Simultaneous estimation of in situ porosity and thermal structure from core sample measurements and resistivity log data at Nankai accretionary prism
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- Material Type
- 記事
- Author/Editor
- Suguru YabeRina FukuchiYohei Hamada
- Publication, Distribution, etc.
- Publication Date
- 2019-11-07
- Publication Date (W3CDTF)
- 2019-11-07
- Periodical title
- EPS : Earth, Planets and Space
- No. or year of volume/issue
- 71(116)
- Volume
- 71(116)
- ISSN (Periodical Title)
- 1880-5981
- ISSN-L (Periodical Title)
- 1343-8832
- Text Language Code
- eng
- DOI
- 10.1186/s40623-019-1097-4
- Persistent ID (NDL)
- info:ndljp/pid/11467661
- 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)
- 2020-03-23T18:58:42+09:00
- Date Captured (W3CDTF)
- 2020-03-23
- 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/11245705
- 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
- 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/s40623-019-1097-4
- Access Restrictions
- インターネット公開
- Related Material (URI)
- Is Referenced By
- Thermal Conductivity Profile in the Nankai Accretionary Prism at IODP NanTroSEIZE Site C0002: Estimations From High‐Pressure Experiments Using Input Site SedimentsPaleo‐Permeability Structure of the Crustal Section of the Samail Ophiolite Based on Automated Detection of Veins in X‐Ray CT Core Images From the Oman Drilling ProjectMajor Mineral Fraction and Physical Properties of Carbonated Peridotite (Listvenite) From ICDP Oman Drilling Project Hole BT1B Inferred From X‐Ray CT Core ImagesDeformation Process and Mechanism of the Frontal Megathrust at the Nankai Subduction ZoneMultiple Types of Porosity – P‐Wave Velocity Relationships for the Nankai TroughA new method for the empirical conversion of logging data to clay mineral fraction in the Nankai accretionary prism
- References
- Slab dehydration and earthquake distribution beneath southwestern and central Japan based on three dimensional thermal modelingNear-trench slip potential of megaquakes evaluated from fault properties and conditions.Frictional properties of JFAST core samples and implications for slow earthquakes at the Tohoku subduction zoneDevelopment and Performance Tests of a Sensor Suite for a Long-Term Borehole Monitoring System in Seafloor Settings in the Nankai Trough, JapanThe origin of strata within the inner accretionary prism of Nankai Trough: Evidence from clay mineral assemblages along the NanTroSEIZE transectContinuous depth profile of the rock strength in the Nankai accretionary prism based on drilling performance parametersHeat flow estimated from BSR and IODP borehole data: Implication of recent uplift and erosion of the imbricate thrust zone in the Nankai Trough off KumanoCrustal velocity field of southwest Japan: Subduction and arc‐arc collisionSource mechanisms and tectonic significance of historical earthquakes along the nankai trough, JapanSite C0011Expedition 315 Site C0001Expedition 316 methodsSite C0022Mineralogy, porosity and fluid control on thermal conductivity of sedimentary rocksFluid transport properties in sediments and their role in large slip near the surface of the plate boundary fault in the Japan TrenchIn situ stress state in the Nankai accretionary wedge estimated from borehole wall failuresGas hydrate saturation at <scp>S</scp>ite <scp>C</scp>0002, <scp>IODP E</scp>xpeditions 314 and 315, in the <scp>K</scp>umano <scp>B</scp>asin, <scp>N</scp>ankai troughIn Situ Stress and Pore Pressure in the Deep Interior of the Nankai Accretionary Prism, Integrated Ocean Drilling Program Site C0002Proceedings of the Ocean Drilling Program, 156 Initial ReportsVariety and spatial heterogeneity of tectonic tremor worldwideElevated pore pressure and anomalously low stress in regions of low frequency earthquakes along the Nankai Trough subduction megathrustShallow very-low-frequency earthquakes accompany slow slip events in the Nankai subduction zoneRecurring and triggered slow-slip events near the trench at the Nankai Trough subduction megathrustConsolidation state of incoming sediments to the Nankai Trough subduction zone: Implications for sediment deformation and propertiesRunaway slip to the trench due to rupture of highly pressurized megathrust beneath the middle trench slope: The tsunamigenesis of the 2011 Tohoku earthquake off the east coast of northern JapanPresent‐day principal horizontal stress orientations in the Kumano forearc basin of the southwest Japan subduction zone determined from IODP NanTroSEIZE drilling Site C0009NanTroSEIZE: The IODP Nankai Trough Seismogenic Zone ExperimentA modified Archie’s law for two conducting phasesAn Empirical Relationship between Velocity and Porosity for Underthrust Sediments in the Nankai Trough Accretionary PrismExpedition 315 Site C0002Expedition 322 summaryInterpretation of porosity and LWD resistivity from the Nankai accretionary wedge in light of clay physicochemical properties: Evidence for erosion and local overpressuringSite C0011Ocean Floor Networks Capture Low-Frequency Earthquake EventExpedition 316 Site C0004Lithostratigraphy of the Taiwan Chelungpu-Fault Drilling Project-A Borehole and Its Neighboring Region, Central TaiwanExpedition 316 summaryHeat flow along the NanTroSEIZE transect: Results from IODP Expeditions 315 and 316 offshore the Kii Peninsula, JapanSite C0012Site C0009Examination of gas hydrate-bearing deep ocean sediments by X-ray Computed Tomography and verification of physical property measurements of sedimentsExpedition 316 Site C0006Exponential approximations to compacted sediment porosity profilesUpdip limit of the seismogenic zone beneath the accretionary prism of southwest Japan: An effect of diagenetic to low-grade metamorphic processes and increasing effective stressExpedition 314 Site C0002Distribution of resistive and conductive structures in Nankai accretionary wedge reveals contrasting stress pathsSite C0012Spatiotemporal distribution of very-low frequency earthquakes in Tokachi-oki near the junction of the Kuril and Japan trenches revealed by using array signal processingExpedition 316 Site C0008Site C0018Anelastic strain recovery reveals extension across SW Japan subduction zoneSubduction factory: 4. Depth-dependent flux of H<sub>2</sub>O from subducting slabs worldwideSite C0021Expedition 315 methodsSegmentation of X‐ray computed tomography images of porous materials: A crucial step for characterization and quantitative analysis of pore structuresExpedition 316 Site C0007Expedition 314 methodsHeat flow in South AfricaSite C0002Site C0002Fault stability inferred from granite sliding experiments at hydrothermal conditionsSite C0010Origin and evolution of a splay fault in the Nankai accretionary wedgeRe-evaluation of temperature at the updip limit of locked portion of Nankai megasplay inferred from IODP Site C0002 temperature observatoryDistribution and depth of bottom-simulating reflectors in the Nankai subduction margin
- References (URI)
- 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CrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 11467661