Geological evidence for shallow ductile-brittle transition zones along subduction interfaces : example from the Shimanto Belt, SW Japan

• 資料種別: 記事
• タイトル: Geological evidence for shallow ductile-brittle transition zones along subduction interfaces : example from the Shimanto Belt, SW Japan
• 著者・編者: Yoshitaka Hashimoto; Natsuko Yamano
• 出版事項: 日本 : Springer science+business media
• 出版年月日等: 2014-10-16
• 出版年（W3CDTF）: 2014-10-16
• タイトル（掲載誌）: EPS : Earth, Planets and Space
• 巻号年月日等（掲載誌）: 66(141)
• 掲載巻: 66(141)
• 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/s40623-014-0141-7; https://doi.org/10.1186/s40623-014-0141-7
• 国立国会図書館永続的識別子: info:ndljp/pid/9227896; https://dl.ndl.go.jp/pid/9227896
• 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）: 2015-04-17T10:30:12+09:00
• 保存日（W3CDTF）: 2014-12-20
• 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）: https://www.earth-planets-space.com/content/66/October/2014
• 掲載誌（国立国会図書館永続的識別子）: info:ndljp/pid/9227755; https://dl.ndl.go.jp/pid/9227755
• 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

• 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 > デジタル化資料 > 雑誌; https://dl.ndl.go.jp/collections/A00002
• 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
• 所蔵機関: 国立国会図書館
• 請求記号: Z19-292
• 掲載誌（国立国会図書館永続的識別子）: info:ndljp/pid/3427605; https://dl.ndl.go.jp/pid/3427605
• 連携機関・データベース: 国立国会図書館 : 国立国会図書館雑誌記事索引; https://ndlsearch.ndl.go.jp
• 書誌ID（NDLBibID）: 9227896; http://id.ndl.go.jp/bib/9227896
• 整理区分コード: 632

• 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/s40623-014-0141-7; https://doi.org/10.1186/s40623-014-0141-7
• 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/9227896; https://dl.ndl.go.jp/pid/9227896; http://link.springer.com/article/10.1186/s40623-014-0141-7/fulltext.html; http://link.springer.com/content/pdf/10.1186/s40623-014-0141-7.pdf; http://link.springer.com/content/pdf/10.1186/s40623-014-0141-7
• 参照: Quantitative estimation of fluid pressure ratio of shear vein in an on-land accretionary complex, the Yokonami mélange, the Cretaceous Shimanto Belt, Kochi, southwest Japan; https://cir.nii.ac.jp/crid/1360285707500145920; Deformation characteristics and peak temperatures of the Sanbagawa Metamorphic and Shimanto Accretionary complexes on the central Kii Peninsula, SW Japan; https://cir.nii.ac.jp/crid/1360290617497491968; Terrestrial and marine organic matter evidence from a Cretaceous deep-sea chert of Japan: Implications for enhanced hydrological cycle during the Aptian OAE 1a; https://cir.nii.ac.jp/crid/1360861704761413376
• 参照: Dynamic deformation of the accretionary prism excites very low frequency earthquakes; https://cir.nii.ac.jp/crid/1050001202761516800; “Block-in-matrix" fabrics that lack shearing but possess composite cleavage planes: A sedimentary mélange origin for the Yuwan accretionary complex in the Ryukyu island arc, Japan; https://cir.nii.ac.jp/crid/1050282677703189760; Episodic slow slip events in the Japan subduction zone before the 2011 Tohoku-Oki earthquake; https://cir.nii.ac.jp/crid/1360002216175330176; Accretionary prisms in subduction earthquake cycles: The theory of dynamic Coulomb wedge; https://cir.nii.ac.jp/crid/1360011142937783424; Hydrogeology and Mechanics of Subduction Zone Forearcs: Fluid Flow and Pore Pressure; https://cir.nii.ac.jp/crid/1360011142939789696; Pressure solution lithification as a mechanism for the stick‐slip behavior of faults; https://cir.nii.ac.jp/crid/1360011145968023040; A new source of water in seismogenic subduction zones; https://cir.nii.ac.jp/crid/1360285708264945536; Frequency-size distribution of competent lenses in a block-in-matrix mélange: Imposed length scales of brittle deformation?; https://cir.nii.ac.jp/crid/1360292619014638976; Underplated units in an accretionary complex: Melange of the Shimanto Belt of eastern Shikoku, southwest Japan; https://cir.nii.ac.jp/crid/1360292619042493568; Pseudotachylytes in an ancient accretionary complex and implications for melt lubrication during subduction zone earthquakes; https://cir.nii.ac.jp/crid/1360292620270965888; Tsunamigenic potential of the shallow subduction plate boundary inferred from slow seismic slip; https://cir.nii.ac.jp/crid/1360565166760580608; Shallow Dynamic Overshoot and Energetic Deep Rupture in the 2011 <i>M</i> _w 9.0 Tohoku-Oki Earthquake; https://cir.nii.ac.jp/crid/1360565168391795456; Episodic slow slip events accompanied by non‐volcanic tremors in southwest Japan subduction zone; https://cir.nii.ac.jp/crid/1360574092884419328; Fluid inclusions; https://cir.nii.ac.jp/crid/1360574094187160448; Experimental stretching of fluid inclusions in calcite—Implications for diagenetic studies; https://cir.nii.ac.jp/crid/1360574094755776256; Large amount of fluid migration around shallow seismogenic depth preserved in tectonic mélange: Yokonami mélange, the Cretaceous Shimanto Belt, Kochi, Southwest Japan; https://cir.nii.ac.jp/crid/1360846643150274560; Propagation of Slow Slip Leading Up to the 2011 <i>M</i> _w 9.0 Tohoku-Oki Earthquake; https://cir.nii.ac.jp/crid/1360846643368612224; Geological and frictional aspects of very‐low‐frequency earthquakes in an accretionary prism; https://cir.nii.ac.jp/crid/1360848655052293248; An analysis of the variation of ocean floor bathymetry and heat flow with age; https://cir.nii.ac.jp/crid/1360855567860209920; Mélange and its seismogenic roof décollement: A plate boundary fault rock in the subduction zone—An example from the Shimanto Belt, Japan; https://cir.nii.ac.jp/crid/1360855571524756864; Paleothermal structure of the Shimanto accretionary prism, Shikoku, Japan: Role of an out-of-sequence thrust; https://cir.nii.ac.jp/crid/1361137043692926464; The thickness of subduction plate boundary faults from the seafloor into the seismogenic zone; https://cir.nii.ac.jp/crid/1361137044704641920; Geology of the earthquake source: an introduction; https://cir.nii.ac.jp/crid/1361418519446488960; Pseudotachylyte from an ancient accretionary complex: Evidence for melt generation during seismic slip along a master décollement?; https://cir.nii.ac.jp/crid/1361418520361633792; Geological record of fluid flow and seismogenesis along an erosive subducting plate boundary; https://cir.nii.ac.jp/crid/1361699995255732096; Tectonolithification of sandstone prior to the onset of seismogenic subduction zone: Evidence from tectonic mélange of the Shimanto Belt, Japan; https://cir.nii.ac.jp/crid/1361981469560535552; Structural evolution of underthrusted sediments, Kodiak Islands, Alaska; https://cir.nii.ac.jp/crid/1361981470734571904; Updip limit of the seismogenic zone beneath the accretionary prism of southwest Japan: An effect of diagenetic to low-grade metamorphic processes and increasing effective stress; https://cir.nii.ac.jp/crid/1361981471029956480; Tectonic incorporation of the upper part of oceanic crust to overriding plate of a convergent margin: An example from the Cretaceous–early Tertiary Mugi Mélange, the Shimanto Belt, Japan; https://cir.nii.ac.jp/crid/1362262945537756928; Record of mega-earthquakes in subduction thrusts: The black fault rocks of Pasagshak Point (Kodiak Island, Alaska); https://cir.nii.ac.jp/crid/1362544418773054848; Deformation mechanisms — recognition from natural tectonites; https://cir.nii.ac.jp/crid/1362544419522981120; Transition of accretionary wedge structures around the up-dip limit of the seismogenic subduction zone; https://cir.nii.ac.jp/crid/1362544420753100544; <i>In situ</i> pressure–temperature conditions of a tectonic mélange: Constraints from fluid inclusion analysis of syn‐mélange veins; https://cir.nii.ac.jp/crid/1362825894807870848; Fractal vein distributions within a fault-fracture mesh in an exhumed accretionary mélange, Chrystalls Beach Complex, New Zealand; https://cir.nii.ac.jp/crid/1362825896217499648; History of metamorphic fluids along outcrop‐scale faults in a Paleogene accretionary prism, SW Japan: Implications for prism‐scale hydrology; https://cir.nii.ac.jp/crid/1363107368617131136; Mélange rheology and seismic style; https://cir.nii.ac.jp/crid/1363107369220609920; A slow thrust slip event following the two 1996 Hyuganada Earthquakes beneath the Bungo Channel, southwest Japan; https://cir.nii.ac.jp/crid/1363388843526550272; Episodic Tremor and Slip on the Cascadia Subduction Zone: The Chatter of Silent Slip; https://cir.nii.ac.jp/crid/1363388844242379392; Thermal constraints on the zone of major thrust earthquake failure: The Cascadia Subduction Zone; https://cir.nii.ac.jp/crid/1363670318756185472; Depth of oceanic-crust underplating in a subduction zone: Inferences from fluid-inclusion analyses of crack-seal veins; https://cir.nii.ac.jp/crid/1363670320143149184; Change in fabric of melange in the Shimanto Belt, Japan: Change in relative convergence?; https://cir.nii.ac.jp/crid/1363951795329529984; Underplating process from melange formation to duplexing: Example from the Cretaceous Shimanto Belt, Kii Peninsula, southwest Japan; https://cir.nii.ac.jp/crid/1364233268348437760; P-T conditions of cataclastic deformation associated with underplating: An example from the Cretaceous Shimanto complex, Kii Peninsula, SW Japan; https://cir.nii.ac.jp/crid/1390001206512074368; Average slip rate at the transition zone on the plate interface beneath the Kii Peninsula, Japan, estimated from deep low-frequency tremors; https://cir.nii.ac.jp/crid/2050588892138454016
• 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）: 9227896; http://id.ndl.go.jp/bib/9227896