Seismic imaging of slab metamorphism and genesis of intermediate-depth intraslab earthquakes
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- 資料種別
- 記事
- 著者・編者
- Akira HasegawaJunichi Nakajima
- 出版年月日等
- 2017-04-10
- 出版年（W3CDTF）
- 2017-04-10
- タイトル（掲載誌）
- Progress in earth and planetary science
- 巻号年月日等（掲載誌）
- 4(12)
- 掲載巻
- 4(12)
- ISSN（掲載誌）
- 2197-4284
- ISSN-L（掲載誌）
- 2197-4284
- 本文の言語コード
- eng
- DOI
- 10.1186/s40645-017-0126-9
- 国立国会図書館永続的識別子
- info:ndljp/pid/10369589
- コレクション（共通）
- コレクション（障害者向け資料：レベル1）
- 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
- 収集根拠
- オンライン資料収集制度
- 受理日（W3CDTF）
- 2017-06-29T04:49:44+09:00
- 保存日（W3CDTF）
- 2017-06-26
- 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（国立国会図書館永続的識別子）
- info:ndljp/pid/10369577
- 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
- 要約等
- 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/s40645-017-0126-9
- オンライン閲覧公開範囲
- インターネット公開
- 関連情報
- Seismic imaging of slab metamorphism and genesis of intermediate-depth intraslab earthquakes
- 関連情報（URI）
- 参照
- Diversity of deep earthquakes with waveform similarityAlong-strike forearc and subducted upper slab structure beneath north Chile: Slow slip implicationsRepeating EarthquakesStructural Heterogeneity in Source Zones of the 2018 Anchorage Intraslab Earthquake and the 1964 Alaska Megathrust EarthquakeThe Wakayama earthquake swarm in JapanAn Estimate of the Effect of 3D Heterogeneous Density Distribution on Coseismic Deformation Using a Spectral Finite-Element ApproachComplex rupture evolution of the 2007 Martinique earthquake: a non-double-couple event in the Caribbean SeaSemi-brittle deformation of antigorite serpentinite under forearc mantle wedge conditionsA weak subducting slab at intermediate depths below northeast JapanRevisiting Intraslab Earthquakes Beneath Kyushu, Japan: Effect of Ridge Subduction on SeismogenesisSeismic imaging of mantle wedge corner flow and arc magmatism内陸地殻およびスラブ内の繰り返し地震とその地震学的およびテクトニクス的意義三重地震面再訪Isolated intermediate-depth seismicity north of the Izu peninsula, Japan : implications for subduction of the Philippine Sea Plate
- 参照
- Three-dimensional structure of V_p, V_s, and V_p/V_s beneath northeastern Japan: Implications for arc magmatism and fluidsSeismic evidence for thermally-controlled dehydration reaction in subducting oceanic crustThree-dimensional seismic velocity structure and configuration of the Philippine Sea slab in southwestern Japan estimated by double-difference tomographyTomographic evidence for hydrated oceanic crust of the Pacific slab beneath northeastern Japan: Implications for water transportation in subduction zonesSeismotectonics beneath the Tokyo metropolitan area, Japan: Effect of slab-slab contact and overlap on seismicityAnomalous deepening of a belt of intraslab earthquakes in the Pacific slab crust under Kanto, central Japan: Possible anomalous thermal shielding, dehydration reactions, and seismicity caused by shallower cold slab materialSystematic changes in the incoming plate structure at the Kuril trenchTomographic imaging of hydrated crust and mantle in the subducting Pacific slab beneath Hokkaido, Japan: Evidence for dehydration embrittlement as a cause of intraslab earthquakesCause of <i>M</i> ∼ 7 intraslab earthquakes beneath the Tokyo metropolitan area, Japan: Possible evidence for a vertical tear at the easternmost portion of the Philippine Sea slabSubduction of a wedge‐shaped Philippine Sea plate beneath Kanto, central Japan, estimated from converted waves and small repeating earthquakesSeismic evidence for reactivation of a buried hydrated fault in the Pacific slab by the 2011 M9.0 Tohoku earthquakeInterslab earthquakes and phase changes in subducting lithosphereNew geophysical insight into the origin of the Denali volcanic gapDouble-planed deep seismic zone and upper-mantle structure in the Northeastern Japan ArcAn inverted continental Moho and serpentinization of the forearc mantleImpact of bending related faulting on the seismic properties of the incoming oceanic plate offshore of NicaraguaDetermination of the isotropic component of deep focus earthquakes by inversion of normal-mode dataExperimental “sytectonic” dehydration of serpentinite under conditions of controlled pore water pressureDeep-Focus Earthquakes and Recycling of Water into the Earth's MantleDeep slab hydration induced by bending-related variations in tectonic pressureSeismic evidence of a two-layer lithospheric deformation in the Indian OceanAntigorite: High-pressure stability in the system MgOSiO2H2O (MSH)Subduction factory 2. Are intermediate‐depth earthquakes in subducting slabs linked to metamorphic dehydration reactions?Deformation of antigorite serpentinite at high temperature and pressureA new analysis of the great 1970 Colombia earthquake and its isotropic componentDeep seismic structureDehydration kinetics of antigorite using in situ high-temperature infrared microspectroscopyThermal–petrological controls on the location of earthquakes within subducting platesIntermediate-depth earthquakes facilitated by eclogitization-related stressesHigh Pore Fluid Pressure May Cause Silent Slip in the Nankai TroughDouble-Difference Tomography: The Method and Its Application to the Hayward Fault, CaliforniaDouble seismic zone of the Nazca plate in northern Chile: High‐resolution velocity structure, petrological implications, and thermomechanical modelingGeophysical evidence for hydration of the crust and mantle of the Nazca plate during bending at the north Chile trenchPressure–temperature conditions of ongoing regional metamorphism beneath the Japanese IslandsGlobal teleseismic earthquake relocation with improved travel times and procedures for depth determinationAnomalous deepening of a seismic belt in the upper-plane of the double seismic zone in the Pacific slab beneath the Hokkaido corner: Possible evidence for thermal shielding caused by subducted forearc crust materialsEarthquakes and plastic deformation of anhydrous slab mantle in double Wadati‐Benioff zonesExperimentally based water budgets for dehydrating slabs and consequences for arc magma generationBending-related faulting and mantle serpentinization at the Middle America trenchOn the extent of mantle hydration caused by plate bendingWestern Nankai Trough seismogenic zone: Results from a wide‐angle ocean bottom seismic surveySerpentine Stability to Mantle Depths and Subduction-Related MagmatismObservability of the isotropic component of a moment tensorImaging the source region of Cascadia tremor and intermediate-depth earthquakes<i>P</i> wave tomographic imaging of the crust and upper mantle beneath the Japan IslandsSpreading rate dependence of gravity anomalies along oceanic transform faultsSimultaneous acoustic emissions monitoring and synchrotron X-ray diffraction at high pressure and temperature: Calibration and application to serpentinite dehydrationDeep EarthquakesDouble seismic zone beneath the middle of Hokkaido, Japan, in the southwestern side of the Kurile ArcA double‐layered seismic zone in Arica, northern ChileRelationship between shallow‐ and intermediate‐depth seismicity in the Eastern Aleutian Subduction ZoneA seismological constraint on the depth of basalt–eclogite transition in a subducting oceanic crustUpper mantle velocity structure estimated from PS-converted wave beneath the north-eastern Japan ArcExperimental deformation of serpentinite and its tectonic implicationsSeismic detection of the untransformed 'basaltic' oceanic crust subducting into the mantleRadial modes from the great 1994 Bolivian earthquake: No evidence for an isotropic component to the sourceAre the lower planes of double seismic zones caused by serpentine dehydration in subducting oceanic mantle?Subduction factory 1. Theoretical mineralogy, densities, seismic wave speeds, and H<sub>2</sub>O contentsHigh-resolution subducting-slab structure beneath northern Honshu, Japan, revealed by double-difference tomographyDouble-planed structure of the deep seismic zone in the northeastern Japan arcSeismic imaging of subduction zone metamorphismStrain Localization and Slip Instability in a Strain-Rate Hardening, Chemically Weakening MaterialPaleogeographic reconstruction and origin of the Philippine SeaSeismic Consequences of Warm Versus Cool Subduction Metamorphism: Examples from Southwest and Northeast JapanUpper lithospheric structure of the subduction zone offshore of southern Arauco peninsula, Chile, at ∼38°SSignificance of non-double couple components of deep and intermediate-depth earthquakes: implications from moment tensor inversions of long-period seismic wavesRole of pore fluid pressure on transient strength changes and fabric development during serpentine dehydration at mantle conditions: Implications for subduction-zone seismicityA periodic shear-heating mechanism for intermediate-depth earthquakes in the mantleExperimental Faulting of Serpentinite during Dehydration: Implications for Earthquakes, Seismic Low-Velocity Zones, and Anomalous Hypocenter Distributions in Subduction ZonesUnbending combined with dehydration embrittlement as a cause for double and triple seismic zonesDeep seismic structure of the Tonga subduction zone: Implications for mantle hydration, tectonic erosion, and arc magmatismEvidence for both crustal and mantle earthquakes in the subducting Juan de Fuca plateShear instability in a viscoelastic material as the cause of deep focus earthquakesGeophysical constraints on slab subduction and arc magmatismH<sub>2</sub>O subduction beyond arcsDouble seismic zone in TongaSections of the Earth's crust in the equatorial AtlanticEffect of pore geometry on <i>V</i><sub><i>P</i></sub>/<i>V</i><sub><i>S</i></sub>: From equilibrium geometry to crackRecycled dehydrated lithosphere observed in plume-influenced mid-ocean-ridge basaltRelationship between bend‐faulting at trenches and intermediate‐depth seismicityIntermediate-depth earthquake faulting by dehydration embrittlement with negative volume changeSeismic waves guided by untransformed oceanic crust subducting into the mantle: the case of the Kanto district, central JapanLocalized polymorphic phase transformations in high‐pressure faults and applications to the physical mechanism of deep earthquakesA three-dimensional image of shallow subduction: crustal structure of the Raukumara Peninsula, New ZealandExistence of a seismic belt in the upper plane of the double seismic zone extending in the along‐arc direction at depths of 70–100 km beneath NE JapanGlobal Prevalence of Double Benioff ZonesDeep-Focus Earthquakes and Their Geological SignificanceThe Mechanics of Deep EarthquakesSubducting plate boundary beneath the northeastern Japan arc estimated from SP converted wavesHigh‐resolution subduction zone seismicity and velocity structure beneath Ibaraki Prefecture, JapanDo intermediate‐ and deep‐focus earthquakes occur on preexisting weak zones? An examination of the Tonga subduction zoneDeformation mechanisms of antigorite serpentinite at subduction zone conditions determined from experimentally and naturally deformed rocksLarge scale isotopic Sr, Nd and O isotopic anatomy of altered oceanic crust: DSDP/ODP sites417/418Common depth of slab‐mantle decoupling: Reconciling diversity and uniformity of subduction zonesTectonic Implications of Serpentinite WeakeningSeismicity of the Gorda Plate, structure of the continental margin, and an eastward jump of the Mendocino Triple JunctionPlate coupling in the northern South Island and southernmost North Island, New Zealand, as illuminated by earthquake focal mechanismsRheological structure and deformation of subducted slabs in the mantle transition zone: implications for mantle circulation and deep earthquakesDowndip tensional earthquakes beneath the Tonga Arc: A double seismic zone?A break in the deepBody wave inversion of the 1970 and 1963 South American large deep‐focus earthquakesPlastic instabilities: Implications for the origin of intermediate and deep focus earthquakesGeneration and maintenance of pore pressure excess in a dehydrating system 1. Experimental and microstructural observations41 Global seismicity: 1900–1999Simulation of Subduction Zone Seismicity by Dehydration of SerpentineDehydration of lawsonite could directly trigger earthquakes in subducting oceanic crustFaulting associated with the olivine to spinel transformation in Mg<sub>2</sub>GeO<sub>4</sub> and its implications for deep‐focus earthquakesSerpentine and the subduction zone water cycleThe role of fluid pressure on frictional behavior at the base of the seismogenic zoneSystem for detecting acoustic emissions in multianvil experiments: Application to deep seismicity in the EarthSeismic evidence for dehydration embrittlement of the subducting Pacific slabControls of faulting and reaction kinetics on serpentinization and double Benioff zonesHigh‐resolution models of subduction zones: Implications for mineral dehydration reactions and the transport of water into the deep mantleDeep EarthquakesSpatial distribution of focal mechanisms for interplate and intraplate earthquakes associated with the subducting Pacific plate beneath the northeastern Japan arc: A triple‐planed deep seismic zoneMorphology of the subducting slab boundary in the northeastern Japan arcTomographic imaging of <i>P</i> and <i>S</i> wave velocity structure beneath northeastern JapanDetailed structures of the subducted Philippine Sea Plate beneath northeast Taiwan: A new type of double seismic zoneOblique subduction and collision: Forearc tectonics of the Kuril arcA new self-organizing mechanism for deep-focus earthquakesDouble seismic zone and dehydration embrittlement of the subducting slabThe relationship of intermediate- and deep-focus seismicity to the hydration and dehydration of subducting slabsCrustal heterogeneity and subduction processes: 3-D<i>Vp, Vp/Vs</i>and<i>Q</i>in the southern North Island, New ZealandFault plane orientations of intermediate‐depth earthquakes in the Middle America TrenchPlate subduction, and generation of earthquakes and magmas in Japan as inferred from seismic observations: An overviewSeismic tomography and earthquake locations in the Nicaraguan and Costa Rican upper mantleFluid flow during slab unbending and dehydration: Implications for intermediate‐depth seismicity, slab weakening and deep water recycling3-D imaging of the northern Hikurangi subduction zone, New Zealand: variations in subducted sediment, slab fluids and slow slipHydrated subducted crust at 100–250 km depth日本列島下のスラブの三次元構造と地震活動Tomographic evidence for the mantle upwelling beneath southwestern Japan and its implications for arc magmatismWhat controls interplate coupling?: Evidence for abrupt change in coupling across a border between two overlying plates in the NE Japan subduction zone
- 参照（URI）
- 連携機関・データベース
- 国立情報学研究所 : CiNii Research
- 提供元機関・データベース
- 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学術機関リポジトリデータベースCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- 書誌ID（NDLBibID）
- 10369589