Can clay minerals account for the behavior of non-asperity on the subducting plate interface？

• Material Type: 記事
• Title: Can clay minerals account for the behavior of non-asperity on the subducting plate interface？
• Author/Editor: Ikuo Katayama; Tatsuro Kubo; Hiroshi Sakuma
• Publication, Distribution, etc.: 日本 : Springer science+business media
• Publication Date: 2015-10-09
• Publication Date (W3CDTF): 2015-10-09
• Periodical title: Progress in earth and planetary science
• No. or year of volume/issue: 2(30)
• Volume: 2(30)
• ISSN (Periodical Title): 2197-4284
• ISSN-L (Periodical Title): 2197-4284
• Text Language Code: eng
• DOI: 10.1186/s40645-015-0063-4; https://doi.org/10.1186/s40645-015-0063-4
• Persistent ID (NDL): info:ndljp/pid/9589762; https://dl.ndl.go.jp/pid/9589762
• Collection: 障害者向け資料
• Collection (Materials For Handicapped People:1): テキストデータ
• Collection (particular): 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
• Acquisition Basis: オンライン資料収集制度
• Date Accepted (W3CDTF): 2016-01-07T15:30:20+09:00
• Date Captured (W3CDTF): 2015-10-20
• Format (IMT): application/pdf
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• Periodical Title (URI): https://www.progearthplanetsci.com/content
• Periodical Title (Persistent ID (NDL)): info:ndljp/pid/9381655; https://dl.ndl.go.jp/pid/9381655
• Data Provider (Database): 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

• Summary, etc.: 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/s40645-015-0063-4; https://doi.org/10.1186/s40645-015-0063-4
• Access Restrictions: インターネット公開
• Related Material (URI): http://id.ndl.go.jp/digimeta/9589762; https://dl.ndl.go.jp/pid/9589762; http://link.springer.com/content/pdf/10.1186/s40645-015-0063-4.pdf; http://link.springer.com/article/10.1186/s40645-015-0063-4/fulltext.html; http://link.springer.com/content/pdf/10.1186/s40645-015-0063-4
• Is Referenced By: Along‐arc variation in short‐term slow slip events caused by 3‐D fluid migration in subduction zones; https://cir.nii.ac.jp/crid/1360004229806369280; Effects of rheological stratification and elasticity of lithosphere on subduction initiation; https://cir.nii.ac.jp/crid/1360017282450945792; A small amount of water reduces the friction of the preferentially oriented montmorillonite gouge; https://cir.nii.ac.jp/crid/1360021390740597504; What is the origin of macroscopic friction?; https://cir.nii.ac.jp/crid/1360285710914105216; Role of Weak Materials in Earthquake Rupture Dynamics; https://cir.nii.ac.jp/crid/1360286993350471168; Interlayer energy of pyrophyllite: Implications for macroscopic friction; https://cir.nii.ac.jp/crid/1361413118166412800; Depth profile of frictional properties in the inner Nankai accretionary prism using cuttings from IODP Site C0002; https://cir.nii.ac.jp/crid/2050307417130254336; 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
• References: Low Coseismic Shear Stress on the Tohoku-Oki Megathrust Determined from Laboratory Experiments; https://cir.nii.ac.jp/crid/1360002218438847488; The 2011 Tohoku earthquake (Mw 9.0) sequence and subduction dynamics in Western Pacific and East Asia; https://cir.nii.ac.jp/crid/1360004232324606464; Time-dependent friction in rocks; https://cir.nii.ac.jp/crid/1360011146128987520; Adhesion energy between mica surfaces: Implications for the frictional coefficient under dry and wet conditions; https://cir.nii.ac.jp/crid/1360285704777560576; Smectite to chlorite conversion by frictional heating along a subduction thrust; https://cir.nii.ac.jp/crid/1360285707111917824; Sediment subduction versus accretion around the pacific; https://cir.nii.ac.jp/crid/1360574092889444864; High Pore Fluid Pressure May Cause Silent Slip in the Nankai Trough; https://cir.nii.ac.jp/crid/1360574092889866368; 3. Sediment Inputs to Subduction Zones; https://cir.nii.ac.jp/crid/1360574092890863744; Frictional properties of megathrust fault gouges at low sliding velocities: New data on effects of normal stress and temperature; https://cir.nii.ac.jp/crid/1360846640974802176; Slow earthquakes associated with fault healing on a serpentinized plate interface; https://cir.nii.ac.jp/crid/1360848658455309824; Do subducting seamounts generate or stop large earthquakes?; https://cir.nii.ac.jp/crid/1360855568531590912; Effect of clay content and mineralogy on frictional sliding behavior of simulated gouges: Binary and ternary mixtures of quartz, illite, and montmorillonite; https://cir.nii.ac.jp/crid/1360855570005949568; Large heat and fluid fluxes driven through mid-plate outcrops on ocean crust; https://cir.nii.ac.jp/crid/1361137043842370688; 11. Friction of the Smectite Clay Montmorillonite; https://cir.nii.ac.jp/crid/1361137044241792128; The effect of mineral bond strength and adsorbed water on fault gouge frictional strength; https://cir.nii.ac.jp/crid/1361137045329746944; Sources of Tsunami and Tsunamigenic Earthquakes in Subduction Zones; https://cir.nii.ac.jp/crid/1361418520009128960; A deep strong reflector in the Nankai accretionary wedge from multichannel seismic data: Implications for underplating and interseismic shear stress release; https://cir.nii.ac.jp/crid/1361418520445508992; Slow Earthquakes and Nonvolcanic Tremor; https://cir.nii.ac.jp/crid/1361418520940507776; Nanoindentation and morphological studies on nylon 66 nanocomposites. I. Effect of clay loading; https://cir.nii.ac.jp/crid/1361418521426803584; Hydrologic control of forearc strength and seismicity in the Costa Rican subduction zone; https://cir.nii.ac.jp/crid/1361699993825042944; Effect of humidity on time‐ and velocity‐dependent friction in rocks; https://cir.nii.ac.jp/crid/1361699994256541568; Effective stress and pore pressure in the Nankai accretionary prism off the Muroto Peninsula, southwestern Japan; https://cir.nii.ac.jp/crid/1361981469136454400; The Seismogenic Zone of Subduction Thrust Faults; https://cir.nii.ac.jp/crid/1361981470169070080; Earthquake stress drop and laboratory‐inferred interseismic strength recovery; https://cir.nii.ac.jp/crid/1361981470397137664; Effect of hydration state on the frictional properties of montmorillonite‐based fault gouge; https://cir.nii.ac.jp/crid/1362262943463419264; Direct observation of frictional contacts: New insights for state-dependent properties; https://cir.nii.ac.jp/crid/1362262945415418112; The key frictional parameters controlling spatial variations in the speed of postseismic-slip propagation on a subduction plate boundary; https://cir.nii.ac.jp/crid/1362544420728098816; Fluids in accretionary prisms; https://cir.nii.ac.jp/crid/1362825895625123712; Frictional healing of quartz gouge under hydrothermal conditions: 1. Experimental evidence for solution transfer healing mechanism; https://cir.nii.ac.jp/crid/1362825895761684224; Serpentinization of the forearc mantle; https://cir.nii.ac.jp/crid/1362825895853921792; Rupture Process of Subduction-Zone Earthquakes; https://cir.nii.ac.jp/crid/1363107368644167040; LABORATORY-DERIVED FRICTION LAWS AND THEIR APPLICATION TO SEISMIC FAULTING; https://cir.nii.ac.jp/crid/1363107368675058816; Weakness of the San Andreas Fault revealed by samples from the active fault zone; https://cir.nii.ac.jp/crid/1363107369114306048; Thrust-type subduction-zone earthquakes and seamount asperities: A physical model for seismic rupture; https://cir.nii.ac.jp/crid/1363107369522568448; The Mechanics of Earthquakes and Faulting; https://cir.nii.ac.jp/crid/1363107369934690560; Comparison of smectite- and illite-rich gouge frictional properties: application to the updip limit of the seismogenic zone along subduction megathrusts; https://cir.nii.ac.jp/crid/1363107370528551040; Frictional strength and healing behavior of phyllosilicate‐rich faults; https://cir.nii.ac.jp/crid/1363388844924138112; Silent fault slip following an interplate thrust earthquake at the Japan Trench; https://cir.nii.ac.jp/crid/1363670319089972224; Earthquakes and friction laws; https://cir.nii.ac.jp/crid/1363951793447762816; The effect of seamount subduction on seismic coupling; https://cir.nii.ac.jp/crid/1364233268741451520; Fractal asperities, invasion of barriers, and interplate earthquakes; https://cir.nii.ac.jp/crid/1390001206513668480
• Data Provider (Database): 国立情報学研究所 : CiNii Research; https://cir.nii.ac.jp/
• Original Data Provider (Database): 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
• Bibliographic ID (NDL): 9589762; http://id.ndl.go.jp/bib/9589762