• タイトル（掲載誌）: EPS : Earth, Planets and Space
• 巻号年月日等（掲載誌）: 69(8)
• 掲載巻: 69(8)
• 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/s40623-016-0593-z; https://doi.org/10.1186/s40623-016-0593-z
• 国立国会図書館永続的識別子: info:ndljp/pid/10319659; https://dl.ndl.go.jp/pid/10319659
• コレクション（共通）: 障害者向け資料
• コレクション（障害者向け資料：レベル1）: テキストデータ
• 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; https://dl.ndl.go.jp/collections/B00035
• 収集根拠: オンライン資料収集制度
• 受理日（W3CDTF）: 2017-04-04T20:19:14+09:00
• 保存日（W3CDTF）: 2017-03-24
• 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（URI）: http://earth-planets-space.springeropen.com/articles?searchType=journalSearch&sort=PubDate&page=2
• 掲載誌（国立国会図書館永続的識別子）: info:ndljp/pid/10319651; https://dl.ndl.go.jp/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; https://dl.ndl.go.jp

• 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/s40623-016-0593-z; https://doi.org/10.1186/s40623-016-0593-z
• 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）: http://id.ndl.go.jp/digimeta/10319659; https://dl.ndl.go.jp/pid/10319659; http://link.springer.com/content/pdf/10.1186/s40623-016-0593-z.pdf; http://link.springer.com/article/10.1186/s40623-016-0593-z/fulltext.html
• 参照: 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; https://cir.nii.ac.jp/crid/1390001206239470720; 海惑星の将来を考える; https://cir.nii.ac.jp/crid/1390570950855611264; Sensitivity of elastic thickness to water in the Martian lithosphere; https://cir.nii.ac.jp/crid/2050870367067985792; Strength models of the terrestrial planets and implications for their lithospheric structure and evolution; https://cir.nii.ac.jp/crid/2051996266985512064
• 参照: Low-temperature, high-stress deformation of olivine under water-saturated conditions; https://cir.nii.ac.jp/crid/1050585039689055744; Rheology of the upper mantle and the mantle wedge: A view from the experimentalists; https://cir.nii.ac.jp/crid/1360011142941004544; The crust and mantle of Mars; https://cir.nii.ac.jp/crid/1360011143898065152; Crustal structure of Mars from gravity and topography; https://cir.nii.ac.jp/crid/1360011144735471232; Evolution of water reservoirs on Mars: Constraints from hydrogen isotopes in martian meteorites; https://cir.nii.ac.jp/crid/1360283690892968192; Rheological decoupling at the Moho and implication to Venusian tectonics; https://cir.nii.ac.jp/crid/1360285708503188992; Strength of Martian lithosphere beneath large volcanoes; https://cir.nii.ac.jp/crid/1360292620746946560; Long‐term deformation driven by small ambient tectonic stresses and strong oscillating tidal within Enceladus with analogy to rock behavior near the San Andreas Fault; https://cir.nii.ac.jp/crid/1360574094522966912; Fluid Core Size of Mars from Detection of the Solar Tide; https://cir.nii.ac.jp/crid/1360574095616458368; Thermal history of Mars inferred from orbital geochemistry of volcanic provinces; https://cir.nii.ac.jp/crid/1360574095997264512; Thermal and albedo mapping of Mars during the Viking primary mission; https://cir.nii.ac.jp/crid/1360855567860211840; Mantle dynamics in Mars and Venus: Influence of an immobile lithosphere on three‐dimensional mantle convection; https://cir.nii.ac.jp/crid/1360855568747787520; Upper limits of power law creep of rocks; https://cir.nii.ac.jp/crid/1360855568765980544; The temperature variation of hardness of olivine and its implication for polycrystalline yield stress; https://cir.nii.ac.jp/crid/1360855568796941056; The early heat loss evolution of Mars and their implications for internal and environmental history; https://cir.nii.ac.jp/crid/1360855569908070016; Dislocation and diffusion creep of synthetic anorthite aggregates; https://cir.nii.ac.jp/crid/1360855570365677312; The thermal evolution of Mars as constrained by paleo-heat flows; https://cir.nii.ac.jp/crid/1360855570489898240; Strength of the lithosphere: Constraints imposed by laboratory experiments; https://cir.nii.ac.jp/crid/1360855570878253952; Martian plate tectonics; https://cir.nii.ac.jp/crid/1360855571116457472; Rheology of the Lower Crust and Upper Mantle: Evidence from Rock Mechanics, Geodesy, and Field Observations; https://cir.nii.ac.jp/crid/1360855571286824576; Martian wrinkle ridge topography: Evidence for subsurface faults from MOLA; https://cir.nii.ac.jp/crid/1361137043993340672; Heat Transfer; https://cir.nii.ac.jp/crid/1361137044873902208; The effect of mineral bond strength and adsorbed water on fault gouge frictional strength; https://cir.nii.ac.jp/crid/1361137045329746944; Thermal and crustal evolution of Mars; https://cir.nii.ac.jp/crid/1361418519369462016; Variations in K/Th on Mars; https://cir.nii.ac.jp/crid/1361418519439399680; Evidence for a differentiated crust in Solis Planum, Mars, from lithospheric strength and heat flow; https://cir.nii.ac.jp/crid/1361418519567088896; Internal Structure and Early Thermal Evolution of Mars from Mars Global Surveyor Topography and Gravity; https://cir.nii.ac.jp/crid/1361418521328689920; Effects of pressure on high-temperature dislocation creep in olivine; https://cir.nii.ac.jp/crid/1361699993396359552; Ancient heat flow, crustal thickness, and lithospheric mantle rheology in the Amenthes region, Mars; https://cir.nii.ac.jp/crid/1361699993454058880; Concentration of H, Si, Cl, K, Fe, and Th in the low‐ and mid‐latitude regions of Mars; https://cir.nii.ac.jp/crid/1361699994631218176; 3D strength and gravity anomalies of the European lithosphere; https://cir.nii.ac.jp/crid/1361699996128253696; Mars North Polar Deposits: Stratigraphy, Age, and Geodynamical Response; https://cir.nii.ac.jp/crid/1361981469530802944; The Borealis basin and the origin of the martian crustal dichotomy; https://cir.nii.ac.jp/crid/1361981470087103488; Global Mineralogical and Aqueous Mars History Derived from OMEGA/Mars Express Data; https://cir.nii.ac.jp/crid/1362262943563763712; 1. Introduction; https://cir.nii.ac.jp/crid/1362262943912654336; The effective elastic thickness (<i>T</i>_<i>e</i>) of continental lithosphere: What does it really mean?; https://cir.nii.ac.jp/crid/1362262944013705728; Geologic setting of serpentine deposits on Mars; https://cir.nii.ac.jp/crid/1362544418611400832; Identification of hydrated silicate minerals on Mars using MRO‐CRISM: Geologic context near Nili Fossae and implications for aqueous alteration; https://cir.nii.ac.jp/crid/1362544418982261376; High‐temperature deformation of dry diabase with application to tectonics on Venus; https://cir.nii.ac.jp/crid/1362544419929846016; Rheology of the Upper Mantle: A Synthesis; https://cir.nii.ac.jp/crid/1362544421132538880; Creep of Crystals; https://cir.nii.ac.jp/crid/1362825895140039808; Low strength of deep San Andreas fault gouge from SAFOD core; https://cir.nii.ac.jp/crid/1362825895811933952; Self-consistent generation of tectonic plates in three-dimensional mantle convection; https://cir.nii.ac.jp/crid/1362825896069036800; Thermal diffusivity and conductivity of olivine, wadsleyite and ringwoodite to 20 GPa and 1373 K; https://cir.nii.ac.jp/crid/1362825896075018752; The evolution of the martian elastic lithosphere and implications for crustal and mantle rheology; https://cir.nii.ac.jp/crid/1363107368695990656; VOLCANISM AND TECTONICS ON VENUS; https://cir.nii.ac.jp/crid/1363107368781805696; Stagnant lid convection on Venus; https://cir.nii.ac.jp/crid/1363107368934227712; Magnetic Lineations in the Ancient Crust of Mars; https://cir.nii.ac.jp/crid/1363107369064244352; Martian surface heat production and crustal heat flow from Mars Odyssey Gamma-Ray spectrometry; https://cir.nii.ac.jp/crid/1363107369691007616; Mantle Convection in the Earth and Planets; https://cir.nii.ac.jp/crid/1363388844123870336; Scaling of stagnant-lid convection with Arrhenius rheology and the effects of mantle melting; https://cir.nii.ac.jp/crid/1363388844885750400; Orbital forcing of the martian polar layered deposits; https://cir.nii.ac.jp/crid/1363670318456329600; Friction of rocks; https://cir.nii.ac.jp/crid/1363670319216204800; Self‐consistent generation of tectonic plates in time‐dependent, three‐dimensional mantle convection simulations; https://cir.nii.ac.jp/crid/1363670320654879488; Low strength of Earth’s uppermost mantle inferred from tri-axial deformation experiments on dry olivine crystals; https://cir.nii.ac.jp/crid/1363951793177821568; Tectonic implications of Mars crustal magnetism; https://cir.nii.ac.jp/crid/1363951794713318016; Early plate tectonics versus single‐plate tectonics on Mars: Evidence from magnetic field history and crust evolution; https://cir.nii.ac.jp/crid/1364233268536666112; Localized gravity/topography admittance and correlation spectra on Mars: Implications for regional and global evolution; https://cir.nii.ac.jp/crid/1364233268738540544; Long term evolution and chaotic diffusion of the insolation quantities of Mars; https://cir.nii.ac.jp/crid/1364233269543803904; Chemical composition and accretion history of terrestrial planets; https://cir.nii.ac.jp/crid/1364233269677957376; On the spatial variability of the Martian elastic lithosphere thickness: Evidence for mantle plumes?; https://cir.nii.ac.jp/crid/1364233270632971648; Variations of elastic plate thickness at continental thrust belts; https://cir.nii.ac.jp/crid/1364233271021730816; Correction to “Localized gravity/topography admittance and correlation spectra on Mars: Implications for regional and global evolution”; https://cir.nii.ac.jp/crid/1364233271219119488
• 連携機関・データベース: 国立情報学研究所 : CiNii Research; https://cir.nii.ac.jp/
• 提供元機関・データベース: 雑誌記事索引データベース; https://ndlsearch.ndl.go.jp; Crossref; https://www.crossref.org; 科学研究費助成事業データベース; https://kaken.nii.ac.jp/ja
• 書誌ID（NDLBibID）: 10319659; http://id.ndl.go.jp/bib/10319659