{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1363388844160796672.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1111/j.1365-246x.1981.tb04891.x"}},{"identifier":{"@type":"URI","@value":"http://academic.oup.com/gji/article-pdf/66/3/579/1829560/66-3-579.pdf"}}],"dc:title":[{"@value":"Thermodynamic parameters in the Earth as determined from seismic profiles"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004053943819137","@type":"Researcher","foaf:name":[{"@value":"J. M. Brown"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388844160796672","@type":"Researcher","foaf:name":[{"@value":"T. J. Shankland"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"0956540X"},{"@type":"EISSN","@value":"1365246X"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/00168009"}],"prism:publicationName":[{"@value":"Geophysical Journal International"}],"dc:publisher":[{"@value":"Oxford University Press (OUP)"}],"prism:publicationDate":"1981-09","prism:volume":"66","prism:number":"3","prism:startingPage":"579","prism:endingPage":"596"},"reviewed":"false","url":[{"@id":"http://academic.oup.com/gji/article-pdf/66/3/579/1829560/66-3-579.pdf"}],"createdAt":"2007-04-03","modifiedAt":"2019-03-24","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050025031472885632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Retention of water in subducted slabs under core-mantle boundary conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1050285299888313600","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Hydrous magnesium-rich magma genesis at the top of the lower mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1050850412716474624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Compressional behavior and spin state of δ-(Al,Fe)OOH at high pressures"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215289972352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High-P, T phase relations in the NaAlSi2O6 system from first principles computation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215916266624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stability of a hydrous δ-phase, AlOOH–MgSiO2(OH)2, and a mechanism for water transport into the base of lower mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216799523968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The pyrite-type high-pressure form of FeOOH"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004229805679232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sound velocities of aluminum‐bearing stishovite in the mantle transition zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004231198784512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reaction boundary between akimotoite and ringwoodite + stishovite in MgSiO3"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004231906435840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mineralogy of the Deep Mantle – The Post-Perovskite Phase and its Geophysical Significance"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232425629312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sound velocities of Fe3Al2Si3O12 almandine up to 19 GPa and 1700 K"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232425662464","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High-pressure phase relation of KREEP basalts: A clue for finding the lost Hadean crust?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232523501056","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Electrical conductivity of the oceanic asthenosphere and its interpretation based on laboratory measurements"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233290488320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ab initio investigation on the high‐temperature thermodynamic properties of Fe<sup>3+</sup>‐bearing MgSiO<sub>3</sub> perovskite"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233419327616","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A perovskitic lower mantle inferred from high-pressure, high-temperature sound velocity data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004234589745536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Three-dimensional electrical conductivity structure beneath Australia from inversion of geomagnetic observatory data: evidence for lateral variations in transition-zone temperature, water content and melt"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005516841542400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stability of Fe-bearing hydrous phases and element partitioning in the system MgO–Al2O3–Fe2O3–SiO2–H2O in Earth's lowermost mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005517197820032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Phase relations of MgSiO3-FeSiO3 system up to 64 GPa and 2300 K using multianvil apparatus with sintered diamond anvils"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005518172987648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"First‐Principles Determination of the Dissociation Phase Boundary of Phase H MgSiO<sub>4</sub>H<sub>2</sub>"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168754316672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sound Velocity of MgSiO<sub>3</sub> Majorite Garnet up to 18 GPa and 2000 K"}]},{"@id":"https://cir.nii.ac.jp/crid/1360013168779014400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The influence of δ-(Al,Fe)OOH on seismic heterogeneities in Earth’s lower mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360016864411897856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermal conductivity of platinum and periclase under extreme conditions of pressure and temperature"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017282460949632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Post‐Perovskite Phase Transition in the Pyrolitic Lowermost Mantle: Implications for Ubiquitous Occurrence of Post‐Perovskite Above CMB"}]},{"@id":"https://cir.nii.ac.jp/crid/1360022306713933440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermal equation of state of F-bearing superhydrous phase B (Mg10Si3O14(OH,F)4): Implications for the transportation of fluorine and water into Earth's lower mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691090465152","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Water partitioning in the Earth's mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704777661056","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"<i>P‐V‐T</i> equation of state of cubic CaSiO<sub>3</sub> perovskite from first‐principles computation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707111988608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Melting relationships in the Fe–Fe3S system up to the outer core conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707112196224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Water partitioning between bridgmanite and postperovskite in the lowermost mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707112318208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Increase of the oxygen vacancy component in bridgmanite with temperature"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707112320384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Iron isotopic fractionation in mineral phases from Earth's lower mantle: Did terrestrial magma ocean crystallization fractionate iron isotopes?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707402309120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sound velocities measurement on MgSiO3 akimotoite at high pressures and high temperatures with simultaneous in situ X-ray diffraction and ultrasonic study"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285709966681984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"<i>Ab initio</i>\n lattice thermal conductivity of MgO from a complete solution of the linearized Boltzmann transport equation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285713381493120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Decomposition boundary from high-pressure clinoenstatite to wadsleyite + stishovite in MgSiO3"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285713381504512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stability of Al-bearing superhydrous phase B at the mantle transition zone and the uppermost lower mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360286991877813376","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"New aluminium hydroxide at multimegabar pressures: Implications for water reservoirs in deep planetary interiors"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165811086080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Hydrous minerals and the storage of water in the deep mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166067185536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stability of Fe–Ni hydride after the reaction between Fe–Ni alloy and hydrous phase (δ-AlOOH) up to 1.2Mbar: Possibility of H contribution to the core density deficit"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166760641152","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stability of hydrous silicate at high pressures and water transport to the deep lower mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565167789932800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"<i>Ab initio</i>Lattice Thermal Conductivity of<mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" display=\"inline\"><mml:msub><mml:mi>MgSiO</mml:mi><mml:mn>3</mml:mn></mml:msub></mml:math>Perovskite as Found in Earth’s Lower Mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182127438976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The second continent: Existence of granitic continental materials around the bottom of the mantle transition zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182379058816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Phase relations in the system MgSiO 3 –Al 2 O 3 up to 52 GPa and 2000 K"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567183240098432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effect of pressure on grain‐growth kinetics of ferropericlase to lower mantle conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567183490991104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effect of cation substitution on bridgmanite elasticity: A key to interpret seismic anomalies in the lower mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567183909433856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Temperature profile in the lowermost mantle from seismological and mineral physics joint modeling"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567184543211008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Methods for inversion of body-wave waveforms for localized three-dimensional seismic structure and an application to D′′ structure beneath Central America"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567184543306496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Waveform inversion for localized three-dimensional seismic velocity structure in the lowermost mantle beneath the Western Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846639281667968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Shock Compression and Melting of an Fe‐Ni‐Si Alloy: Implications for the Temperature Profile of the Earth's Core and the Heat Flux Across the Core‐Mantle Boundary"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640220132992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Elastic wave velocity of polycrystalline Mj80Py20 garnet to 21 GPa and 2,000 K"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640846330112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sound velocity measurements of CaSiO3 perovskite to 133GPa and implications for lowermost mantle seismic anomalies"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640846529792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Supercritical fluid in the mantle transition zone deduced from H–D interdiffusion of wadsleyite"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846643368189056","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Iron Partitioning and Density Changes of Pyrolite in Earth’s Lower Mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654734561792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Precise measurements of enthalpy of postspinel transition in Mg<sub>2</sub>SiO<sub>4</sub> and application to the phase boundary calculation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657065735808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Melting behavior of the lower-mantle ferropericlase across the spin crossover: Implication for the ultra-low velocity zones at the lowermost mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657104193408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High-pressure phase transitions of anorthosite crust in the Earth's deep mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657355761152","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Phase transitions of serpentine in the lower mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848658366837120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Computational support for a pyrolitic lower mantle containing ferric iron"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848660499789056","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermodynamic properties of (Mg,Fe2+)SiO3 perovskite at the lower-mantle pressures and temperatures: an internally consistent LSDA+<i>U</i>study"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567792849408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Discriminating lower mantle composition"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567814480000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High-resolution 3-D S-velocity structure in the D″ region at the western margin of the Pacific LLSVP: Evidence for small-scale plumes and paleoslabs"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593683835264","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Single-crystal X-ray structure refinement of Al-bearing superhydrous phase B"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861705562171520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sound Velocities of Superhydrous Phase B up to 21 GPa and 900 K"}]},{"@id":"https://cir.nii.ac.jp/crid/1361131416748377728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effect of spin transition of iron on the thermal conductivity of (Fe, Al)-bearing bridgmanite"}]},{"@id":"https://cir.nii.ac.jp/crid/1361975287438746880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Elastic wave velocities of (Mg0.91Fe0.09)2SiO4 ringwoodite under P–T conditions of the mantle transition region"}]},{"@id":"https://cir.nii.ac.jp/crid/1364227868969768448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermoelastic Properties of K0.7Na0.3AlSi3O8 Hollandite and NaAlSi2O6 Jadeite: Implication for the Fate of the Subducted Continental Crust in the Deep Mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204238418944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"地球型惑星内部物理学の最近の進展"},{"@language":"en","@value":"Recent Advances in Geophysical Studies of the Interior of Terrestrial Planets"},{"@language":"ja-Kana","@value":"チキュウガタ ワクセイ ナイブ ブツリガク ノ サイキン ノ シンテン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204381782656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Development of Sintered Diamond Techniques in Kawai-Type Apparatus and its Applications to Mineralogy of the Lower Mantle"},{"@language":"ja","@value":"焼結ダイヤモンドアンビルを用いた川井式装置による高圧発生技術の開発と下部マントル鉱物学への応用"},{"@value":"受賞記念解説 高圧力学会奨励賞 焼結ダイヤモンドアンビルを用いた川井式装置による高圧発生技術の開発と下部マントル鉱物学への応用"},{"@language":"ja-Kana","@value":"ジュショウ キネン カイセツ コウアツリョク ガッカイ ショウレイショウ ショウケツ ダイヤモンドアンビル オ モチイタ カワイシキ ソウチ ニ ヨル コウアツ ハッセイ ギジュツ ノ カイハツ ト カブ マントル コウブツガク エ ノ オウヨウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206526075008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"第一原理計算による理論高圧鉱物物性学の開拓"},{"@language":"en","@value":"Creation of the ab initio theoretical high-pressure mineral physics"},{"@value":"日本鉱物科学会賞第12回受賞者 受賞記念研究紹介 第一原理計算による理論高圧鉱物物性学の開拓"},{"@language":"ja-Kana","@value":"ニホン コウブツ カガクカイショウ ダイ12カイ ジュショウシャ ジュショウ キネン ケンキュウ ショウカイ ダイイチ ゲンリ ケイサン ニ ヨル リロン コウアツ コウブツ ブッセイガク ノ カイタク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681501709696","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"主要マントル鉱物の高温高圧物性と実験地球物理学"},{"@language":"en","@value":"Experimental geophysics—measurement of physical and chemical properties of major mantle minerals at high pressures and temperatures"},{"@value":"日本鉱物科学会賞第14回受賞者 受賞記念研究紹介 主要マントル鉱物の高温高圧物性と実験地球物理学"},{"@language":"ja-Kana","@value":"ニホン コウブツ カガクカイショウ ダイ14カイ ジュショウシャ ジュショウ キネン ケンキュウ ショウカイ シュヨウ マントル コウブツ ノ コウオン コウアツ ブッセイ ト ジッケン チキュウ ブツリガク"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792003430784","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The sound velocity of wüstite at high pressures : implications for low-velocity anomalies at the base of the lower mantle"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1111/j.1365-246x.1981.tb04891.x"},{"@type":"CROSSREF","@value":"10.1007/s00269-012-0485-0_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1038/nature22823_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1002/2016gl068377_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1007/s00269-016-0869-7_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1029/2012jb009696_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1038/nature11004_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1093/gji/ggt455_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1029/2019gl083472_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.2138/am-2019-6913_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2012.09.038_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.4131/jshpreview.21.221_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2015.05.007_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.gsf.2017.10.002_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2008.01.003_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1029/2021gl093499_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1038/s41598-021-91180-9_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1080/08957959.2023.2193892_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1029/2021gl096219_references_DOI_YBnjK6BGWObx0SyKJmqynzNwdt3"},{"@type":"CROSSREF","@value":"10.1002/2013jb010905_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1103/physrevb.95.184303_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.2138/am-2018-6499_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2017.12.032_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2015.06.004_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2016.05.006_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.2465/gkk.150104_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2018.10.014_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1186/s40645-020-00333-3_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2021.106824_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1038/s41561-024-01464-8_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1038/ngeo2074_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1103/physrevlett.110.025904_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1029/2010gl043491_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1038/srep33337_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1073/pnas.0905920106_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1093/gji/ggt520_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1093/gji/ggu288_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2018.09.014_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2014.05.059_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2017.12.004_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.2465/gkk.161209_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.icarus.2019.113539_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1002/2017jb014723_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1007/s00269-014-0712-y_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1126/science.1181443_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1002/2015jb012211_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1038/ngeo2458_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1111/j.1365-246x.2012.05511.x_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.chemgeo.2015.05.005_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2020.106552_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2020.106544_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1007/s00269-021-01152-8_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1029/2022gl098674_references_DOI_YBnjK6BGWObx0SyKJmqynzNwdt3"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2019.05.042_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2019.106297_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2018.10.034_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2012.06.040_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2017.07.001_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2013.06.005_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.5026/jgeography.124.1_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1038/s41598-019-43949-2_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2010.08.003_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.gsf.2012.08.003_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/b978-0-444-53802-4.00054-3_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2012.01.002_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.2138/am-2018-6313ccby_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2016.08.009_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.3390/min10030261_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2019.115714_references_DOI_O2uZCEaOeBmob5PHjRm1j1I167D"}]}