Dominant role of temperature on deep earthquake mechanics for the Tonga slab near the bottom of the upper mantle

• 資料種別: 記事
• タイトル: Dominant role of temperature on deep earthquake mechanics for the Tonga slab near the bottom of the upper mantle
• 著者・編者: Satoshi Kaneshima; Shoichi Yoshioka
• 出版事項: 日本 : Springer science+business media
• 出版年月日等: 2014-10-15
• 出版年（W3CDTF）: 2014-10-15
• タイトル（掲載誌）: EPS : Earth, Planets and Space
• 巻号年月日等（掲載誌）: 66(138)
• 掲載巻: 66(138)
• 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/s40623-014-0138-2; https://doi.org/10.1186/s40623-014-0138-2
• 国立国会図書館永続的識別子: info:ndljp/pid/9227893; https://dl.ndl.go.jp/pid/9227893
• 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）: 2015-04-17T10:30:12+09:00
• 保存日（W3CDTF）: 2014-10-20
• 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://www.earth-planets-space.com/content/66/October/2014
• 掲載誌（国立国会図書館永続的識別子）: info:ndljp/pid/9227755; https://dl.ndl.go.jp/pid/9227755
• 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

• 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 > デジタル化資料 > 雑誌; https://dl.ndl.go.jp/collections/A00002
• 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
• 所蔵機関: 国立国会図書館
• 請求記号: Z19-292
• 掲載誌（国立国会図書館永続的識別子）: info:ndljp/pid/3427605; https://dl.ndl.go.jp/pid/3427605
• 連携機関・データベース: 国立国会図書館 : 国立国会図書館雑誌記事索引; https://ndlsearch.ndl.go.jp
• 書誌ID（NDLBibID）: 9227893; http://id.ndl.go.jp/bib/9227893
• 整理区分コード: 632

• 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/s40623-014-0138-2; https://doi.org/10.1186/s40623-014-0138-2
• 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/9227893; https://dl.ndl.go.jp/pid/9227893; http://link.springer.com/article/10.1186/s40623-014-0138-2/fulltext.html; http://link.springer.com/content/pdf/10.1186/s40623-014-0138-2.pdf; http://link.springer.com/content/pdf/10.1186/s40623-014-0138-2
• 参照: Seismic scatterers in the mid-lower mantle; https://cir.nii.ac.jp/crid/1360002216113790208; Temperature Dependence of H₂O Solubility in Al‐Free Stishovite; https://cir.nii.ac.jp/crid/1360584341823550336; Seismic scatterers in the lower mantle near subduction zones; https://cir.nii.ac.jp/crid/1361131419431101952
• 参照: Geophysical and mineralogical constraints on the post-spinel transformation for the Tonga slab; https://cir.nii.ac.jp/crid/1360002216113765632; Deep-Focus Earthquakes and Recycling of Water into the Earth's Mantle; https://cir.nii.ac.jp/crid/1360011145934916352; New, improved version of generic mapping tools released; https://cir.nii.ac.jp/crid/1360292617909532032; Precursors to ScS Phases and dipping interface in the upper mantle beneath southwestern Japan; https://cir.nii.ac.jp/crid/1360292618620733824; Complex morphology of subducted lithosphere in the mantle beneath the Tonga trench; https://cir.nii.ac.jp/crid/1360292619038877312; High temperature anomalies oceanward of subducting slabs at the 410-km discontinuity; https://cir.nii.ac.jp/crid/1360855567871048832; Subduction zone thermal structure and mineralogy and their relationship to seismic wave reflections and conversions at the slab/mantle interface; https://cir.nii.ac.jp/crid/1360855569614057600; Noise reduction and detection of weak, coherent signals through phase-weighted stacks; https://cir.nii.ac.jp/crid/1361137043909510016; Metastable mantle phase transformations and deep earthquakes in subducting oceanic lithosphere; https://cir.nii.ac.jp/crid/1361137044282190208; Petrogenetic grid in the system MgO‐SiO₂‐H₂O up to 30 GPa, 1600°C: Applications to hydrous peridotite subducting into the Earth’s deep interior; https://cir.nii.ac.jp/crid/1361137044450773632; Ringwoodite growth rates from olivine with ∼75ppmw H2O: Metastable olivine must be nearly anhydrous to exist in the mantle transition zone; https://cir.nii.ac.jp/crid/1361137046439113088; Evidence for a metastable olivine wedge inside the subducted Mariana slab; https://cir.nii.ac.jp/crid/1361418520814017664; Constraints on seismic velocities in the Earth from traveltimes; https://cir.nii.ac.jp/crid/1361699994760834048; Plate motions, slab dynamics and back-arc deformation; https://cir.nii.ac.jp/crid/1361699996033209088; The influence of trench migration on slab penetration into the lower mantle; https://cir.nii.ac.jp/crid/1362544420171474432; Thermal structure and seismicity of subducting lithosphere; https://cir.nii.ac.jp/crid/1362825893553109632; Seismic evidence of negligible water carried below 400-km depth in subducting lithosphere; https://cir.nii.ac.jp/crid/1362825894498661888; Slab temperature and thickness from seismic tomography: 1. Method and application to Tonga; https://cir.nii.ac.jp/crid/1362825894529257344; Numerical simulations of deformation and dynamics of horizontally lying slabs; https://cir.nii.ac.jp/crid/1362825895959051392; Rheological structure and deformation of subducted slabs in the mantle transition zone: implications for mantle circulation and deep earthquakes; https://cir.nii.ac.jp/crid/1362825896037663872; Stress fields associated with metastable phase transitions in descending slabs and deep-focus earthquakes; https://cir.nii.ac.jp/crid/1362825896251183488; Plastic instabilities: Implications for the origin of intermediate and deep focus earthquakes; https://cir.nii.ac.jp/crid/1363107370363088768; Small scale heterogeneity in the mid-lower mantle beneath the circum-Pacific area; https://cir.nii.ac.jp/crid/1363107370828510976; Maximum depth of seismicity and thermal parameter of the subducting slab: general empirical relation and its application; https://cir.nii.ac.jp/crid/1363107370861527168; Effects of variable thermal conductivity on the mineralogy of subducting slabs and implications for mechanisms of deep earthquakes; https://cir.nii.ac.jp/crid/1363388845569368960; Physical conditions producing slab stagnation: Constraints of the Clapeyron slope, mantle viscosity, trench retreat, and dip angles; https://cir.nii.ac.jp/crid/1363670321241208448; Dipping Low-Velocity Layer in the Mid-Lower Mantle: Evidence for Geochemical Heterogeneity; https://cir.nii.ac.jp/crid/1363951793754080896; Mechanism and kinetics of the α–β transition in San Carlos olivine Mg_1.8Fe_0.2SiO₄; https://cir.nii.ac.jp/crid/1363951794483469824; Buoyancy, bending, and seismic visibility in deep slab stagnation; https://cir.nii.ac.jp/crid/1363951794685667200; Recent progress in experimental mineral physics: Phase relations of hydrous systems and the role of water in slab dynamics; https://cir.nii.ac.jp/crid/1363951794916241792; Seismological constraints on the mechanism of deep earthquakes: temperature dependence of deep earthquake source properties; https://cir.nii.ac.jp/crid/1363951794967154688; On the separation of crustal component from subducted oceanic lithosphere near the 660 km discontinuity; https://cir.nii.ac.jp/crid/1364233269628570368; Seismological and experimental constraints on metastable phase transformations and rheology of the Mariana slab; https://cir.nii.ac.jp/crid/1364233270871378816
• 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）: 9227893; http://id.ndl.go.jp/bib/9227893