Geological evidence for shallow ductile-brittle transition zones along subduction interfaces : example from the Shimanto Belt, SW Japan
Available in National Diet Library
Find on the publisher's website
NDL Digital Collections
Digital data available
Check on the publisher's website
DOI[10.1186/s40623-014-0141-7]to the data of the same series
Holdings of Libraries in Japan
This page shows libraries in Japan other than the National Diet Library that hold the material.
Please contact your local library for information on how to use materials or whether it is possible to request materials from the holding libraries.
other
CiNii Research
Search ServicePaperYou can check the holdings of institutions and databases with which CiNii Research is linked at the site of CiNii Research.CiNii Research
Search ServiceDigitalYou can check the holdings of institutions and databases with which CiNii Research is linked at the site of CiNii Research.
Bibliographic Record
You can check the details of this material, its authority (keywords that refer to materials on the same subject, author's name, etc.), etc.
- Material Type
- 記事
- Author/Editor
- Yoshitaka HashimotoNatsuko Yamano
- Publication, Distribution, etc.
- Publication Date
- 2014-10-16
- Publication Date (W3CDTF)
- 2014-10-16
- Periodical title
- EPS : Earth, Planets and Space
- No. or year of volume/issue
- 66(141)
- Volume
- 66(141)
- ISSN (Periodical Title)
- 1880-5981
- ISSN-L (Periodical Title)
- 1343-8832
- Text Language Code
- eng
- DOI
- 10.1186/s40623-014-0141-7
- Persistent ID (NDL)
- info:ndljp/pid/9227896
- 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)
- 9227896
- Bibliographic Record Category (NDL)
- 632
- Summary, etc.
- 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/s40623-014-0141-7
- Access Restrictions
- インターネット公開
- Related Material (URI)
- Is Referenced By
- Quantitative estimation of fluid pressure ratio of shear vein in an on-land accretionary complex, the Yokonami mélange, the Cretaceous Shimanto Belt, Kochi, southwest JapanDeformation characteristics and peak temperatures of the Sanbagawa Metamorphic and Shimanto Accretionary complexes on the central Kii Peninsula, SW JapanTerrestrial and marine organic matter evidence from a Cretaceous deep-sea chert of Japan: Implications for enhanced hydrological cycle during the Aptian OAE 1a
- References
- Dynamic deformation of the accretionary prism excites very low frequency earthquakes“Block-in-matrix" fabrics that lack shearing but possess composite cleavage planes: A sedimentary mélange origin for the Yuwan accretionary complex in the Ryukyu island arc, JapanEpisodic slow slip events in the Japan subduction zone before the 2011 Tohoku-Oki earthquakeAccretionary prisms in subduction earthquake cycles: The theory of dynamic Coulomb wedgeHydrogeology and Mechanics of Subduction Zone Forearcs: Fluid Flow and Pore PressurePressure solution lithification as a mechanism for the stick‐slip behavior of faultsA new source of water in seismogenic subduction zonesFrequency-size distribution of competent lenses in a block-in-matrix mélange: Imposed length scales of brittle deformation?Underplated units in an accretionary complex: Melange of the Shimanto Belt of eastern Shikoku, southwest JapanPseudotachylytes in an ancient accretionary complex and implications for melt lubrication during subduction zone earthquakesTsunamigenic potential of the shallow subduction plate boundary inferred from slow seismic slipShallow Dynamic Overshoot and Energetic Deep Rupture in the 2011 <i>M</i> <sub>w</sub> 9.0 Tohoku-Oki EarthquakeEpisodic slow slip events accompanied by non‐volcanic tremors in southwest Japan subduction zoneFluid inclusionsExperimental stretching of fluid inclusions in calcite—Implications for diagenetic studiesLarge amount of fluid migration around shallow seismogenic depth preserved in tectonic mélange: Yokonami mélange, the Cretaceous Shimanto Belt, Kochi, Southwest JapanPropagation of Slow Slip Leading Up to the 2011 <i>M</i> <sub>w</sub> 9.0 Tohoku-Oki EarthquakeGeological and frictional aspects of very‐low‐frequency earthquakes in an accretionary prismAn analysis of the variation of ocean floor bathymetry and heat flow with ageMélange and its seismogenic roof décollement: A plate boundary fault rock in the subduction zone—An example from the Shimanto Belt, JapanPaleothermal structure of the Shimanto accretionary prism, Shikoku, Japan: Role of an out-of-sequence thrustThe thickness of subduction plate boundary faults from the seafloor into the seismogenic zoneGeology of the earthquake source: an introductionPseudotachylyte from an ancient accretionary complex: Evidence for melt generation during seismic slip along a master décollement?Geological record of fluid flow and seismogenesis along an erosive subducting plate boundaryTectonolithification of sandstone prior to the onset of seismogenic subduction zone: Evidence from tectonic mélange of the Shimanto Belt, JapanStructural evolution of underthrusted sediments, Kodiak Islands, AlaskaUpdip limit of the seismogenic zone beneath the accretionary prism of southwest Japan: An effect of diagenetic to low-grade metamorphic processes and increasing effective stressTectonic 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, JapanRecord of mega-earthquakes in subduction thrusts: The black fault rocks of Pasagshak Point (Kodiak Island, Alaska)Deformation mechanisms — recognition from natural tectonitesTransition of accretionary wedge structures around the up-dip limit of the seismogenic subduction zone<i>In situ</i> pressure–temperature conditions of a tectonic mélange: Constraints from fluid inclusion analysis of syn‐mélange veinsFractal vein distributions within a fault-fracture mesh in an exhumed accretionary mélange, Chrystalls Beach Complex, New ZealandHistory of metamorphic fluids along outcrop‐scale faults in a Paleogene accretionary prism, SW Japan: Implications for prism‐scale hydrologyMélange rheology and seismic styleA slow thrust slip event following the two 1996 Hyuganada Earthquakes beneath the Bungo Channel, southwest JapanEpisodic Tremor and Slip on the Cascadia Subduction Zone: The Chatter of Silent SlipThermal constraints on the zone of major thrust earthquake failure: The Cascadia Subduction ZoneDepth of oceanic-crust underplating in a subduction zone: Inferences from fluid-inclusion analyses of crack-seal veinsChange in fabric of melange in the Shimanto Belt, Japan: Change in relative convergence?Underplating process from melange formation to duplexing: Example from the Cretaceous Shimanto Belt, Kii Peninsula, southwest JapanP-T conditions of cataclastic deformation associated with underplating: An example from the Cretaceous Shimanto complex, Kii Peninsula, SW JapanAverage slip rate at the transition zone on the plate interface beneath the Kii Peninsula, Japan, estimated from deep low-frequency tremors
- Data Provider (Database)
- 国立情報学研究所 : CiNii Research
- Original Data Provider (Database)
- 雑誌記事索引データベースCrossref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CrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 9227896