Back-transformation processes in high-pressure minerals : implications for planetary collisions and diamond transportation from the deep Earth

• 資料種別: 記事
• タイトル: Back-transformation processes in high-pressure minerals : implications for planetary collisions and diamond transportation from the deep Earth
• 著者・編者: Tomoaki Kubo; Ko Kamura; Masahiro Imamura
• 出版事項: 日本 : Springer Nature
• 出版年月日等: 2022-04-21
• 出版年（W3CDTF）: 2022-04-21
• タイトル（掲載誌）: Progress in earth and planetary science
• 巻号年月日等（掲載誌）: 9(21)
• 掲載巻: 9(21)
• 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/s40645-022-00480-9; https://doi.org/10.1186/s40645-022-00480-9
• 国立国会図書館永続的識別子: info:ndljp/pid/12307832; https://dl.ndl.go.jp/pid/12307832
• 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）: 2022-07-11T20:40:38+09:00
• 保存日（W3CDTF）: 2022-07-11
• 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://progearthplanetsci.springeropen.com/articles
• 掲載誌（国立国会図書館永続的識別子）: info:ndljp/pid/12307811; https://dl.ndl.go.jp/pid/12307811
• 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/s40645-022-00480-9; https://doi.org/10.1186/s40645-022-00480-9
• 関連情報（URI）: http://id.ndl.go.jp/digimeta/12307832; https://dl.ndl.go.jp/pid/12307832; https://link.springer.com/content/pdf/10.1186/s40645-022-00480-9.pdf; https://link.springer.com/article/10.1186/s40645-022-00480-9/fulltext.html
• 参照: Vesicular Olivines and Pyroxenes in Shocked Kamargaon L6 Chondrite: Implications for Primary Volatiles and Its Multiple Impacts History; https://cir.nii.ac.jp/crid/1360017282426659200; Effect of grain size on amorphization mechanism and kinetics of bridgmanite in shocked meteorites; https://cir.nii.ac.jp/crid/1360021389806446848; Bridgmanite Freezing in Shocked Meteorites Due To Amorphization‐Induced Stress; https://cir.nii.ac.jp/crid/1360298757432488704; 高温下時分割放射光回折測定によるブリッジマナイトのアモルファス化反応の研究; https://cir.nii.ac.jp/crid/1390013010127892096; Preface for article collection “Thermal, dynamical, and chemical processes in our early Solar System”; https://cir.nii.ac.jp/crid/2050588892112943360
• 参照: Creep strength of ringwoodite measured at pressure–temperature conditions of the lower part of the mantle transition zone using a deformation–DIA apparatus; https://cir.nii.ac.jp/crid/1360004232135485824; Olivine melting at high pressure condition in the chassignite Northwest Africa 2737; https://cir.nii.ac.jp/crid/1360004232425675392; Curious kinetic behavior in silica polymorphs solves seifertite puzzle in shocked meteorite; https://cir.nii.ac.jp/crid/1360004235936359296; Experimental and thermodynamic investigations on the stability of Mg₁₄Si₅O₂₄anhydrous phase B with relevance to Mg₂SiO₄forsterite, wadsleyite, and ringwoodite; https://cir.nii.ac.jp/crid/1360004238404766592; Back‐transformation mechanisms of ringwoodite and majorite in an ordinary chondrite; https://cir.nii.ac.jp/crid/1360009142504201856; Development of the Multi-anvil Assembly 6-6 for DIA and D-DIA type high-pressure apparatuses; https://cir.nii.ac.jp/crid/1360011146346397312; Back-transformation of high-pressure phases in a shock melt vein of an H-chondrite during atmospheric passage: Implications for the survival of high-pressure phases after decompression; https://cir.nii.ac.jp/crid/1360011146530120320; Survival of majoritic garnet in diamond by direct kimberlite ascent from deep mantle; https://cir.nii.ac.jp/crid/1360285708263354752; Thermal equation of state of (Mg0.91Fe0.09)2SiO4 ringwoodite; https://cir.nii.ac.jp/crid/1360292619984851712; Discovery of bridgmanite, the most abundant mineral in Earth, in a shocked meteorite; https://cir.nii.ac.jp/crid/1360292621166579840; Stability of high-density clinoenstatite at upper-mantle pressures; https://cir.nii.ac.jp/crid/1360292621176032384; Lower mantle diamonds from Rio Soriso (Juina area, Mato Grosso, Brazil); https://cir.nii.ac.jp/crid/1360292621188099200; Calorimetric study of olivine solid solutions in the system Mg2SiO4-Fe2SiO4; https://cir.nii.ac.jp/crid/1360292621247935104; Discovery of davemaoite, CaSiO ₃ -perovskite, as a mineral from the lower mantle; https://cir.nii.ac.jp/crid/1360298345428156544; Coherent and subsequent incoherent ringwoodite growth in olivine of shocked L6 chondrites; https://cir.nii.ac.jp/crid/1360567182088591360; Formation of a metastable hollandite phase from amorphous plagioclase: A possible origin of lingunite in shocked chondritic meteorites; https://cir.nii.ac.jp/crid/1360567182379079552; Hydrous mantle transition zone indicated by ringwoodite included within diamond; https://cir.nii.ac.jp/crid/1360574093795642880; Back-transformation of high-pressure minerals in shocked chondrites: Low-pressure mineral evidence for strong shock; https://cir.nii.ac.jp/crid/1360574094114535168; Shock metamorphism of Elephant Moraine A79001: Implications for olivine–ringwoodite transformation and the complex thermal history of heavily shocked Martian meteorites; https://cir.nii.ac.jp/crid/1360574094962637184; An in situ X ray diffraction study of the kinetics of the Ni₂SiO₄ olivine‐spinel transformation; https://cir.nii.ac.jp/crid/1360574095311213184; High‐pressure minerals in shocked meteorites; https://cir.nii.ac.jp/crid/1360846643276521472; Natural dissociation of olivine to (Mg,Fe)SiO ₃ perovskite and magnesiowüstite in a shocked Martian meteorite; https://cir.nii.ac.jp/crid/1360848658887233408; Evidence for fractional crystallization of wadsleyite and ringwoodite from olivine melts in chondrules entrained in shock-melt veins; https://cir.nii.ac.jp/crid/1360855568890573440; Pyroxene solid solution in garnets included in diamond; https://cir.nii.ac.jp/crid/1360855569784792832; Olivine‐modified spinel‐spinel transitions in the system Mg₂SiO₄‐Fe₂SiO₄: Calorimetric measurements, thermochemical calculation, and geophysical application; https://cir.nii.ac.jp/crid/1360855570715602176; Natural (Mg,Fe)SiO ₃ -Ilmenite and -Perovskite in the Tenham Meteorite; https://cir.nii.ac.jp/crid/1361137043957067008; Water controls the fields of metastable olivine in cold subducting slabs; https://cir.nii.ac.jp/crid/1361137045331183488; Formation of high-pressure minerals in shocked L6 chondrite Yamato 791384: constraints on shock conditions and parent body size; https://cir.nii.ac.jp/crid/1361137046101839232; Orthoenstatite/clinoenstatite phase transformation in MgSiO₃ at high‐pressure and high‐temperature determined by in situ X‐ray diffraction: Implications for nature of the X discontinuity; https://cir.nii.ac.jp/crid/1361418520422618752; Decompression and unmixing of crystals included in diamonds from the mantle transition zone; https://cir.nii.ac.jp/crid/1361699994050966272; Origin of kimberlites and related magmas; https://cir.nii.ac.jp/crid/1361699994955457024; The kinetics of grain boundary nucleated reactions; https://cir.nii.ac.jp/crid/1362262944382890752; Electron microscopy of (Mg, Fe)SiO₃ Perovskite: Evidence for structural phase transitions and implications for the lower mantle; https://cir.nii.ac.jp/crid/1362262944766077056; Shock‐induced transition of NaAlSi₃O₈ feldspar into a hollandite structure in a L6 chondrite; https://cir.nii.ac.jp/crid/1362544418564579968; Grain-growth kinetics in wadsleyite: Effects of chemical environment; https://cir.nii.ac.jp/crid/1362544418748304896; Timescales of shock processes in chondritic and martian meteorites; https://cir.nii.ac.jp/crid/1362825893335412096; Kinetics of the olivine-spinel transformation in subducting lithosphere: experimental constraints and implications for deep slab processes; https://cir.nii.ac.jp/crid/1362825895573835264; Natural NaAlSi ₃ O ₈ -Hollandite in the Shocked Sixiangkou Meteorite; https://cir.nii.ac.jp/crid/1362825896286756992; The NaCl pressure standard; https://cir.nii.ac.jp/crid/1363107369004675584; High-temperature Raman spectroscopic and X-ray diffraction study of beta -Mg₂SiO₄; insights into its high-temperature thermodynamic properties and the beta - to alpha -phase-transition mechanism and kinetics; https://cir.nii.ac.jp/crid/1363107369510994176; Natural Occurrence of MgSiO ₃ -Ilmenite and Evidence for MgSiO ₃ -Perovskite in a Shocked L Chondrite; https://cir.nii.ac.jp/crid/1363107370328724864; Subducting oceanic crust: The source of deep diamonds; https://cir.nii.ac.jp/crid/1363388843720644096; Thermodynamic Data, Models, and Phase Diagrams in Multicomponent Oxide Systems; https://cir.nii.ac.jp/crid/1363388844185684352; Host rock solid-state transformation in a shock-induced melt vein of Tenham L6 chondrite; https://cir.nii.ac.jp/crid/1363388845179373440; Plagioclase breakdown as an indicator for shock conditions of meteorites; https://cir.nii.ac.jp/crid/1363670321239097728; The Phase Boundary Between α- and β-Mg ₂ SiO ₄ Determined by in Situ X-ray Observation; https://cir.nii.ac.jp/crid/1363951793892275840; Effects of shock and Martian alteration on Tissint hydrogen isotope ratios and water content; https://cir.nii.ac.jp/crid/1364233270804479104; 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）: 12307832; http://id.ndl.go.jp/bib/12307832