Stress reversal recorded in calcite vein cuttings from the Nankai accretionary prism, southwest Japan
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DOI[10.1186/s40623-014-0144-4]to the data of the same series
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- Material Type
- 記事
- Author/Editor
- Toru TakeshitaAsuka YamaguchiNorio Shigematsu
- Publication, Distribution, etc.
- Publication Date
- 2014-10-29
- Publication Date (W3CDTF)
- 2014-10-29
- Periodical title
- EPS : Earth, Planets and Space
- No. or year of volume/issue
- 66(144)
- Volume
- 66(144)
- ISSN (Periodical Title)
- 1880-5981
- ISSN-L (Periodical Title)
- 1343-8832
- Text Language Code
- eng
- DOI
- 10.1186/s40623-014-0144-4
- Persistent ID (NDL)
- info:ndljp/pid/9227898
- Collection
- Collection (Materials For Handicapped People:1)
- 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
- Acquisition Basis
- オンライン資料収集制度
- Date Accepted (W3CDTF)
- 2015-04-17T10:30:12+09:00
- Date Captured (W3CDTF)
- 2014-12-20
- Format (IMT)
- application/pdf
- Access Restrictions
- 国立国会図書館内限定公開
- Service for the Digitized Contents Transmission Service
- 図書館・個人送信対象外
- Availability of remote photoduplication service
- 可
- Periodical Title (URI)
- Periodical Title (Persistent ID (NDL))
- info:ndljp/pid/9227755
- 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
- Collection (particular)
- 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
- Access Restrictions
- 国立国会図書館内限定公開
- Service for the Digitized Contents Transmission Service
- 図書館・個人送信対象外
- Availability of remote photoduplication service
- 可
- Holding library
- 国立国会図書館
- Call No.
- Z19-292
- Periodical Title (Persistent ID (NDL))
- info:ndljp/pid/3427605
- Data Provider (Database)
- 国立国会図書館 : 国立国会図書館雑誌記事索引
- Bibliographic ID (NDL)
- 9227898
- Bibliographic Record Category (NDL)
- 632
- Summary, etc.
- 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
- Access Restrictions
- インターネット公開
- Rights (production)
- Creative Commons Attribution 4.0 International
- Related Material (URI)
- Is Referenced By
- 応力逆解析手法の発展と応用Experiments on method for washing drill cuttings: evaluation of soaking, stirring, and milling effects
- References
- Stress field observation and modeling from the NanTroSEIZE scientific drillings in the Nankai Trough system, SW JapanEvidence for mechanical decoupling of the upper plate at the Nankai subduction zone: Constraints from core‐scale faults at NantroSEIZE Sites C0001 and C0002Stress states at the subduction input site, Nankai Subduction Zone, using anelastic strain recovery (ASR) data in the basement basalt and overlying sedimentsCrustal velocity field of southwest Japan: Subduction and arc‐arc collisionSource mechanisms and tectonic significance of historical earthquakes along the nankai trough, JapanA review of the formation of tectonic veins and their microstructuresInterseismic stress accumulation at the locked zone of Nankai Trough seismogenic fault off Kii PeninsulaComplex Ruptures of the 11 April 2011 Mw 6.6 Iwaki Earthquake Triggered by the 11 March 2011 Mw 9.0 Tohoku Earthquake, JapanA model for the motion of the Philippine Sea Plate consistent with NUVEL‐1 and geological dataNanTroSEIZE: The IODP Nankai Trough Seismogenic Zone ExperimentMagnetic anomalies in the Shikoku Basin: a new interpretationc-Axis fabrics and microstructures in a recrystallized quartz vein deformed under fluid-rich greenschist conditionsMechanisms of fluid flow and fluid–rock interaction in fossil metamorphic hydrothermal systems inferred from vein–wallrock patterns, geometry and microstructureStress switching in subduction forearcs: Implications for overpressure containment and strength cycling on megathrustsDynamic changes in fluid redox state associated with episodic fault rupture along a megasplay fault in a subduction zoneGenetic links among fluid cycling, vein formation, regional deformation, and plutonism in the Juneau gold belt, southeastern AlaskaStress-history of foldingOrigin of lode-gold deposits of the Juneau gold belt, southeastern AlaskaDynamic analysis and two types of kink bands in quartz veins deformed under subgreenschist conditionsLow-temperature deformation in calcite veins of SAFOD core samples (San Andreas Fault) — Microstructural analysis and implications for fault rheologyEXPERIMENTAL DEFORMATION OF CALCITE CRYSTALSKinematics of crystal growth in syntectonic fibrous veinsImplications of fault-valve behaviour for rupture nucleation and recurrenceSeismic reflection and bathymetric evidences for the Nankai earthquake rupture across a stable segment-boundaryNearly complete stress drop in the 2011 Mw 9.0 off the Pacific coast of Tohoku EarthquakeA normal-faulting seismic sequence triggered by the 2011 off the Pacific coast of Tohoku Earthquake : wholesale stress regime changes in the upper plateShallow inland earthquakes in NE Japan possibly triggered by the 2011 off the Pacific coast of Tohoku Earthquake
- Data Provider (Database)
- 国立情報学研究所 : CiNii Research
- Original Data Provider (Database)
- 学術機関リポジトリデータベース雑誌記事索引データベースCrossrefCiNii Articles科学研究費助成事業データベース科学研究費助成事業データベースCrossrefCrossref
- Bibliographic ID (NDL)
- 9227898
- NAID
- 120005530837