Natural and experimental high-pressure, shock-produced terrestrial and extraterrestrial materials
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- Material Type
- 記事
- Title
- Author/Editor
- Masaaki MiyaharaNaotaka TomiokaLuca Bindi
- Publication, Distribution, etc.
- Publication Date
- 2021-10-18
- Publication Date (W3CDTF)
- 2021-10-18
- Periodical title
- Progress in earth and planetary science
- No. or year of volume/issue
- 8(58)
- Volume
- 8(58)
- ISSN (Periodical Title)
- 2197-4284
- ISSN-L (Periodical Title)
- 2197-4284
- Text Language Code
- eng
- DOI
- 10.1186/s40645-021-00451-6
- Persistent ID (NDL)
- info:ndljp/pid/12307800
- 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)
- 2022-07-11T20:40:38+09:00
- Date Captured (W3CDTF)
- 2022-07-11
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- application/pdf
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- 国立国会図書館内限定公開
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- 可
- Periodical Title (URI)
- Periodical Title (Persistent ID (NDL))
- info:ndljp/pid/11667979
- 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/s40645-021-00451-6
- Access Restrictions
- インターネット公開
- Related Material (URI)
- Is Referenced By
- Vesicular Olivines and Pyroxenes in Shocked Kamargaon L6 Chondrite: Implications for Primary Volatiles and Its Multiple Impacts HistoryExperimental Evidence for Shear‐Induced Melting and Generation of Stishovite in Granite at Low (<18 GPa) Shock Pressure衝撃変成を受けた隕石中に発見された新鉱物：秋本石Preface for article collection “Thermal, dynamical, and chemical processes in our early Solar System”
- References
- Poirierite, a dense metastable polymorph of magnesium iron silicate in shocked meteoritesDiscovery of moganite in a lunar meteorite as a trace of H <sub>2</sub> O ice in the Moon’s regolithUltrafast olivine-ringwoodite transformation during shock compressionDiscovery of natural MgSiO <sub>3</sub> tetragonal garnet in a shocked chondritic meteoriteQuantifying the Release of Climate‐Active Gases by Large Meteorite Impacts With a Case Study of ChicxulubStability of a hydrous δ-phase, AlOOH–MgSiO2(OH)2, and a mechanism for water transport into the base of lower mantleJadeite in Chelyabinsk meteorite and the nature of an impact event on its parent bodyNatural occurrence of pure nano-polycrystalline diamond from impact craterCoesite and stishovite in a shocked lunar meteorite, Asuka-881757, and impact events in lunar surfaceEvidence for multiple dynamic events and subsequent decompression stage recorded in a shock veinOlivine melting at high pressure condition in the chassignite Northwest Africa 2737A new high-pressure form of Mg2SiO4 highlighting diffusionless phase transitions of olivineCurious kinetic behavior in silica polymorphs solves seifertite puzzle in shocked meteoriteBack‐transformation mechanisms of ringwoodite and majorite in an ordinary chondriteHigh‐pressure phases in shock‐induced melt of the unique highly shocked <scp>LL</scp>6 chondrite Northwest Africa 757Ahrensite, γ-Fe2SiO4, a new shock-metamorphic mineral from the Tissint meteorite: Implications for the Tissint shock event on MarsHexagonal Diamond—A New Form of CarbonShock behavior of zircon: phase transition to scheelite structure and decompositionDiscovery of high-pressure ZrSiO4 polymorph in naturally occurring shock-metamorphosed zirconsHigh-pressure phases in an ultramafic rock from MarsA vacancy‐rich, partially inverted spinelloid silicate, (Mg,Fe,Si)<sub>2</sub>(Si,□)O<sub>4</sub>, as a major matrix phase in shock melt veins of the Tenham and Suizhou L6 chondritesSynthesis of a perovskite-type polymorph of CaSiO3Cosmic history and a candidate parent asteroid for the quasicrystal-bearing meteorite KhatyrkaBack-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 decompressionDiscovery of Elgoresyite, (Mg,Fe)<sub>5</sub>Si<sub>2</sub>O<sub>9</sub>: Implications for Novel Iron-Magnesium Silicates in Rocky Planetary InteriorsShock synthesis of quasicrystals with implications for their origin in asteroid collisionsMaskelynite formation via solid‐state transformation: Evidence of infrared and X‐ray anisotropyA unique CO-like micrometeorite hosting an exotic Al-Cu-Fe-bearing assemblage – close affinities with the Khatyrka meteoriteRiesite, a New High Pressure Polymorph of TiO2 from the Ries Impact StructureOrigin, properties, and structure of breyite: The second most abundant mineral inclusion in super-deep diamondsDiscovery of nanophase iron particles and high pressure clinoenstatite in a heavily shocked ordinary chondrite: Implications for the decomposition of pyroxeneMajoritic garnet grains within shock-induced melt veins in amphibolites from the Ries impact crater suggest ultrahigh crystallization pressures between 18 and 9 GPaJadeite formation in shocked ordinary chondritesRapid recovery of life at ground zero of the end-Cretaceous mass extinctionEvidence for the charge disproportionation of iron in extraterrestrial bridgmaniteNatural quasicrystal with decagonal symmetryThe stability and equation of state for the cotunnite phase of TiO2 up to 70 GPaKhatyrka, a new <scp>CV</scp>3 find from the Koryak Mountains, Eastern RussiaCharacterization of a high-pressure phase of silica from the Martian meteorite ShergottyA dense polymorph of Ca3(PO4)2: a high pressure phase of apatite decomposition and its geochemical significanceShock metamorphism of quartz in nature and experiment: II. Significance in geoscience*Synthesis and crystal-chemical characterization of MgSiO3 perovskiteThe Pyrite-Type High-Pressure Form of SilicaDiscovery of bridgmanite, the most abundant mineral in Earth, in a shocked meteoriteStability of high-density clinoenstatite at upper-mantle pressuresCoesite and stishovite in the Vredefort Dome, South AfricaExtraterrestrial, shock-formed, cage-like nanostructured carbonaceous materialsMelting experiments on the forsterite–pyrope system at 8 and 13.5 GPaAn evolutionary system of mineralogy, Part IV: Planetesimal differentiation and impact mineralization (4566 to 4560 Ma)The nature, distribution and genesis of the coesite and stishovite associated with the pseudotachylite of the Vredefort Dome, South AfricaDecagonite, Al<sub>71</sub>Ni<sub>24</sub>Fe<sub>5</sub>, a quasicrystal with decagonal symmetry from the Khatyrka CV3 carbonaceous chondriteLingunite-a high-pressure plagioclase polymorph at mineral interfaces in doleritic rock of the Lockne impact structure (Sweden)Si-rich Mg-sursassite Mg4Al5Si7O23(OH)5 with octahedrally coordinated Si: A new ultrahigh-pressure hydrous phaseStöfflerite, (Ca,Na)(Si,Al)4O8 in the hollandite structure: A new high-pressure polymorph of anorthite from martian meteorite NWA 856New minerals and nomenclature modifications approved in 2017Origin of micrometer-sized impact diamonds in ureilites by catalytic growth involving Fe-Ni-silicide: The example of Kenna meteoritePreparation of a new Al-Cu-Fe quasicrystal with large grain sizes by rapid solidificationThe formation of peak rings in large impact cratersTransformation of graphite to lonsdaleite and diamond in the Goalpara ureilite directly observed by TEMCoherent and subsequent incoherent ringwoodite growth in olivine of shocked L6 chondritesShock-induced deformation of Shergottites: Shock-pressures and perturbations of magmatic ages on MarsFormation of a metastable hollandite phase from amorphous plagioclase: A possible origin of lingunite in shocked chondritic meteoritesDiscovery of seifertite in a shocked lunar meteoriteHigh-pressure minerals in eucrite suggest a small source crater on VestaCa‐Al‐Fe‐rich inclusion in the Vigarano CV3 chondriteSystematic investigations of high‐pressure polymorphs in shocked ordinary chondritesNew shock microstructures in titanite (CaTiSiO5) from the peak ring of the Chicxulub impact structure, MexicoMaking tissintite: Mimicking meteorites in the multi-anvilHydrous mantle transition zone indicated by ringwoodite included within diamondBack-transformation of high-pressure minerals in shocked chondrites: Low-pressure mineral evidence for strong shockShock metamorphism of planetary silicate rocks and sediments: Proposal for an updated classification systemFocused Ion Beam (FIB) combined with SEM and TEM: Advanced analytical tools for studies of chemical composition, microstructure and crystal structure in geomaterials on a nanometre scaleA new mineral with an olivine structure and pyroxene composition in the shock-induced melt veins of Tenham L6 chondriteThe Kenna ureilite: an ultramafic rock with evidence for igneous, metamorphic, and shock originStishovite: Synthesis by Shock WaveNoble-gas enrichment in vapour-growth diamonds and the origin of diamonds in ureilitesComplicated pressure–temperature path recorded in the eucrite PadvarninkaiShock‐Induced Incongruent Melting of Olivine in Kamargaon L6 ChondriteGlasses formed by hypervelocity impactCarbyne with finite length: The one-dimensional <i>sp</i> carbonProducing highly complicated materials. Nature does it betterWangdaodeite, the LiNbO<sub>3</sub>‐structured high‐pressure polymorph of ilmenite, a new mineral from the Suizhou L6 chondrite(Fe,Ni)2P allabogdanite can be an ambient pressure phase in iron meteoritesChenmingite, FeCr2O4 in the CaFe2O4-type structure, a shock-induced, high-pressure mineral in the Tissint martian meteoriteTrace Element Conundrum of Natural QuasicrystalsImpact shock origin of diamonds in ureilite meteoritesErratum: Formation of Diamond by Explosive ShockSynthesis of inverse ringwoodite sheds light on the subduction history of Tibetan ophiolitesHigh‐pressure minerals in shocked meteoritesUnique large diamonds in a ureilite from Almahata Sitta 2008 TC3 asteroidAlbite dissociation reaction in the Northwest Africa 8275 shocked LL chondrite and implications for its impact historyPhase transition processes of olivine in the shocked Martian meteorite Tissint: Clues to origin of ringwoodite-, bridgmanite- and magnesiowüstite-bearing assemblagesNatural dissociation of olivine to (Mg,Fe)SiO <sub>3</sub> perovskite and magnesiowüstite in a shocked Martian meteoritePetrology and Raman spectroscopy of high pressure phases in the Gujba CB chondrite and the shock history of the CB parent bodyShock‐induced thermal history of an <scp>EH</scp>3 chondrite, Asuka 10164Discovery of stishovite in Apollo 15299 sampleIntergrowth textures of diaplectic glass and crystal in shock-loaded P-anorthiteCaSiO3 perovskite in diamond indicates the recycling of oceanic crust into the lower mantleA new natural high-pressure (Na,Ca)-hexaluminosilicate [(CaxNa1−x)Al3+xSi3−xO11] in shocked Martian meteoritesTransmission electron microscope observation of α, β and γ (Mg, Fe)2SiO4 in shocked meteorites: planar defects and polymorphic transitionsEvidence for fractional crystallization of wadsleyite and ringwoodite from olivine melts in chondrules entrained in shock-melt veinsMicrostructures and structural phase transition in (Mg,Fe)SiO3 majoriteMicrostructural constraints on the mechanisms of the transformation to reidite in naturally shocked zirconEquations of state of ZrSiO<sub>4</sub>phases in the upper mantlePyroxene solid solution in garnets included in diamondDonwilhelmsite, [CaAl4Si2O11], a new lunar high-pressure Ca-Al-silicate with relevance for subducted terrestrial sedimentsHigh-pressure phase transformations of albite, jadeite and nephelinePhase transformations in the earth's mantle and subducting slabs: Implications for their compositions, seismic velocity and density structures and dynamicsHigh-pressure KAlSi3O8, an aluminosilicate with sixfold coordinationElucidation of impact event recorded in the lherzolitic shergottite NWA 7397Discovery of coesite from the martian shergottite Northwest Africa 8657Coesite and stishovite in shocked crystalline rocksCarbynes: Carriers of Primordial Noble Gases in MeteoritesQuartz–coesite–stishovite relations in shocked metaquartzites from the Vredefort impact structure, South AfricaAre quasicrystals really so rare in the Universe?Allabogdanite, the high-pressure polymorph of (Fe,Ni)2P, a stishovite-grade indicator of impact processes in the Fe–Ni–P systemEvidence of cross-cutting and redox reaction in Khatyrka meteorite reveals metallic-Al minerals formed in outer spaceDiamonds in MeteoritesFine‐structures of planar deformation features in shocked olivine: A comparison between Martian meteorites and experimentally shocked basalts as an indicator for shock pressureProbing the hydrothermal system of the Chicxulub impact craterPhase relations in the transition zoneNatural (Mg,Fe)SiO <sub>3</sub> -Ilmenite and -Perovskite in the Tenham MeteoriteAnatomy of black veins in Zagami: clues to the formation of high-pressure phasesMaohokite, a post‐spinel polymorph of MgFe<sub>2</sub>O<sub>4</sub> in shocked gneiss from the Xiuyan crater in ChinaThe cubic-tetragonal phase transition in the system majorite (Mg 4 Si 4 O 12 ) - pyrope (Mg 3 Al 2 Si 3 O 12 ), and garnet symmetry in the Earth's transition zoneA New Dense Crystalline SilicaSynthesis of polyynes to model the sp-carbon allotrope carbynePyroxene-Garnet Transformation in Coorara MeteoriteA New Allotropic Form of Carbon from the Ries CraterThe constitution of the mantle—ISynthesis of γ-Mg2SiO4Phase Diagrams for GeoscientistsA microstructural investigation of natural lamellar ringwoodite in olivine of the shocked Sixiangkou chondriteStability of the high-pressure polymorph of zircon (ZrSiO4) in the deep mantleFormation of high-pressure minerals in shocked L6 chondrite Yamato 791384: constraints on shock conditions and parent body sizeShock metamorphism of ordinary chondritesPhase relations in the system KAlSi3O8–NaAlSi3O8 at high pressure–high temperature conditions and their implication for the petrogenesis of linguniteA Post-Stishovite SiO <sub>2</sub> Polymorph in the Meteorite Shergotty: Implications for Impact EventsCa-rich majorite derived from high-temperature melt and thermally stressed hornblende in shock veins of crustal rocks from the Ries impact crater (Germany)Silicate perovskite from phase transformations of pyrope‐garnet at high pressure and temperatureDiscovery of the Fe-analogue of akimotoite in the shocked Suizhou L6 chondriteMineralogical evidence for the origin of diamond in ureilitesLonsdaleite, a Hexagonal Polymorph of DiamondHigh‐pressure phases in shock‐induced melt veins of the Umbarger L6 chondrite: Constraints of shock pressureIcosahedrite, Al63Cu24Fe13, the first natural quasicrystalDeep Mantle Cycling of Oceanic Crust: Evidence from Diamonds and Their Mineral InclusionsRocks from the Mantle Transition Zone: Majorite-Bearing Xenoliths from Malaita, Southwest PacificAkaogiite: An ultra-dense polymorph of TiO2 with the baddeleyite-type structure, in shocked garnet gneiss from the Ries Crater, GermanyThe breakdown of diopside to Ca-rich majorite and glass in a shocked H chondriteThe Majorite-Pyrope + Magnesiowüstite Assemblage: Constraints on the History of Shock Veins in ChondritesLonsdaleite is faulted and twinned cubic diamond and does not exist as a discrete materialHigh-resolution subsurface water-ice distributions on MarsNatural occurrence of Fe<sub>2</sub>SiO<sub>4</sub>-spinel in the shocked Umbarger L6 chondriteA large shock vein in L chondrite Roosevelt County 106: Evidence for a long‐duration shock pulse on the L chondrite parent bodyIce-VII inclusions in diamonds: Evidence for aqueous fluid in Earth’s deep mantleStability Relations of Silicate Spinels, Ilmenites, and PerovskitesOlivine-Garnet Transformation in a MeteoriteEvidence for the extraterrestrial origin of a natural quasicrystalNatural occurrence of reidite in the Xiuyan crater of ChinaElastic properties of hydrous ringwoodite (γ-phase) in Mg2SiO4Transformation textures, mechanisms of formation of high‐pressure minerals in shock melt veins of L6 chondrites, and pressure‐temperature conditions of the shock eventsTetragonal Almandine-Pyrope Phase, TAPP: finally a name for it, the new mineral jeffbeniteShock-induced growth and metastability of stishovite and coesite in lithic clasts from suevite of the Ries impact crater (Germany)New scaling laws on impact fragmentationA new natural, super-hard, transparent polymorph of carbon from the Popigai impact crater, RussiaStructural characterisation of the high-pressure phase CaAl 4 Si 2 O 11A Monoclinic Post-Stishovite Polymorph of Silica in the Shergotty MeteoriteThe system Mg2SiO4Fe2SiO4 at high pressures and temperaturesStellar MgSiO<sub>3</sub>Perovskite: A Shock-transformed Stardust Silicate Found in a MeteoriteHigh-pressure transformations in pyroxenesPost‐oxide phases of forsterite and enstatiteStructure and thermal history of the H-chondrite parent asteroid revealed by thermochronometryIn situ X-ray diffraction study of enstatite up to 12 GPa and 1473 K and equations of stateShock‐induced transition of NaAlSi<sub>3</sub>O<sub>8</sub> feldspar into a hollandite structure in a L6 chondriteHigh-pressure phases in a shock-induced melt vein of the Tenham L6 chondrite: Constraints on shock pressure and durationTissintite, (Ca, Na, □)AlSi2O6, a highly-defective, shock-induced, high-pressure clinopyroxene in the Tissint martian meteoriteNanoscale records of ancient shock deformation: Reidite (ZrSiO4) in sandstone at the Ordovician Rock Elm impact craterFirst Natural Occurrence of CoesiteMelting and crystal–liquid partitioning in the system Mg2SiO4–Fe2SiO4 to 25 GPaDiamonds from the Popigai impact structure, RussiaAkimotoite, (Mg,Fe)SiO<sub>3</sub>, a new silicate mineral of the ilmenite group in the Tenham chondriteCarbyne from First Principles: Chain of C Atoms, a Nanorod or a NanoropeDiamonds, Meteorites, and the Origin of the Solar System.Diamond and silicon carbide in impact melt rock from the Ries impact craterStability of CaCl<sub>2</sub>‐type and α‐PbO<sub>2</sub>‐type SiO<sub>2</sub> at high pressure and temperature determined by in‐situ X‐ray measurementsNatural high-pressure polymorph of merrillite in the shock veins of the Suizhou meteoriteAn Ultradense Polymorph of Rutile with Seven-Coordinated Titanium from the Ries CraterSymmetry change of majorite solid solution in the system Mg<sub>3</sub>Al<sub>2</sub>Si<sub>3</sub>O<sub>12</sub>-MgSiO<sub>3</sub>Ringwoodite, Natural (Mg,Fe)2SiO4 Spinel in the Tenham MeteoriteDiscovery of asimowite, the Fe-analog of wadsleyite, in shock-melted silicate droplets of the Suizhou L6 and the Quebrada Chimborazo 001 CB3.0 chondritesDmitryivanovite: A new high-pressure calcium aluminum oxide from the Northwest Africa 470 CH3 chondrite characterized using electron backscatter diffraction analysisDiscovery of coesite and stishovite in eucriteNatural NaAlSi <sub>3</sub> O <sub>8</sub> -Hollandite in the Shocked Sixiangkou MeteoriteShock-induced transformation of olivine to a new metastable (Mg,Fe)2SiO4 polymorph in Martian meteoritesLiebermannite, <scp>KA</scp>lSi<sub>3</sub>O<sub>8</sub>, a new shock‐metamorphic, high‐pressure mineral from the Zagami Martian meteoriteShock metamorphism and petrography of the Shergotty achondriteShock metamorphism of the Coconino Sandstone at Meteor Crater, ArizonaImpact-induced shock and the formation of natural quasicrystals in the early solar systemNatural Occurrence of MgSiO <sub>3</sub> -Ilmenite and Evidence for MgSiO <sub>3</sub> -Perovskite in a Shocked L ChondriteNatural CaTi2O4-structured FeCr2O4 polymorph in the Suizhou meteorite and its significance in mantle mineralogyHigh pressure minerals in the Château-Renard (L6) ordinary chondrite: implications for collisions on its parent bodyPostspinel transformations in the system Mg<sub>2</sub>SiO<sub>4</sub>‐Fe<sub>2</sub>SiO<sub>4</sub> and some geophysical implicationsRock fluidization during peak-ring formation of large impact structuresGarnet phase of MgSiO3 filling the pyroxene–ilmenite gap at very high temperaturePetrography and geochemistry of the chassignite Northwest Africa 2737 (NWA 2737)Back transformation and oxidation of (Mg, Fe)2SiO4 spinels at high temperaturesMan-Made DiamondsVestaite, (Ti4+Fe2+)Ti34+O9, a new mineral in the shocked eucrite Northwest Africa 8003The high-pressure phases of MgSiO3Host rock solid-state transformation in a shock-induced melt vein of Tenham L6 chondriteSolubility of water in the α, β and γ phases of (Mg,Fe) 2 SiO 4Heterogeneous mineral assemblages in martian meteorite Tissint as a result of a recent small impact event on MarsKinetics of the Coesite-Quartz Transition: Application to the Exhumation of Ultrahigh-Pressure RocksNatural QuasicrystalsFirst discovery of stishovite in an iron meteoriteMartian Dunite NWA 2737: Petrographic constraints on geological history, shock events, and olivine colorFractional crystallization of olivine melt inclusion in shock-induced chondritic melt veinStishovite, SiO<sub>2</sub>, a very high pressure new mineral from Meteor Crater, ArizonaAllabogdanite, (Fe,Ni)<sub>2</sub>P, a new mineral from the Onello meteorite: The occurrence and crystal structureMicrostructural dynamics of central uplifts: Reidite offset by zircon twins at the Woodleigh impact structure, AustraliaStability of majorite (Mg, Fe)SiO3 at high pressures and 1800°CA large planetary body inferred from diamond inclusions in a ureilite meteoriteBaddeleyite-Type High-Pressure Phase of TiO <sub>2</sub>High-pressure modifications of CaAl2O4 and CaGa2O4The constitution of the mantle—IISubduction of continental crust and terrigenous and pelagic sediments: an experimental studyHigh-Pressure Phase Transitions of the Feldspars, and Further Characterization of LingunitePressure-induced structural modifications and amorphization in olivine compoundsHigh‐pressure polymorphs in Yamato‐790729 L6 chondrite and their significance for collisional conditionsThe effect of Fe on the crystal structure of wadsleyite ?-(Mg1 ? x Fe x )2SiO4, 0.00?x?0.40Plagioclase breakdown as an indicator for shock conditions of meteoritesMaskelynite: Formation by Explosive ShockSystematics and Evaluation of Meteorite ClassificationReidite: An impact-produced high-pressure polymorph of zircon found in marine sedimentsCarbyne Forms of Carbon: Do They Exist?Equation of state of lower mantle (Al,Fe)-MgSiO3 perovskiteTuite, gamma-Ca3(PO4)2: a new mineral from the Suizhou L6 chondriteCarbon: Observations on the New Allotropic FormPreviously unknown quasicrystal periodic approximant found in spaceMelting experiments on anhydrous peridotite KLB‐1 from 5.0 to 22.5 GPaSynthesis of Mg2SiO4-Fe2SiO4 spinel solid solutionsNatural occurrence and synthesis of two new postspinel polymorphs of chromiteXieite, a new mineral of high-pressure FeCr2O4 polymorphHigh pressure transitions in the system KAlSi3O8-NaAlSi3O8Ureilitic breccias: clues to the petrologic structure and impact disruption of the ureilite parent asteroidSeifertite, a dense orthorhombic polymorph of silica from the Martian meteorites Shergotty and ZagamiEffects of shock and Martian alteration on Tissint hydrogen isotope ratios and water contentPressure‐temperature phase diagram for the Allende meteoriteHigh‐pressure polymorphism of Fe<sub>2</sub>P and its implications for meteorites and Earth's coreHigh-pressure (Mg, Fe)2SiO4 phases in the Tenham chondritic meteoriteNew Decagonal Al–Ni–Fe and Al–Ni–Co Alloys Prepared by Liquid QuenchingA high pressure hexagonal form of MgSiO3Kinetic studies of the .ALPHA.-quartz-coesite transformation of SiO2.Materials — ultrahard polycrystalline diamond from graphite
- 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科学研究費助成事業データベース科学研究費助成事業データベース科学研究費助成事業データベース科学研究費助成事業データベース科学研究費助成事業データベースCrossrefCrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 12307800