Stress reversal recorded in calcite vein cuttings from the Nankai accretionary prism, southwest Japan

• 資料種別: 記事
• タイトル: Stress reversal recorded in calcite vein cuttings from the Nankai accretionary prism, southwest Japan
• 著者・編者: Toru Takeshita; Asuka Yamaguchi; Norio Shigematsu
• 出版事項: 日本 : Springer science+business media
• 出版年月日等: 2014-10-29
• 出版年（W3CDTF）: 2014-10-29
• タイトル（掲載誌）: EPS : Earth, Planets and Space
• 巻号年月日等（掲載誌）: 66(144)
• 掲載巻: 66(144)
• 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/s40623-014-0144-4; https://doi.org/10.1186/s40623-014-0144-4
• 国立国会図書館永続的識別子: info:ndljp/pid/9227898; https://dl.ndl.go.jp/pid/9227898
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• 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
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• 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
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• 請求記号: Z19-292
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• 書誌ID（NDLBibID）: 9227898; http://id.ndl.go.jp/bib/9227898
• 整理区分コード: 632

• 要約等: The Nankai Trough subduction zone in southwest Japan is a typical convergent margin where the Philippine Sea plate subducts in the northwest direction beneath the Eurasian plate, and devastating earthquakes have repeatedly occurred in this region in the past. In order to investigate the evolution of the stress state in the subduction zone, we analyzed deformation microstructures and the preferred orientation of calcite grains in two cuttings of calcite veins from Hole C0002F that was drilled through the inner wedge of the Nankai accretionary prism during the Integrated Ocean Discovery Program (IODP) Expedition 338 in 2012. For both samples collected at depths of 1,085.5 and 1,885.5 meters below the sea floor (mbsf), the c-axes of calcite grains are preferentially oriented perpendicular to the vein wall, which is indicative of competitive growth of calcite during the vein opening caused by a vein normal extension. Also, mechanical e-twins were developed in both samples, and these are inferred to have been developed under the same stress field as that responsible for the formation of calcite veins based on the paleostress analyses in grains with e-twins. For the calcite vein retrieved at the depth of 1,885.5 mbsf, kink bands were also developed by the compression in the direction perpendicular to the vein wall, which is indicative of stress reversal after the formation of mechanical e-twins. Although we could not reach a definite conclusion for the cause of the stress reversal, it could have occurred during either fold development or seismic cycles in the Nankai accretionary prism.
• DOI: 10.1186/s40623-014-0144-4; https://doi.org/10.1186/s40623-014-0144-4
• 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 4.0 International
• 関連情報（URI）: https://hdl.handle.net/2115/57785; http://id.ndl.go.jp/digimeta/9227898; https://dl.ndl.go.jp/pid/9227898; http://link.springer.com/article/10.1186/s40623-014-0144-4/fulltext.html; http://link.springer.com/content/pdf/10.1186/s40623-014-0144-4.pdf; http://link.springer.com/content/pdf/10.1186/s40623-014-0144-4; http://hdl.handle.net/2115/57785
• 参照: 応力逆解析手法の発展と応用; https://cir.nii.ac.jp/crid/1390001206239580416; Experiments on method for washing drill cuttings: evaluation of soaking, stirring, and milling effects; https://cir.nii.ac.jp/crid/1390282680294647168
• 参照: Stress field observation and modeling from the NanTroSEIZE scientific drillings in the Nankai Trough system, SW Japan; https://cir.nii.ac.jp/crid/1360004232523359104; Evidence for mechanical decoupling of the upper plate at the Nankai subduction zone: Constraints from core‐scale faults at NantroSEIZE Sites C0001 and C0002; https://cir.nii.ac.jp/crid/1360004233289870976; Stress states at the subduction input site, Nankai Subduction Zone, using anelastic strain recovery (ASR) data in the basement basalt and overlying sediments; https://cir.nii.ac.jp/crid/1360285707500062720; Crustal velocity field of southwest Japan: Subduction and arc‐arc collision; https://cir.nii.ac.jp/crid/1360292617909503360; Source mechanisms and tectonic significance of historical earthquakes along the nankai trough, Japan; https://cir.nii.ac.jp/crid/1360292617916830848; A review of the formation of tectonic veins and their microstructures; https://cir.nii.ac.jp/crid/1360292618644075648; Interseismic stress accumulation at the locked zone of Nankai Trough seismogenic fault off Kii Peninsula; https://cir.nii.ac.jp/crid/1360567182476777984; Complex Ruptures of the 11 April 2011 Mw 6.6 Iwaki Earthquake Triggered by the 11 March 2011 Mw 9.0 Tohoku Earthquake, Japan; https://cir.nii.ac.jp/crid/1360848663120748160; A model for the motion of the Philippine Sea Plate consistent with NUVEL‐1 and geological data; https://cir.nii.ac.jp/crid/1360855567866336512; NanTroSEIZE: The IODP Nankai Trough Seismogenic Zone Experiment; https://cir.nii.ac.jp/crid/1360855567869180160; Magnetic anomalies in the Shikoku Basin: a new interpretation; https://cir.nii.ac.jp/crid/1360855567870246912; c-Axis fabrics and microstructures in a recrystallized quartz vein deformed under fluid-rich greenschist conditions; https://cir.nii.ac.jp/crid/1360855569113841024; Mechanisms of fluid flow and fluid–rock interaction in fossil metamorphic hydrothermal systems inferred from vein–wallrock patterns, geometry and microstructure; https://cir.nii.ac.jp/crid/1360855569755699072; Stress switching in subduction forearcs: Implications for overpressure containment and strength cycling on megathrusts; https://cir.nii.ac.jp/crid/1361418520535566208; Dynamic changes in fluid redox state associated with episodic fault rupture along a megasplay fault in a subduction zone; https://cir.nii.ac.jp/crid/1362262944430116480; Genetic links among fluid cycling, vein formation, regional deformation, and plutonism in the Juneau gold belt, southeastern Alaska; https://cir.nii.ac.jp/crid/1362544418888763136; Stress-history of folding; https://cir.nii.ac.jp/crid/1362825894291980288; Origin of lode-gold deposits of the Juneau gold belt, southeastern Alaska; https://cir.nii.ac.jp/crid/1362825895037935744; Dynamic analysis and two types of kink bands in quartz veins deformed under subgreenschist conditions; https://cir.nii.ac.jp/crid/1362825895822200832; Low-temperature deformation in calcite veins of SAFOD core samples (San Andreas Fault) — Microstructural analysis and implications for fault rheology; https://cir.nii.ac.jp/crid/1362825896076824576; EXPERIMENTAL DEFORMATION OF CALCITE CRYSTALS; https://cir.nii.ac.jp/crid/1363388843487132928; Kinematics of crystal growth in syntectonic fibrous veins; https://cir.nii.ac.jp/crid/1363388845265547008; Implications of fault-valve behaviour for rupture nucleation and recurrence; https://cir.nii.ac.jp/crid/1363951795302132608; Seismic reflection and bathymetric evidences for the Nankai earthquake rupture across a stable segment-boundary; https://cir.nii.ac.jp/crid/2051151842091770240; Nearly complete stress drop in the 2011 Mw 9.0 off the Pacific coast of Tohoku Earthquake; https://cir.nii.ac.jp/crid/2051433317068452224; A normal-faulting seismic sequence triggered by the 2011 off the Pacific coast of Tohoku Earthquake : wholesale stress regime changes in the upper plate; https://cir.nii.ac.jp/crid/2051714792045164672; Shallow inland earthquakes in NE Japan possibly triggered by the 2011 off the Pacific coast of Tohoku Earthquake; https://cir.nii.ac.jp/crid/2051996267021875328
• 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）: 9227898; http://id.ndl.go.jp/bib/9227898
• NII論文ID: 120005530837