Non-volcanic seismic swarm and fluid transportation driven by subduction of the Philippine Sea slab beneath the Kii Peninsula, Japan
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DOI[10.1186/1880-5981-66-86]to the data of the same series
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- Material Type
- 記事
- Author/Editor
- Aitaro KatoAtsushi SaigaTetsuya Takeda
- Publication, Distribution, etc.
- Publication Date
- 2014-08-04
- Publication Date (W3CDTF)
- 2014-08-04
- Periodical title
- EPS : Earth, Planets and Space
- No. or year of volume/issue
- 66(86)
- Volume
- 66(86)
- ISSN (Periodical Title)
- 1880-5981
- ISSN-L (Periodical Title)
- 1343-8832
- Text Language Code
- eng
- DOI
- 10.1186/1880-5981-66-86
- Persistent ID (NDL)
- info:ndljp/pid/9227841
- 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)
- 2014-10-10
- 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/3427598
- 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)
- 9227841
- 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
- 10.1186/1880-5981-66-86
- Access Restrictions
- インターネット公開
- Related Material (URI)
- Is Referenced By
- Complex microseismic activity and depth-dependent stress field changes in Wakayama, southwestern JapanPossible slow slip event beneath the Kii Peninsula, southwest Japan, inferred from historical tilt records in 1973Special issue ‘Geofluid processes in subduction zones and mantle dynamics’Deep plutonic bodies over low-frequency earthquakes revealed from receiver-side Green's functionsTriggering of earthquake swarms following the 2011 Tohoku megathrust earthquakeDown-dip variations in a subducting low-velocity zone linked to episodic tremor and slip: a new constraint from ScSp wavesThe Role of Fluid‐Related Heterogeneous Structures in Controlling the Fault Slip Behavior in the Slow‐Earthquake Source Region Along the Nankai Subduction Zone, Southwest JapanSeismological evidence of a dehydration reaction in the subducting oceanic crust beneath western Shikoku in southwest JapanWhat makes low-frequency earthquakes low frequencyWidespread distribution of ascending fluids transporting mantle helium in the fore-arc region and their upwelling processes: Noble gas and major element composition of deep groundwater in the Kii Peninsula, southwest JapanThe Wakayama earthquake swarm in JapanExperimental constraints on the serpentinization rate of fore‐arc peridotites: Implications for the upwelling condition of the slab‐derived fluidHydrous state of the subducting Philippine Sea plate inferred from receiver function image using onshore and offshore dataUltramafic Rocks from the Sanbagawa Belt: Records of Mantle Wedge ProcessesThermochronology of hydrothermal alteration zones in the Kii Peninsula, southwest Japan: an attempt for detecting the thermal anomalies and implications to the regional exhumation historyInfluence of crustal lithology and the thermal state on microseismicity in the Wakayama region, southern Honshu, JapanVelocity increase in the uppermost oceanic crust of subducting Philippine Sea plate beneath the Kanto region due to dehydration inferred from high-frequency trapped P wavesAmbient noise tomography for a high-resolution 3D S-wave velocity model of the Kinki Region, Southwestern Japan, using dense seismic array data
- References
- Three-dimensional structure of V_p, V_s, and V_p/V_s beneath northeastern Japan: Implications for arc magmatism and fluidsThree-dimensional seismic velocity structure and configuration of the Philippine Sea slab in southwestern Japan estimated by double-difference tomographySubducting Slab Ultra-Slow Velocity Layer Coincident with Silent Earthquakes in Southern MexicoCracked media, Poisson's ratio and the structure of the upper oceanic crustFluid and deformation regime of an advancing subduction system at Marlborough, New ZealandPore pressure and oceanic crustal seismic structureWater transportation through the Philippine Sea slab subducting beneath the central Kyushu region, Japan, as derived from receiver function analysesDouble-Difference Tomography: The Method and Its Application to the Hayward Fault, CaliforniaAnisotropic structures of oceanic slab and mantle wedge in a deep low‐frequency tremor zone beneath the Kii Peninsula, SW JapanSeismicity-based estimation of the driving fluid pressure in the case of swarm activity in Western BohemiaMaximum-likelihood estimation of hypocenter with origin time eliminated using nonlinear inversion techniqueChanges in effective stress during the 2003–2004 Ubaye seismic swarm, FranceImaging the source region of Cascadia tremor and intermediate-depth earthquakesSlow Earthquakes, Preseismic Velocity Changes, and the Origin of Slow Frictional Stick-SlipA seismological constraint on the depth of basalt–eclogite transition in a subducting oceanic crustThe Removal of Free Surface Interactions From Three-Component SeismogramsSubduction factory 1. Theoretical mineralogy, densities, seismic wave speeds, and H<sub>2</sub>O contentsSeismic velocities in dry and saturated cracked solidsHydrologic control of forearc strength and seismicity in the Costa Rican subduction zoneRegionality of deep low-frequency earthquakes associated with subduction of the Philippine Sea plate along the Nankai Trough, southwest JapanSeismic evidence for overpressured subducted oceanic crust and megathrust fault sealingThree‐dimensional <i>P</i> wave velocity model for the San Francisco Bay region, CaliforniaConstitutive properties for the shear failure of intact granite in seismogenic environmentsEffect of pore geometry on <i>V</i><sub><i>P</i></sub>/<i>V</i><sub><i>S</i></sub>: From equilibrium geometry to crackThe role of fluids in lower-crustal earthquakes near continental riftsAqueous fluids derived from a subducting slab: Observed high 3He emanation and conductive anomaly in a non-volcanic region, Kii Peninsula southwest JapanSeismic and geodetic evidence for the existence of hot materials beneath the Wakayama swarm activity, southwestern JapanEvidence for water‐filled cracks in earthquake source regionsA survey of 71 earthquake bursts across southern California: Exploring the role of pore fluid pressure fluctuations and aseismic slip as driversLocal earthquake tomography with flexible griddingPoisson's ratio and crustal seismologySeismicity patterns of earthquake swarms due to fluid intrusion and stress triggeringThe isolation of receiver effects from teleseismic<i>P</i>waveformsRegional variations of the cutoff depth of seismicity in the crust and their relation to heat flow and large inland-earthquakes.Geothermal gradient and heat flow data in and around Japan (I): apprasial of heat flow from geothermal gradient dataLow Vp and Vp/Vs zone beneath the northern Fossa Magna basin, central Japan, derived from a dense array observationGeophysical assessment of migration and storage conditions of fluids in subduction zones
- 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CrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 9227841