Estimation of slip rate and fault displacement during shallow earthquake rupture in the Nankai subduction zone

• 資料種別: 記事
• タイトル: Estimation of slip rate and fault displacement during shallow earthquake rupture in the Nankai subduction zone
• 著者・編者: Yohei Hamada; Arito Sakaguchi; Wataru Tanikawa
• 出版事項: 日本 : Springer science+business media
• 出版年月日等: 2015-03-13
• 出版年（W3CDTF）: 2015-03-13
• タイトル（掲載誌）: EPS : Earth, Planets and Space
• 巻号年月日等（掲載誌）: 67(39)
• 掲載巻: 67(39)
• 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/s40623-015-0208-0; https://doi.org/10.1186/s40623-015-0208-0
• 国立国会図書館永続的識別子: info:ndljp/pid/9381167; https://dl.ndl.go.jp/pid/9381167
• 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/March/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

• 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/s40623-015-0208-0; https://doi.org/10.1186/s40623-015-0208-0
• 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/9381167; https://dl.ndl.go.jp/pid/9381167; http://link.springer.com/content/pdf/10.1186/s40623-015-0208-0.pdf; http://link.springer.com/article/10.1186/s40623-015-0208-0/fulltext.html; http://link.springer.com/content/pdf/10.1186/s40623-015-0208-0; https://link.springer.com/content/pdf/10.1186/s40623-015-0208-0.pdf
• 参照: Deformation Structures From Splay and Décollement Faults in the Nankai Accretionary Prism, SW Japan(IODP NanTroSEIZE Expedition 316): Evidence for Slow and Rapid Slip in Fault Rocks; https://cir.nii.ac.jp/crid/1050855765273939328; Continuous depth profile of the rock strength in the Nankai accretionary prism based on drilling performance parameters; https://cir.nii.ac.jp/crid/1360283691807326592; Deformation Process and Mechanism of the Frontal Megathrust at the Nankai Subduction Zone; https://cir.nii.ac.jp/crid/1360298757401003648; Exothermic events in a fossil seismogenic fault acquiring thermoviscous remanent magnetization in an exhumed accretionary complex; https://cir.nii.ac.jp/crid/1360302864779705856; Lowering of the kinetic barrier of clay-mineral reactions along a seismogenic fault: Example from the Nankai subduction zone, Japan; https://cir.nii.ac.jp/crid/1360302866834024192; Three‐dimensional texture of natural pseudotachylyte: Pseudotachylyte formation mechanism in hydrous accretionary complex; https://cir.nii.ac.jp/crid/1360567185481585792; 科学掘削による地震断層の応力状態・物性・すべりパラメーターの評価; https://cir.nii.ac.jp/crid/1390282679214266752; 南海トラフ地震発生帯掘削がもたらした沈み込み帯の新しい描像; https://cir.nii.ac.jp/crid/1390845712966874112; Kinetic effect of heating rate on the thermal maturity of carbonaceous material as an indicator of frictional heat during earthquakes; https://cir.nii.ac.jp/crid/2051433317012921984
• 参照: High‐velocity frictional properties of clay‐rich fault gouge in a megasplay fault zone, Nankai subduction zone; https://cir.nii.ac.jp/crid/1050001202542012800; Estimation of slip parameters associated with frictional heating during the 1999 Taiwan Chi-Chi earthquake by vitrinite reflectance geothermometry; https://cir.nii.ac.jp/crid/1050866514666966656; Low Coseismic Shear Stress on the Tohoku-Oki Megathrust Determined from Laboratory Experiments; https://cir.nii.ac.jp/crid/1360002218438847488; Coal maturation by frictional heat during rapid fault slip; https://cir.nii.ac.jp/crid/1360004233289962880; Three-Dimensional Splay Fault Geometry and Implications for Tsunami Generation; https://cir.nii.ac.jp/crid/1360011142936447872; Plate convergence and long‐term crustal deformation in central Japan; https://cir.nii.ac.jp/crid/1360011142939448064; Thermal history estimation of the Taiwan Chelungpu fault using rock‐magnetic methods; https://cir.nii.ac.jp/crid/1360011143894792320; Frictional and hydrologic properties of clay‐rich fault gouge; https://cir.nii.ac.jp/crid/1360011145474388864; Contiguous rupture areas of two Nankai Trough earthquakes revealed by high‐resolution tsunami waveform inversion; https://cir.nii.ac.jp/crid/1360292617911260288; Source mechanisms and tectonic significance of historical earthquakes along the nankai trough, Japan; https://cir.nii.ac.jp/crid/1360292617916830848; Coseismic frictional heating and fluid-rock interaction in a slip zone within a shallow accretionary prism and implications for earthquake slip behavior; https://cir.nii.ac.jp/crid/1360292618852189568; Thermal maturity of a fold–thrust belt based on vitrinite reflectance analysis in the Western Foothills complex, western Taiwan; https://cir.nii.ac.jp/crid/1360292621062091904; 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; Progressive illitization in fault gouge caused by seismic slip propagation along a megasplay fault in the Nankai Trough; https://cir.nii.ac.jp/crid/1360565168428152832; Re-evaluation of frictional heat recorded in the dark gouge of the shallow part of a megasplay fault at the Nankai Trough; https://cir.nii.ac.jp/crid/1360567182476813440; Splay Fault Branching Along the Nankai Subduction Zone; https://cir.nii.ac.jp/crid/1360574092890685184; Seismic slip propagation to the updip end of plate boundary subduction interface faults: Vitrinite reflectance geothermometry on Integrated Ocean Drilling Program NanTro SEIZE cores; https://cir.nii.ac.jp/crid/1360846643404852096; The Philippine Sea: New survey results reveal the structure and the history of the marginal basins; https://cir.nii.ac.jp/crid/1360855567860176128; NanTroSEIZE: The IODP Nankai Trough Seismogenic Zone Experiment; https://cir.nii.ac.jp/crid/1360855567869180160; NanTroSEIZE Stage 1: NanTroSEIZE Shallow Megasplay and Frontal Thrusts Addendum; https://cir.nii.ac.jp/crid/1360855568784109568; Vitrinite reflectance and shear-induced graphitization in orogenic belts: A case study from the Kandersteg area, Helvetic Alps, Switzerland; https://cir.nii.ac.jp/crid/1361137044611853184; Changes to magnetic minerals caused by frictional heating during the 1999 Taiwan Chi-Chi earthquake; https://cir.nii.ac.jp/crid/1361137046414310912; Experimental frictional heating of coal gouge at seismic slip rates: Evidence for devolatilization and thermal pressurization of gouge fluids; https://cir.nii.ac.jp/crid/1361418518547318400; Estimated dynamic shear stress and frictional heat during the 1999 Taiwan Chi-Chi earthquake: A chemical kinetics approach with isothermal heating experiments; https://cir.nii.ac.jp/crid/1361418519489515008; Rupture process of the 1944 Tonankai earthquake (<i>M</i>_<i>s</i> 8.1) from the inversion of teleseismic and regional seismograms; https://cir.nii.ac.jp/crid/1361699995252579072; Coseismic fluid–rock interactions at high temperatures in the Chelungpu fault; https://cir.nii.ac.jp/crid/1361981469348269056; A chemical kinetic approach to estimate dynamic shear stress during the 1999 Taiwan Chi‐Chi earthquake; https://cir.nii.ac.jp/crid/1362262944993952128; Estimation of temperature rise in a shallow slip zone of the megasplay fault in the Nankai Trough; https://cir.nii.ac.jp/crid/1362544420807292032; Fluid-inclusion technique for determining maximum temperature in calcite and its comparison to the vitrinite reflectance geothermometer; https://cir.nii.ac.jp/crid/1363388846249755392; High precision slip distribution of the 1944 Tonankai earthquake inferred from tsunami waveforms: Possible slip on a splay fault; https://cir.nii.ac.jp/crid/1363670318316813440; Heating during thrust faulting in the rocky mountains: friction or fiction?; https://cir.nii.ac.jp/crid/1363951793228726016; Earthquakes and friction laws; https://cir.nii.ac.jp/crid/1363951793447762816; Thermal considerations in inferring frictional heating from vitrinite reflectance and implications for shallow coseismic slip within the Nankai Subduction Zone; https://cir.nii.ac.jp/crid/1363951795801146368; Very low frequency earthquakes excited by the 2004 off Kii peninsula earthquakes: a dynamic deformation process in the large accretionary prism; https://cir.nii.ac.jp/crid/1390001206512583680; Source rupture process of the 1944 Tonankai earthquake and the 1945 Mikawa earthquake derived from low-gain seismograms; https://cir.nii.ac.jp/crid/1390001206513406976; Coseismic slip distribution of the 1946 Nankai earthquake and aseismic slips caused by the earthquake; https://cir.nii.ac.jp/crid/1390282681488085504; Low‐frequency tremors associated with reverse faults in a shallow accretionary prism; https://cir.nii.ac.jp/crid/1570009750829304960; Geochemical and mineralogical characteristics of fault gouge in the Median Tectonic Line, Japan : evidence for earthquake slip; https://cir.nii.ac.jp/crid/2050025942186658176
• 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）: 9381167; http://id.ndl.go.jp/bib/9381167