Simultaneous estimation of in situ porosity and thermal structure from core sample measurements and resistivity log data at Nankai accretionary prism

• 資料種別: 記事
• タイトル: Simultaneous estimation of in situ porosity and thermal structure from core sample measurements and resistivity log data at Nankai accretionary prism
• 著者・編者: Suguru Yabe; Rina Fukuchi; Yohei Hamada
• 出版事項: 日本 : Springer Nature
• 出版年月日等: 2019-11-07
• 出版年（W3CDTF）: 2019-11-07
• タイトル（掲載誌）: EPS : Earth, Planets and Space
• 巻号年月日等（掲載誌）: 71(116)
• 掲載巻: 71(116)
• ISSN（掲載誌）: 1880-5981
• ISSN-L（掲載誌）: 1343-8832
• 本文の言語コード: eng
• DOI: 10.1186/s40623-019-1097-4; https://doi.org/10.1186/s40623-019-1097-4
• 国立国会図書館永続的識別子: info:ndljp/pid/11467661; https://dl.ndl.go.jp/pid/11467661
• コレクション（共通）: 障害者向け資料
• コレクション（障害者向け資料：レベル1）: テキストデータ
• 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; https://dl.ndl.go.jp/collections/B00035
• 収集根拠: オンライン資料収集制度
• 受理日（W3CDTF）: 2020-03-23T18:58:42+09:00
• 保存日（W3CDTF）: 2020-03-23
• 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（URI）: https://earth-planets-space.springeropen.com/articles
• 掲載誌（国立国会図書館永続的識別子）: info:ndljp/pid/11245705; https://dl.ndl.go.jp/pid/11245705
• 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; https://dl.ndl.go.jp

• 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/s40623-019-1097-4; https://doi.org/10.1186/s40623-019-1097-4
• オンライン閲覧公開範囲: インターネット公開
• 関連情報（URI）: http://id.ndl.go.jp/digimeta/11467661; https://dl.ndl.go.jp/pid/11467661; http://link.springer.com/content/pdf/10.1186/s40623-019-1097-4.pdf; http://link.springer.com/article/10.1186/s40623-019-1097-4/fulltext.html
• 参照: Thermal Conductivity Profile in the Nankai Accretionary Prism at IODP NanTroSEIZE Site C0002: Estimations From High‐Pressure Experiments Using Input Site Sediments; https://cir.nii.ac.jp/crid/1050004225304853120; Paleo‐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 Project; https://cir.nii.ac.jp/crid/1360021390743190912; Major Mineral Fraction and Physical Properties of Carbonated Peridotite (Listvenite) From ICDP Oman Drilling Project Hole BT1B Inferred From X‐Ray CT Core Images; https://cir.nii.ac.jp/crid/1360294643725324288; Deformation Process and Mechanism of the Frontal Megathrust at the Nankai Subduction Zone; https://cir.nii.ac.jp/crid/1360298757401003648; Multiple Types of Porosity – P‐Wave Velocity Relationships for the Nankai Trough; https://cir.nii.ac.jp/crid/1360298757432546176; A new method for the empirical conversion of logging data to clay mineral fraction in the Nankai accretionary prism; https://cir.nii.ac.jp/crid/2051151842051758976
• 参照: Slab dehydration and earthquake distribution beneath southwestern and central Japan based on three dimensional thermal modeling; https://cir.nii.ac.jp/crid/1050294045370256000; Near-trench slip potential of megaquakes evaluated from fault properties and conditions.; https://cir.nii.ac.jp/crid/1050845760765733504; Frictional properties of JFAST core samples and implications for slow earthquakes at the Tohoku subduction zone; https://cir.nii.ac.jp/crid/1360002214351275136; Development and Performance Tests of a Sensor Suite for a Long-Term Borehole Monitoring System in Seafloor Settings in the Nankai Trough, Japan; https://cir.nii.ac.jp/crid/1360011142933035776; The origin of strata within the inner accretionary prism of Nankai Trough: Evidence from clay mineral assemblages along the NanTroSEIZE transect; https://cir.nii.ac.jp/crid/1360011142941276544; Continuous depth profile of the rock strength in the Nankai accretionary prism based on drilling performance parameters; https://cir.nii.ac.jp/crid/1360283691807326592; Heat flow estimated from BSR and IODP borehole data: Implication of recent uplift and erosion of the imbricate thrust zone in the Nankai Trough off Kumano; https://cir.nii.ac.jp/crid/1360285708264706688; Crustal velocity field of southwest Japan: Subduction and arc‐arc collision; https://cir.nii.ac.jp/crid/1360292617909503360; Source mechanisms and tectonic significance of historical earthquakes along the nankai trough, Japan; https://cir.nii.ac.jp/crid/1360292617916830848; Site C0011; https://cir.nii.ac.jp/crid/1360292618477309440; Expedition 315 Site C0001; https://cir.nii.ac.jp/crid/1360292618549312000; Expedition 316 methods; https://cir.nii.ac.jp/crid/1360292619096624128; Site C0022; https://cir.nii.ac.jp/crid/1360292619447929984; Mineralogy, porosity and fluid control on thermal conductivity of sedimentary rocks; https://cir.nii.ac.jp/crid/1360292620472303232; Fluid transport properties in sediments and their role in large slip near the surface of the plate boundary fault in the Japan Trench; https://cir.nii.ac.jp/crid/1360565165869657984; In situ stress state in the Nankai accretionary wedge estimated from borehole wall failures; https://cir.nii.ac.jp/crid/1360565166661581056; Gas 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 trough; https://cir.nii.ac.jp/crid/1360565168117704448; In Situ Stress and Pore Pressure in the Deep Interior of the Nankai Accretionary Prism, Integrated Ocean Drilling Program Site C0002; https://cir.nii.ac.jp/crid/1360567179761375488; Proceedings of the Ocean Drilling Program, 156 Initial Reports; https://cir.nii.ac.jp/crid/1360574095073855616; Variety and spatial heterogeneity of tectonic tremor worldwide; https://cir.nii.ac.jp/crid/1360846641639199744; Elevated pore pressure and anomalously low stress in regions of low frequency earthquakes along the Nankai Trough subduction megathrust; https://cir.nii.ac.jp/crid/1360846641639742976; Shallow very-low-frequency earthquakes accompany slow slip events in the Nankai subduction zone; https://cir.nii.ac.jp/crid/1360846641753424128; Recurring and triggered slow-slip events near the trench at the Nankai Trough subduction megathrust; https://cir.nii.ac.jp/crid/1360846643379862144; Consolidation state of incoming sediments to the Nankai Trough subduction zone: Implications for sediment deformation and properties; https://cir.nii.ac.jp/crid/1360848654731818624; Runaway 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 Japan; https://cir.nii.ac.jp/crid/1360848657065384320; Present‐day principal horizontal stress orientations in the Kumano forearc basin of the southwest Japan subduction zone determined from IODP NanTroSEIZE drilling Site C0009; https://cir.nii.ac.jp/crid/1360848658216798080; NanTroSEIZE: The IODP Nankai Trough Seismogenic Zone Experiment; https://cir.nii.ac.jp/crid/1360855567869180160; A modified Archie’s law for two conducting phases; https://cir.nii.ac.jp/crid/1360855568447836032; An Empirical Relationship between Velocity and Porosity for Underthrust Sediments in the Nankai Trough Accretionary Prism; https://cir.nii.ac.jp/crid/1360855569884717952; Expedition 315 Site C0002; https://cir.nii.ac.jp/crid/1360855571221245696; Expedition 322 summary; https://cir.nii.ac.jp/crid/1361137044267397632; Interpretation of porosity and LWD resistivity from the Nankai accretionary wedge in light of clay physicochemical properties: Evidence for erosion and local overpressuring; https://cir.nii.ac.jp/crid/1361137044508603776; https://cir.nii.ac.jp/crid/1361137044962032384; Ocean Floor Networks Capture Low-Frequency Earthquake Event; https://cir.nii.ac.jp/crid/1361137046126175232; Expedition 316 Site C0004; https://cir.nii.ac.jp/crid/1361418519979595392; Lithostratigraphy of the Taiwan Chelungpu-Fault Drilling Project-A Borehole and Its Neighboring Region, Central Taiwan; https://cir.nii.ac.jp/crid/1361418520976491776; Expedition 316 summary; https://cir.nii.ac.jp/crid/1361418521095418880; Heat flow along the NanTroSEIZE transect: Results from IODP Expeditions 315 and 316 offshore the Kii Peninsula, Japan; https://cir.nii.ac.jp/crid/1361418521448212480; Site C0012; https://cir.nii.ac.jp/crid/1361699996369497344; Site C0009; https://cir.nii.ac.jp/crid/1361699996418289664; Examination of gas hydrate-bearing deep ocean sediments by X-ray Computed Tomography and verification of physical property measurements of sediments; https://cir.nii.ac.jp/crid/1361975841943867008; Expedition 316 Site C0006; https://cir.nii.ac.jp/crid/1361981468452281344; Exponential approximations to compacted sediment porosity profiles; https://cir.nii.ac.jp/crid/1361981468986749824; Updip limit of the seismogenic zone beneath the accretionary prism of southwest Japan: An effect of diagenetic to low-grade metamorphic processes and increasing effective stress; https://cir.nii.ac.jp/crid/1361981471029956480; Expedition 314 Site C0002; https://cir.nii.ac.jp/crid/1362262944740107136; Distribution of resistive and conductive structures in Nankai accretionary wedge reveals contrasting stress paths; https://cir.nii.ac.jp/crid/1362262945441899008; https://cir.nii.ac.jp/crid/1362262946048841344; Spatiotemporal distribution of very-low frequency earthquakes in Tokachi-oki near the junction of the Kuril and Japan trenches revealed by using array signal processing; https://cir.nii.ac.jp/crid/1362544418722734080; Expedition 316 Site C0008; https://cir.nii.ac.jp/crid/1362544419148929920; Site C0018; https://cir.nii.ac.jp/crid/1362544421247201792; Anelastic strain recovery reveals extension across SW Japan subduction zone; https://cir.nii.ac.jp/crid/1362544421423511808; Subduction factory: 4. Depth-dependent flux of H₂O from subducting slabs worldwide; https://cir.nii.ac.jp/crid/1362825893373320576; Site C0021; https://cir.nii.ac.jp/crid/1362825893585236864; Expedition 315 methods; https://cir.nii.ac.jp/crid/1363107370547250688; Segmentation of X‐ray computed tomography images of porous materials: A crucial step for characterization and quantitative analysis of pore structures; https://cir.nii.ac.jp/crid/1363388845119904768; Expedition 316 Site C0007; https://cir.nii.ac.jp/crid/1363388846049874304; Expedition 314 methods; https://cir.nii.ac.jp/crid/1363670318793842048; Heat flow in South Africa; https://cir.nii.ac.jp/crid/1363951793281794176; Site C0002; https://cir.nii.ac.jp/crid/1364233268691137792; https://cir.nii.ac.jp/crid/1364233268703157504; Fault stability inferred from granite sliding experiments at hydrothermal conditions; https://cir.nii.ac.jp/crid/1364233268924600832; Site C0010; https://cir.nii.ac.jp/crid/1364233271127801984; Origin and evolution of a splay fault in the Nankai accretionary wedge; https://cir.nii.ac.jp/crid/1571417126454293760; Re-evaluation of temperature at the updip limit of locked portion of Nankai megasplay inferred from IODP Site C0002 temperature observatory; https://cir.nii.ac.jp/crid/2051433317070227328; Distribution and depth of bottom-simulating reflectors in the Nankai subduction margin; https://cir.nii.ac.jp/crid/2051996266966349952
• 参照（URI）: https://cir.nii.ac.jp/crid/1371975846746366848
• 連携機関・データベース: 国立情報学研究所 : CiNii Research; https://cir.nii.ac.jp/
• 提供元機関・データベース: 雑誌記事索引データベース; https://ndlsearch.ndl.go.jp; Crossref; https://www.crossref.org; 科学研究費助成事業データベース; https://kaken.nii.ac.jp/ja
• 書誌ID（NDLBibID）: 11467661; http://id.ndl.go.jp/bib/11467661