Effect of stress state on slow rupture propagation in synthetic fault gouges

• 資料種別: 記事
• タイトル: Effect of stress state on slow rupture propagation in synthetic fault gouges
• 著者・編者: Ken-ichi Hirauchi; Jun Muto
• 出版事項: 日本 : Springer science+business media
• 出版年月日等: 2015-02-24
• 出版年（W3CDTF）: 2015-02-24
• タイトル（掲載誌）: EPS : Earth, Planets and Space
• 巻号年月日等（掲載誌）: 67(25)
• 掲載巻: 67(25)
• 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/s40623-015-0199-x; https://doi.org/10.1186/s40623-015-0199-x
• 国立国会図書館永続的識別子: info:ndljp/pid/9381152; https://dl.ndl.go.jp/pid/9381152
• 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）: 2015-06-08T22:01:55+09:00
• 保存日（W3CDTF）: 2015-04-20
• 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/67/February/2015
• 掲載誌（国立国会図書館永続的識別子）: info:ndljp/pid/9227920; https://dl.ndl.go.jp/pid/9227920
• 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: Z74-E817
• 掲載誌（国立国会図書館永続的識別子）: info:ndljp/pid/13773260; https://dl.ndl.go.jp/pid/13773260
• 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）: 9381152; http://id.ndl.go.jp/bib/9381152
• 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/s40623-015-0199-x; https://doi.org/10.1186/s40623-015-0199-x
• 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/9381152; https://dl.ndl.go.jp/pid/9381152; http://link.springer.com/content/pdf/10.1186/s40623-015-0199-x.pdf; http://link.springer.com/article/10.1186/s40623-015-0199-x/fulltext.html; http://link.springer.com/content/pdf/10.1186/s40623-015-0199-x
• 参照: Dehydration of brucite + antigorite under mantle wedge conditions: insights from the direct comparison of microstructures before and after experiments; https://cir.nii.ac.jp/crid/1360017280626151168; 蛇紋岩の力学的性質とそのテクトニックな意義; https://cir.nii.ac.jp/crid/1390282679213864576
• 参照: Recurrence behavior of short‐term slow slip and correlated nonvolcanic tremor episodes in western Shikoku, southwest Japan; https://cir.nii.ac.jp/crid/1050294045371264512; Spatial variations in antigorite fabric across a serpentinite subduction channel: insights from the Ohmachi Seamount, Izu-Bonin arc; https://cir.nii.ac.jp/crid/1050564288821961472; Electric potential changes associated with nucleation of stick-slip of simulated gouges; https://cir.nii.ac.jp/crid/1360002216175302912; Preseismic fault slip and earthquake prediction; https://cir.nii.ac.jp/crid/1360011143777769216; Weakening of the slab–mantle wedge interface induced by metasomatic growth of talc; https://cir.nii.ac.jp/crid/1360011144270517376; Rheological contrast between serpentine species and implications for slab–mantle wedge decoupling; https://cir.nii.ac.jp/crid/1360283691152066304; Nonvolcanic Deep Tremor Associated with Subduction in Southwest Japan; https://cir.nii.ac.jp/crid/1360292617909770624; Strain hardening and strength of clay‐rich fault gouges; https://cir.nii.ac.jp/crid/1360292618491671680; Role of fault gouge dilatancy on aseismic deformation transients; https://cir.nii.ac.jp/crid/1360292620361139968; On the relation between fault strength and frictional stability; https://cir.nii.ac.jp/crid/1360292620404307456; Permeability anisotropy of serpentinite and fluid pathways in a subduction zone; https://cir.nii.ac.jp/crid/1360565168428158336; Low-frequency earthquakes in Shikoku, Japan, and their relationship to episodic tremor and slip; https://cir.nii.ac.jp/crid/1360574092886258944; Short‐time scale correlation between slow slip and tremor in Cascadia; https://cir.nii.ac.jp/crid/1360574096071074944; Detachment fronts and the onset of dynamic friction; https://cir.nii.ac.jp/crid/1360855569033391232; Frictional strength and strain weakening in simulated fault gouge: Competition between geometrical weakening and chemical strengthening; https://cir.nii.ac.jp/crid/1360855569439657856; Slow Earthquakes, Preseismic Velocity Changes, and the Origin of Slow Frictional Stick-Slip; https://cir.nii.ac.jp/crid/1361137044364045312; Scaling of the shear rupture process from nucleation to dynamic propagation: Implications of geometric irregularity of the rupturing surfaces; https://cir.nii.ac.jp/crid/1361418518833610240; Dynamic properties of stick-slip friction of rock; https://cir.nii.ac.jp/crid/1361418519591063040; Slow Earthquakes and Nonvolcanic Tremor; https://cir.nii.ac.jp/crid/1361418520940507776; Strain Localization and Slip Instability in a Strain-Rate Hardening, Chemically Weakening Material; https://cir.nii.ac.jp/crid/1361418521052320384; Implications of the mechanical and frictional behavior of serpentinite to seismogenic faulting; https://cir.nii.ac.jp/crid/1361699994551858048; Correlation between velocity dependence of friction and strain localization in large displacement experiments on feldspar, muscovite and biotite gouge; https://cir.nii.ac.jp/crid/1361699994784210560; Seismic evidence for overpressured subducted oceanic crust and megathrust fault sealing; https://cir.nii.ac.jp/crid/1361699994853040640; Scaling Relationships of Source Parameters for Slow Slip Events; https://cir.nii.ac.jp/crid/1361699996015672064; Frictional behavior of large displacement experimental faults; https://cir.nii.ac.jp/crid/1362262943702240896; From Sub-Rayleigh to Supershear Ruptures During Stick-Slip Experiments on Crustal Rocks; https://cir.nii.ac.jp/crid/1362262944084880000; Spatial and temporal evolution of a long term slow slip event: the 2006 Guerrero Slow Slip Event; https://cir.nii.ac.jp/crid/1362544418456071296; Shear zones in granular material; https://cir.nii.ac.jp/crid/1362544420503145088; Spatio‐temporal complexity of slip on a fault; https://cir.nii.ac.jp/crid/1362544420670610560; Instabilities at frictional interfaces: Creep patches, nucleation, and rupture fronts; https://cir.nii.ac.jp/crid/1362825893502768512; Strain-rate effect on frictional strength and the slip nucleation process; https://cir.nii.ac.jp/crid/1362825895106549120; Slip-stick and the evolution of frictional strength; https://cir.nii.ac.jp/crid/1363107369139034624; High pore pressures and porosity at 35 km depth in the Cascadia subduction zone; https://cir.nii.ac.jp/crid/1363107369285936128; The frictional behavior of lizardite and antigorite serpentinites: Experiments, constitutive models, and implications for natural faults; https://cir.nii.ac.jp/crid/1363388843565554816; Episodic Tremor and Slip on the Cascadia Subduction Zone: The Chatter of Silent Slip; https://cir.nii.ac.jp/crid/1363388844242379392; Episodic slow slip events and rate‐and‐state friction; https://cir.nii.ac.jp/crid/1363388844590807552; The Dynamics of the Onset of Frictional Slip; https://cir.nii.ac.jp/crid/1363388846114988288; Chapter 2 Fabrics of Experimental Fault Zones: Their Development and Relationship to Mechanical Behavior; https://cir.nii.ac.jp/crid/1363670318503611392; An integrated perspective of the continuum between earthquakes and slow-slip phenomena; https://cir.nii.ac.jp/crid/1363951793178291456; Effects of physical fault properties on frictional instabilities produced on simulated faults; https://cir.nii.ac.jp/crid/1363951794473108352; The Coefficient of Friction of Chrysotile Gouge at Seismogenic Depths; https://cir.nii.ac.jp/crid/1363951794658744192; Experimental observation of stick-slip instability fronts; https://cir.nii.ac.jp/crid/1363951796126110336; A comparison of similar aerosol measurements made on the NASA P3‐B, DC‐8, and NSF C‐130 aircraft during TRACE‐P and ACE‐Asia; https://cir.nii.ac.jp/crid/1364233268662593536; Inhibition of subduction thrust earthquakes by low-temperature plastic flow in serpentine; https://cir.nii.ac.jp/crid/1364233269490309248; Experimental measurements of permeability evolution during triaxial compression of initially intact crystalline rocks and implications for fluid flow in fault zones; https://cir.nii.ac.jp/crid/1364233269613595776; Slow Earthquakes Coincident with Episodic Tremors and Slow Slip Events; https://cir.nii.ac.jp/crid/1364233269991901952; A Silent Slip Event on the Deeper Cascadia Subduction Interface; https://cir.nii.ac.jp/crid/1364233270426238080; A scaling low for slow earthquakes; https://cir.nii.ac.jp/crid/1572824501329363968; A long-term slow slip event from 1996 to 1997 in the Kii Channel, Japan; https://cir.nii.ac.jp/crid/2050307417163364224
• 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）: 9381152; http://id.ndl.go.jp/bib/9381152