Quartz deposition and its influence on the deformation process of megathrusts in subduction zones

• 資料種別: 記事
• タイトル: Quartz deposition and its influence on the deformation process of megathrusts in subduction zones
• 著者・編者: Jun Kameda; Kuniyo Kawabata; Yohei Hamada
• 出版事項: 日本 : Springer science+business media
• 出版年月日等: 2014-04-16
• 出版年（W3CDTF）: 2014-04-16
• タイトル（掲載誌）: EPS : Earth, Planets and Space
• 巻号年月日等（掲載誌）: 66(13)
• 掲載巻: 66(13)
• ISSN（掲載誌）: 1880-5981
• ISSN-L（掲載誌）: 1343-8832
• 本文の言語コード: eng
• DOI: 10.1186/1880-5981-66-13; https://doi.org/10.1186/1880-5981-66-13
• 国立国会図書館永続的識別子: info:ndljp/pid/9227768; https://dl.ndl.go.jp/pid/9227768
• 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）: 2014-10-10
• 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/April/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/3427593; https://dl.ndl.go.jp/pid/3427593
• 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）: 9227768; http://id.ndl.go.jp/bib/9227768
• 整理区分コード: 632

• 要約等: We present a quantitative examination of the liberation and subsequent deposition of silica at the subduction zone plate interface in the Mugi melange, an exhumed accretionary complex in the Shimanto Belt of southwest Japan. Frequency and thickness measurements indicate that mineralized veins hosted in deformed shales make up approximately 0.4% of the volume of this exposure. In addition, whole-rock geochemical evidence suggests that the net volume of SiO2 liberated from the melange at temperatures of < 200 degrees C was as much as 35%, with up to 40% of the SiO2 loss related to the smectite-illite (S-I) conversion reaction, and the rest attributable to the pressure solution of detrital quartz and feldspar. Kinetic modeling of the S-I reaction indicates active liberation of SiO2 at approximately 70 degrees C to 200 degrees C, with peak SiO2 loss at around 100 degrees C, although these estimates should be slightly shifted toward lower temperature conditions based on X-ray diffraction (XRD) analyses of mixed-layer S-I in the Mugi melange. The onset of pressure solution was not fully constrained, but has been documented to occur at around 150 degrees C in the study area. The deposition in deformed shales of quartz liberated by pressure solution and the S-I reaction is probably linked to seismogenic behavior along the plate interface by (1) progressively enhanced velocity-weakening properties, which are favorable for unstable seismogenic faulting, including very-low-frequency earthquakes and (2) increasing intrinsic frictional strength, which leads to a step-down of the plate boundary decollement into oceanic basalt.
• DOI: 10.1186/1880-5981-66-13; https://doi.org/10.1186/1880-5981-66-13
• オンライン閲覧公開範囲: インターネット公開
• 著作権情報: Creative Commons Attribution 2.0 Generic
• 関連情報（URI）: https://hdl.handle.net/2115/56747; http://id.ndl.go.jp/digimeta/9227768; https://dl.ndl.go.jp/pid/9227768; http://link.springer.com/content/pdf/10.1186/1880-5981-66-13.pdf; http://link.springer.com/article/10.1186/1880-5981-66-13/fulltext.html; http://hdl.handle.net/2115/56747
• 参照: Alteration and dehydration of subducting oceanic crust within subduction zones : implications for décollement step-down and plate-boundary seismogenesis; https://cir.nii.ac.jp/crid/1050306506454155648; Heterogeneous Sediment Input at the Nankai Trough Subduction Zone: Implications for Shallow Slow Earthquake Localization; https://cir.nii.ac.jp/crid/1360854882786727936; 瑞浪層群中村層における脈状岩石の形成過程; https://cir.nii.ac.jp/crid/1390005999446309888
• 参照: Effects of fluid circulation in subducting crust on Nankai margin seismogenic zone temperatures; https://cir.nii.ac.jp/crid/1360011142941320832; Are open fractures necessarily aligned with maximum horizontal stress?; https://cir.nii.ac.jp/crid/1360011145775470848; Stretching of fluid inclusions in calcite as an indicator of frictional heating on faults; https://cir.nii.ac.jp/crid/1360011146051296256; Smectite to chlorite conversion by frictional heating along a subduction thrust; https://cir.nii.ac.jp/crid/1360285707111917824; Mechanism of burial metamorphism of argillaceous sediment: 1. Mineralogical and chemical evidence; https://cir.nii.ac.jp/crid/1360292619168639872; On the relation between fault strength and frictional stability; https://cir.nii.ac.jp/crid/1360292620404307456; Clay gouge; https://cir.nii.ac.jp/crid/1360292621336184704; Tsunamigenic potential of the shallow subduction plate boundary inferred from slow seismic slip; https://cir.nii.ac.jp/crid/1360565166760580608; Sources and physicochemical characteristics of fluids along a subduction‐zone megathrust: A geochemical approach using syn‐tectonic mineral veins in the Mugi mélange, Shimanto accretionary complex; https://cir.nii.ac.jp/crid/1360567183243227008; Underplating of mélange evidenced by the depositional ages: U–Pb dating of zircons from the Shimanto accretionary complex, southwest Japan; https://cir.nii.ac.jp/crid/1360574094234849920; The Thermal Transformation of Smectite to Illite; https://cir.nii.ac.jp/crid/1360574094643075840; Frictional slip of granite at hydrothermal conditions; https://cir.nii.ac.jp/crid/1360574094745441408; Decomposition of Experimental X-Ray Diffraction Patterns (Profile Fitting): A Convenient Way to Study Clay Minerals; https://cir.nii.ac.jp/crid/1360574095607660288; Science policy study hearings announced; https://cir.nii.ac.jp/crid/1360574095827239040; Fluidization of granular material in a subduction thrust at seismogenic depths; https://cir.nii.ac.jp/crid/1360574096464323328; 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; Geological and frictional aspects of very‐low‐frequency earthquakes in an accretionary prism; https://cir.nii.ac.jp/crid/1360848655052293248; 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; Late-Stage Diagenesis of Illitic Clay Minerals as Seen by Decomposition of X-Ray Diffraction Patterns: Contrasted Behaviors of Sedimentary Basins with Different Burial Histories; https://cir.nii.ac.jp/crid/1361418518727329152; The role of tectonic shear strain on the illitization mechanism of mixed-layers illite–smectite. A case study from a fault zone in the Northern Apennines, Italy; https://cir.nii.ac.jp/crid/1361418519066119680; Mineralogy and Sedimentation of Recent Deep-Sea Clay in the Atlantic Ocean and Adjacent Seas and Oceans; https://cir.nii.ac.jp/crid/1361418520283352576; Evaluation of in situ smectite dehydration as a pore water freshening mechanism in the Nankai Trough, offshore southwest Japan; https://cir.nii.ac.jp/crid/1361699996019086464; Mass transfer and pressure solution in deformed shale of accretionary complex: Examples from the Shimanto Belt, southwestern Japan; https://cir.nii.ac.jp/crid/1361981469264012160; Smectite-illite-muscovite transformations, quartz dissolution, and Silica release in shales; https://cir.nii.ac.jp/crid/1361981470450101760; 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; Progressive deformation of a Tertiary Trench Slope, Kodiak Islands, Alaska; https://cir.nii.ac.jp/crid/1362262943509958144; 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; Very low frequency earthquakes along the Ryukyu subduction zone; https://cir.nii.ac.jp/crid/1362544421035771008; Quartz cement in sandstones: a review; https://cir.nii.ac.jp/crid/1362825894761599744; The isocon diagram; a simple solution to Gresens' equation for metasomatic alteration; https://cir.nii.ac.jp/crid/1362825895594579072; 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; 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; Tectonic deformation: stress paths and strain histories; https://cir.nii.ac.jp/crid/1363951794404378112; Change in fabric of melange in the Shimanto Belt, Japan: Change in relative convergence?; https://cir.nii.ac.jp/crid/1363951795329529984; Evaluation of factors controlling smectite transformation and fluid production in subduction zones: Application to the Nankai Trough; https://cir.nii.ac.jp/crid/1364233269084464512; Peeling oceanic crust in subduction zones; https://cir.nii.ac.jp/crid/1364233269756845440; Low‐frequency tremors associated with reverse faults in a shallow accretionary prism; https://cir.nii.ac.jp/crid/1570009750829304960
• 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: 学術機関リポジトリデータベース; https://irdb.nii.ac.jp; 雑誌記事索引データベース; https://ndlsearch.ndl.go.jp; Crossref; https://www.crossref.org; CiNii Articles; 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）: 9227768; http://id.ndl.go.jp/bib/9227768
• NII論文ID: 120005464722