{"@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/1360855568720824832.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/s0012-821x(03)00695-2"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012821X03006952?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012821X03006952?httpAccept=text/plain"}}],"dc:title":[{"@value":"A new natural high-pressure (Na,Ca)-hexaluminosilicate [(CaxNa1−x)Al3+xSi3−xO11] in shocked Martian meteorites"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380855568720824832","@type":"Researcher","foaf:name":[{"@value":"Pierre Beck"}]},{"@id":"https://cir.nii.ac.jp/crid/1380855568720824834","@type":"Researcher","foaf:name":[{"@value":"Philippe Gillet"}]},{"@id":"https://cir.nii.ac.jp/crid/1380855568720824835","@type":"Researcher","foaf:name":[{"@value":"Laurent Gautron"}]},{"@id":"https://cir.nii.ac.jp/crid/1380855568720824833","@type":"Researcher","foaf:name":[{"@value":"Isabelle Daniel"}]},{"@id":"https://cir.nii.ac.jp/crid/1380855568720824836","@type":"Researcher","foaf:name":[{"@value":"Ahmed El Goresy"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"0012821X"}],"prism:publicationName":[{"@value":"Earth and Planetary Science Letters"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2004-02","prism:volume":"219","prism:number":"1-2","prism:startingPage":"1","prism:endingPage":"12"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0012821X03006952?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0012821X03006952?httpAccept=text/plain"}],"createdAt":"2004-01-23","modifiedAt":"2019-02-15","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004235936359296","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Curious kinetic behavior in silica polymorphs solves seifertite puzzle in shocked meteorite"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707111862656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High-pressure phase relations in the system CaAl4Si2O11–NaAl3Si3O11 with implication for Na-rich CAS phase in shocked Martian meteorites"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707402286720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Phase transformations of Ca3Al2Si3O12 grossular garnet to the depths of the Earth's mantle transition zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285714482798720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Lunar and Martian Silica"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182088682496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"U–Pb isotopic systematics of shock-loaded and annealed baddeleyite: Implications for crystallization ages of Martian meteorite shergottites"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182119961856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Shock-induced deformation of Shergottites: Shock-pressures and perturbations of magmatic ages on Mars"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182379079552","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Formation of a metastable hollandite phase from amorphous plagioclase: A possible origin of lingunite in shocked chondritic meteorites"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846643276521472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High‐pressure minerals in shocked meteorites"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657355773056","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Phase transition processes of olivine in the shocked Martian meteorite Tissint: Clues to origin of ringwoodite-, bridgmanite- and magnesiowüstite-bearing assemblages"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848658887233408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Natural dissociation of olivine to (Mg,Fe)SiO\n            <sub>3</sub>\n            perovskite and magnesiowüstite in a shocked Martian meteorite"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593666753024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Elucidation of impact event recorded in the lherzolitic shergottite NWA 7397"}]},{"@id":"https://cir.nii.ac.jp/crid/1390854064974986880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A High-Pressure Mineral in a Meteorite and Collision Process Revealed by TEM"},{"@language":"ja","@value":"TEMで解き明かす隕石中の高圧鉱物と衝突過程"},{"@language":"ja-Kana","@value":"TEM デ トキアカス インセキ チュウ ノ コウアツ コウブツ ト ショウトツ カテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942153536512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Natural and experimental high-pressure, shock-produced terrestrial and extraterrestrial materials"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892104880128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Can quasicrystals survive in planetary collisions?"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/s0012-821x(03)00695-2"},{"@type":"CROSSREF","@value":"10.1126/sciadv.1500075_references_DOI_7r6TR8f0P45PKyJxQPHGOn6CHdZ"},{"@type":"CROSSREF","@value":"10.3390/min8070267_references_DOI_7r6TR8f0P45PKyJxQPHGOn6CHdZ"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2012.10.002_references_DOI_7r6TR8f0P45PKyJxQPHGOn6CHdZ"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2009.11.043_references_DOI_7r6TR8f0P45PKyJxQPHGOn6CHdZ"},{"@type":"CROSSREF","@value":"10.1186/s40645-021-00421-y_references_DOI_7r6TR8f0P45PKyJxQPHGOn6CHdZ"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2016.08.006_references_DOI_7r6TR8f0P45PKyJxQPHGOn6CHdZ"},{"@type":"CROSSREF","@value":"10.1111/maps.12902_references_DOI_7r6TR8f0P45PKyJxQPHGOn6CHdZ"},{"@type":"CROSSREF","@value":"10.1073/pnas.1016921108_references_DOI_7r6TR8f0P45PKyJxQPHGOn6CHdZ"},{"@type":"CROSSREF","@value":"10.4131/jshpreview.31.157_references_DOI_7r6TR8f0P45PKyJxQPHGOn6CHdZ"},{"@type":"CROSSREF","@value":"10.1111/maps.13735_references_DOI_7r6TR8f0P45PKyJxQPHGOn6CHdZ"},{"@type":"CROSSREF","@value":"10.1186/s40645-021-00451-6_references_DOI_7r6TR8f0P45PKyJxQPHGOn6CHdZ"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2017.09.006_references_DOI_7r6TR8f0P45PKyJxQPHGOn6CHdZ"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2011.02.001_references_DOI_7r6TR8f0P45PKyJxQPHGOn6CHdZ"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2012.06.002_references_DOI_7r6TR8f0P45PKyJxQPHGOn6CHdZ"}]}