Can quasicrystals survive in planetary collisions?

• 資料種別: 記事
• タイトル: Can quasicrystals survive in planetary collisions?
• 著者・編者: Vincenzo Stagno; Luca Bindi; Sota Takagi
• 出版事項: 日本 : Springer Nature
• 出版年月日等: 2021-04-20
• 出版年（W3CDTF）: 2021-04-20
• タイトル（掲載誌）: Progress in earth and planetary science
• 巻号年月日等（掲載誌）: 8(27)
• 掲載巻: 8(27)
• 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/s40645-021-00421-y; https://doi.org/10.1186/s40645-021-00421-y
• 国立国会図書館永続的識別子: info:ndljp/pid/11886982; https://dl.ndl.go.jp/pid/11886982
• 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）: 2021-11-19T10:01:09+09:00
• 保存日（W3CDTF）: 2021-11-19
• 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/11667979; https://dl.ndl.go.jp/pid/11667979
• 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/s40645-021-00421-y; https://doi.org/10.1186/s40645-021-00421-y
• 関連情報（URI）: http://id.ndl.go.jp/digimeta/11886982; https://dl.ndl.go.jp/pid/11886982; https://link.springer.com/content/pdf/10.1186/s40645-021-00421-y.pdf; https://link.springer.com/article/10.1186/s40645-021-00421-y/fulltext.html; http://hdl.handle.net/11573/1681835; http://hdl.handle.net/2158/1235373
• 参照: Preface for article collection “Thermal, dynamical, and chemical processes in our early Solar System”; https://cir.nii.ac.jp/crid/2050588892112943360
• 参照: Poirierite, a dense metastable polymorph of magnesium iron silicate in shocked meteorites; https://cir.nii.ac.jp/crid/1050005508516260736; Icosahedral AlCuFe quasicrystal at high pressure and temperature and its implications for the stability of icosahedrite; https://cir.nii.ac.jp/crid/1360002216855632512; Cosmic history and a candidate parent asteroid for the quasicrystal-bearing meteorite Khatyrka; https://cir.nii.ac.jp/crid/1360011145839873280; Shock synthesis of quasicrystals with implications for their origin in asteroid collisions; https://cir.nii.ac.jp/crid/1360013170275813632; A unique CO-like micrometeorite hosting an exotic Al-Cu-Fe-bearing assemblage – close affinities with the Khatyrka meteorite; https://cir.nii.ac.jp/crid/1360013172305044992; The chemical composition of metallic spheroids and metallic particles within impactite from Barringer Meteorite Crater, Arizona; https://cir.nii.ac.jp/crid/1360013172800515072; A metal particle from a Ca,Al-rich inclusion from the meteorite Allende, and the condensation of refractory siderophile elements; https://cir.nii.ac.jp/crid/1360013172920634368; Quasicrystals at extreme conditions: The role of pressure in stabilizing icosahedral Al₆₃Cu₂₄Fe₁₃at high temperature; https://cir.nii.ac.jp/crid/1360013173144345600; Evidence for the charge disproportionation of iron in extraterrestrial bridgmanite; https://cir.nii.ac.jp/crid/1360292618639441152; Natural quasicrystal with decagonal symmetry; https://cir.nii.ac.jp/crid/1360292619156803712; Khatyrka, a new <scp>CV</scp>3 find from the Koryak Mountains, Eastern Russia; https://cir.nii.ac.jp/crid/1360292619582760064; Equations of state of six metals above<mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" display="inline"><mml:mrow><mml:mn>94</mml:mn><mml:mspace width="0.3em"/><mml:mi mathvariant="normal">GPa</mml:mi></mml:mrow></mml:math>; https://cir.nii.ac.jp/crid/1360292620405288320; Decagonite, Al₇₁Ni₂₄Fe₅, a quasicrystal with decagonal symmetry from the Khatyrka CV3 carbonaceous chondrite; https://cir.nii.ac.jp/crid/1360294647286674816; Shock Synthesis of Decagonal Quasicrystals; https://cir.nii.ac.jp/crid/1360294647799291392; Shock Synthesis of Five-component Icosahedral Quasicrystals; https://cir.nii.ac.jp/crid/1360294647992834176; Stability and strain of decagonal Al-Ni-Co quasicrystal under high pressure up to 70GPa; https://cir.nii.ac.jp/crid/1360294648181244928; Experimental evidence for the existence of iron-rich metal in the Earth's lower mantle; https://cir.nii.ac.jp/crid/1360574094015588480; Shock metamorphism of planetary silicate rocks and sediments: Proposal for an updated classification system; https://cir.nii.ac.jp/crid/1360574094155674240; Phase equilibria in the nominally Al 65 Cu 23 Fe 12 system at 3, 5 and 21 GPa: Implications for the quasicrystal-bearing Khatyrka meteorite; https://cir.nii.ac.jp/crid/1360576121767953408; First synthesis of a unique icosahedral phase from the Khatyrka meteorite by shock-recovery experiment; https://cir.nii.ac.jp/crid/1360576122173391744; Trace Element Conundrum of Natural Quasicrystals; https://cir.nii.ac.jp/crid/1360576122971741568; High‐pressure minerals in shocked meteorites; https://cir.nii.ac.jp/crid/1360846643276521472; X-ray diffraction study of the icosahedral AlCuFe quasicrystal at megabar pressures; https://cir.nii.ac.jp/crid/1360848657289190144; Accretion and differentiation of the terrestrial planets with implications for the compositions of early-formed Solar System bodies and accretion of water; https://cir.nii.ac.jp/crid/1360855568631201664; A new natural high-pressure (Na,Ca)-hexaluminosilicate [(CaxNa1−x)Al3+xSi3−xO11] in shocked Martian meteorites; https://cir.nii.ac.jp/crid/1360855568720824832; 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; Stability of icosahedral Al-Cu-Fe and two approximant phases under high pressure up to 35 GPa; https://cir.nii.ac.jp/crid/1360855569320101248; Quasicrystals; https://cir.nii.ac.jp/crid/1360855570803885440; X-ray absorption and diffraction spectroscopy of icosahedral Al-Cu-Fe quasicrystals under high pressure; https://cir.nii.ac.jp/crid/1360855571185854208; EosFit7c and a Fortran module (library) for equation of state calculations; https://cir.nii.ac.jp/crid/1360855571280085888; Composition of the Metallic Phases in some Stone and Stony-Iron Meteorites; https://cir.nii.ac.jp/crid/1360857596719312896; Evidence of the impacting body of the Ries crater — the discovery of Fe-Cr-Ni veinlets below the crater bottom; https://cir.nii.ac.jp/crid/1360857597444344704; Evidence of cross-cutting and redox reaction in Khatyrka meteorite reveals metallic-Al minerals formed in outer space; https://cir.nii.ac.jp/crid/1360857598145561856; Static compression of iron to 300 GPa and Fe_0.8Ni_0.2 alloy to 260 GPa: Implications for composition of the core; https://cir.nii.ac.jp/crid/1361137044032055424; The composition of the Earth; https://cir.nii.ac.jp/crid/1361137045118512256; 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; Quasicrystals: A New Class of Ordered Structures; https://cir.nii.ac.jp/crid/1361418518594381184; Discovery of the Fe-analogue of akimotoite in the shocked Suizhou L6 chondrite; https://cir.nii.ac.jp/crid/1361418521004069376; Icosahedrite, Al63Cu24Fe13, the first natural quasicrystal; https://cir.nii.ac.jp/crid/1361699994346636672; Akaogiite: An ultra-dense polymorph of TiO2 with the baddeleyite-type structure, in shocked garnet gneiss from the Ries Crater, Germany; https://cir.nii.ac.jp/crid/1361699995525817856; The Majorite-Pyrope + Magnesiowüstite Assemblage: Constraints on the History of Shock Veins in Chondrites; https://cir.nii.ac.jp/crid/1361699995738062336; X-ray diffraction and equation of state of solid neon to 110 GPa; https://cir.nii.ac.jp/crid/1361981469682281472; Evidence for the extraterrestrial origin of a natural quasicrystal; https://cir.nii.ac.jp/crid/1361981470361137664; A Monoclinic Post-Stishovite Polymorph of Silica in the Shergotty Meteorite; https://cir.nii.ac.jp/crid/1362262944761269376; Timescales of shock processes in chondritic and martian meteorites; https://cir.nii.ac.jp/crid/1362825893335412096; An Ultradense Polymorph of Rutile with Seven-Coordinated Titanium from the Ries Crater; https://cir.nii.ac.jp/crid/1362825895181949568; Natural NaAlSi ₃ O ₈ -Hollandite in the Shocked Sixiangkou Meteorite; https://cir.nii.ac.jp/crid/1362825896286756992; Impact-induced shock and the formation of natural quasicrystals in the early solar system; https://cir.nii.ac.jp/crid/1363107370123261696; A natural shock-induced dense polymorph of rutile with α-PbO2 structure in the suevite from the Ries crater in Germany; https://cir.nii.ac.jp/crid/1363388845158882048; Host rock solid-state transformation in a shock-induced melt vein of Tenham L6 chondrite; https://cir.nii.ac.jp/crid/1363388845179373440; Natural Quasicrystals; https://cir.nii.ac.jp/crid/1363388846101888000; Fractional crystallization of olivine melt inclusion in shock-induced chondritic melt vein; https://cir.nii.ac.jp/crid/1363670318265145984; Metallic Phase with Long-Range Orientational Order and No Translational Symmetry; https://cir.nii.ac.jp/crid/1363670319925427328; Previously unknown quasicrystal periodic approximant found in space; https://cir.nii.ac.jp/crid/1364233269520570112; Seifertite, a dense orthorhombic polymorph of silica from the Martian meteorites Shergotty and Zagami; https://cir.nii.ac.jp/crid/1364233270773365888
• 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）: 11886982; http://id.ndl.go.jp/bib/11886982