{"@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/1361981469496863744.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.160.3823.66"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.160.3823.66"}}],"dc:title":[{"@value":"Olivine-Garnet Transformation in a Meteorite"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>\n            Garnet has been identified for the first time as a meteorite mineral in the Coorara chondrite from Western Australia. It replaces olivine grains in a 1-millimeter veinlet traversing the body of the meteorite. The associated olivine has abnormally low birefringence, which suggests a highly shocked condition. Microprobe analyses do not distinguish the garnet from the associated olivine, which has the composition (Mg\n            <jats:sub>.75</jats:sub>\n            Fe\n            <jats:sub>.25</jats:sub>\n            )\n            <jats:sub>2</jats:sub>\n            SiO\n            <jats:sub>4</jats:sub>\n            ; the garnet may have the composition Mg\n            <jats:sub>3</jats:sub>\n            Fe\n            <jats:sub>2</jats:sub>\n            Si\n            <jats:sub>3</jats:sub>\n            O\n            <jats:sub>12</jats:sub>\n            but be unresolvable from the accompanying olivine, or alternatively is nonstoichiometric. Transformation of olivine to garnet under high pressure could have significant implications for the phase composition of the Earth's mantle.\n          </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381981469496863745","@type":"Researcher","foaf:name":[{"@value":"Brian Mason"}],"jpcoar:affiliationName":[{"@value":"U.S. National Museum, Washington, D.C. 20560"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469496863744","@type":"Researcher","foaf:name":[{"@value":"J. Nelen"}],"jpcoar:affiliationName":[{"@value":"U.S. National Museum, Washington, D.C. 20560"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469496863746","@type":"Researcher","foaf:name":[{"@value":"John S. White"}],"jpcoar:affiliationName":[{"@value":"U.S. National Museum, Washington, D.C. 20560"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00368075"},{"@type":"EISSN","@value":"10959203"}],"prism:publicationName":[{"@value":"Science"}],"dc:publisher":[{"@value":"American Association for the Advancement of Science (AAAS)"}],"prism:publicationDate":"1968-04-05","prism:volume":"160","prism:number":"3823","prism:startingPage":"66","prism:endingPage":"67"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.160.3823.66"}],"createdAt":"2006-10-05","modifiedAt":"2024-01-11","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360298757432488704","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Bridgmanite Freezing in Shocked Meteorites Due To Amorphization‐Induced Stress"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565169054229888","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Infrared and Mossbauer Spectra of Synthetic Garnets A3Fe2Si3O12 (A: Mn, Cd, Ca)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092406786944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Systematic investigations of high‐pressure polymorphs in shocked ordinary chondrites"}]},{"@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/1390282681502662784","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"High-pressure minerals in the Earth and planetary materials"},{"@language":"ja","@value":"地球惑星物質中の高圧鉱物"},{"@language":"ja-Kana","@value":"チキュウ ワクセイ ブッシツ チュウ ノ コウアツ コウブツ"}]},{"@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"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1126/science.160.3823.66"},{"@type":"CROSSREF","@value":"10.1029/2022gl098231_references_DOI_FEepeCClb622Cxjl3JuE4y7Zt0p"},{"@type":"CROSSREF","@value":"10.2465/gkk.111226_references_DOI_FEepeCClb622Cxjl3JuE4y7Zt0p"},{"@type":"CROSSREF","@value":"10.1111/maps.13608_references_DOI_FEepeCClb622Cxjl3JuE4y7Zt0p"},{"@type":"CROSSREF","@value":"10.1111/maps.12902_references_DOI_FEepeCClb622Cxjl3JuE4y7Zt0p"},{"@type":"CROSSREF","@value":"10.1186/s40645-021-00451-6_references_DOI_FEepeCClb622Cxjl3JuE4y7Zt0p"},{"@type":"CROSSREF","@value":"10.1246/bcsj.50.3186_references_DOI_FEepeCClb622Cxjl3JuE4y7Zt0p"}]}