{"@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/1361137046101839232.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.epsl.2004.08.018"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012821X04005217?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012821X04005217?httpAccept=text/plain"}},{"identifier":{"@type":"NAID","@value":"30007244648"}}],"dc:title":[{"@value":"Formation of high-pressure minerals in shocked L6 chondrite Yamato 791384: constraints on shock conditions and parent body size"}],"description":[{"notation":[{"@value":"We have studied the high-pressure phases observed in Yamato 791384 L6 chondrite. Host meteorite mainly consists of olivine, pyroxenes and plagioclase glass. Mineral fragments observed in the veins and the vein margin region of the host meteorite were partially or totally transformed into high-pressure phases; ringwoodite, majorite, akimotoite, NaAlSi3O8 hollandite and jadeite. Matrix of the shock vein contains majorite–pyrope solid solution. The spatial distribution indicates that high-pressure phases are present in the shock veins and host rocks adjacent to the shock veins. Investigation of the high-pressure phases revealed that, in Y791384, fragments and adjacent matrix were subjected to pressures around of 18–23 GPa and the vein experienced temperatures around 2300 °C during the shock event. Ringwoodite lamellae were observed in the host olivine adjacent to the vein. Kinetic investigation for ringwoodite lamellar growth in olivine indicates that the shocked meteorite experienced the pressure for at least 4 s. Such long duration of the pressure pulse indicates that the size of the parent body was greater than 10 km."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381137046101839234","@type":"Researcher","foaf:name":[{"@value":"Eiji Ohtani"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137046101839236","@type":"Researcher","foaf:name":[{"@value":"Yukiko Kimura"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137046101839235","@type":"Researcher","foaf:name":[{"@value":"Makoto Kimura"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137046101839232","@type":"Researcher","foaf:name":[{"@value":"Toshiko Takata"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137046101839237","@type":"Researcher","foaf:name":[{"@value":"Tadashi Kondo"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137046101839233","@type":"Researcher","foaf:name":[{"@value":"Tomoaki Kubo"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"0012821X"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/0012821X"}],"prism:publicationName":[{"@value":"Earth and Planetary Science Letters"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2004-11","prism:volume":"227","prism:number":"3-4","prism:startingPage":"505","prism:endingPage":"515"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","https://www.elsevier.com/legal/tdmrep-license"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0012821X04005217?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0012821X04005217?httpAccept=text/plain"}],"createdAt":"2004-09-29","modifiedAt":"2025-11-02","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050005508516260736","@type":"Article","resourceType":"学術雑誌論文(journal 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garnet in a shocked chondritic meteorite"},{"@value":"Discovery of natural MgSiO\n            <sub>3</sub>\n            tetragonal garnet in a shocked chondritic meteorite"}]},{"@id":"https://cir.nii.ac.jp/crid/1050306506451268352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Widespread Tissintite in Strongly Shock-Lithified Lunar Regolith Breccias"},{"@value":"Widespread Tissintite in Strongly Shock‐Lithified Lunar Regolith Breccias"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216855511936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Jadeite in Chelyabinsk meteorite and the nature of an impact event on its parent body"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232135215488","@type":"Article","resourceType":"学術雑誌論文(journal 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カガク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206526497408","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"High-pressure polymorphs in shocked meteorites"},{"@language":"ja","@value":"衝撃を経験した隕石に含まれる高圧相"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206544944256","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Raman spectroscopic study of a garnetite xenolith from Malaita, Southwest Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206546754944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Jadeite in shocked meteorites and its textural variations"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206546995456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Jadeitite (jadeite jade) from Japan: History, characteristics, and perspectives"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680523043712","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Amorphization of plagioclase under ultrahigh-pressure"},{"@language":"ja","@value":"超高圧下における斜長石の非晶質化"}]},{"@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/1390282681502781440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Introduction to Meteorite Mineralogy"},{"@language":"ja","@value":"隕石中の鉱物：序説"},{"@value":"日本鉱物科学会賞第11回受賞者 受賞記念研究紹介 隕石中の鉱物 : 序説"},{"@language":"ja-Kana","@value":"ニホン コウブツ カガクカイショウ ダイ11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 インセキ チュウ ノ コウブツ : ジョセツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390585869249091328","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"極限かつ複合動的試料環境下におけるサブミリ秒X線回折計測手法の開発"},{"@language":"en","@value":"Development of a Sub-millisecond X-ray Diffraction System under Changing Temperature and Pressure Conditions"},{"@value":"極限かつ複合動的試料環境下におけるサブミリ秒X線回折計測手法の開発 : 総合報告(学会賞受賞論文)"},{"@language":"ja-Kana","@value":"キョクゲン カツ フクゴウ ドウテキ シリョウ カンキョウ カ ニ オケル サブミリビョウ Xセン カイセツ ケイソク シュホウ ノ カイハツ : ソウゴウ ホウコク(ガッカイショウ ジュショウ ロンブン)"}]},{"@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 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