{"@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/1360004232135215488.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.epsl.2011.05.010"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012821X11002810?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012821X11002810?httpAccept=text/plain"}},{"identifier":{"@type":"NAID","@value":"10030499148"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Evidence for multiple dynamic events and subsequent decompression stage recorded in a shock vein"}],"description":[{"notation":[{"@value":"We investigated a shock vein of the Yamato 791384 L6 chondrite to clarify the nature and sequence of the dynamic processes that resulted from the shock events. The chondritic host-rock of Y-791384 mainly consists of olivine (Fa24–25), low-Ca pyroxene (Fs18–22), albitic feldspar (An9–10Ab84–86Or5–7), troilite and metallic Fe–Ni. The shock vein contains majorite (or majorite-pyropess) and magnesiowustite (+ minor jadeite) as high-pressure polymorphs. Two different dynamic events were recorded in the shock vein. The majorite grain contained vitrified (Mg,Fe)SiO3-perovskite inclusions. The (Mg,Fe)SiO3-perovskite was crystallized from a chondritic melt, and is a remnant of a first dynamic event. The majorite and magnesiowustite were also crystallized directly from a chondritic melt but induced by a second dynamic event. The pressure condition for the first and second dynamic events would be >~24 GPa and <~22 GPa, respectively. Pervasive feather-shaped olivine (Fa16) nucleated on the magnesiowustite and majorite. This feather-shaped olivine is evidence for rapidly grown olivine from the melt related to the shock event. Phase relations deduced from high-pressure melting experiments of the Allende meteorite and peridotite indicate that the magnesiowustite and majorite + olivine pair cannot coexist at equilibrium condition. The disequilibrium assemblage reflects a decompression stage. These features demonstrate the complexity of events during a natural dynamic process."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420564276190572672","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"90400241"},{"@type":"NRID","@value":"1000090400241"},{"@type":"NRID","@value":"9000005339723"},{"@type":"NRID","@value":"9000406037723"},{"@type":"NRID","@value":"9000370745807"},{"@type":"NRID","@value":"9000406040039"},{"@type":"NRID","@value":"9000256493633"},{"@type":"NRID","@value":"9000001491802"},{"@type":"NRID","@value":"9000411393573"},{"@type":"NRID","@value":"9000415313124"},{"@type":"NRID","@value":"9000002103202"},{"@type":"NRID","@value":"9000005336674"},{"@type":"NRID","@value":"9000290139430"},{"@type":"NRID","@value":"9000254454299"},{"@type":"NRID","@value":"9000406039308"},{"@type":"NRID","@value":"9000254061922"},{"@type":"NRID","@value":"9000254454380"},{"@type":"NRID","@value":"9000367422086"},{"@type":"NRID","@value":"9000256493545"},{"@type":"NRID","@value":"9000017443621"},{"@type":"NRID","@value":"9000256491986"},{"@type":"NRID","@value":"9000001910719"},{"@type":"NRID","@value":"9000002048198"},{"@type":"NRID","@value":"9000257916750"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0149905"}],"foaf:name":[{"@value":"Masaaki 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Ohtani"}]},{"@id":"https://cir.nii.ac.jp/crid/1420001326229056384","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"20142226"},{"@type":"NRID","@value":"1000020142226"},{"@type":"NRID","@value":"9000002203822"},{"@type":"NRID","@value":"9000392140284"},{"@type":"NRID","@value":"9000007631486"},{"@type":"NRID","@value":"9000002250429"},{"@type":"NRID","@value":"9000258434787"},{"@type":"NRID","@value":"9000004619243"},{"@type":"NRID","@value":"9000025001631"},{"@type":"NRID","@value":"9000002250523"},{"@type":"NRID","@value":"9000005301811"},{"@type":"NRID","@value":"9000339174420"},{"@type":"NRID","@value":"9000002203330"},{"@type":"NRID","@value":"9000406037102"},{"@type":"NRID","@value":"9000002255447"},{"@type":"NRID","@value":"9000002204788"},{"@type":"NRID","@value":"9000006217004"},{"@type":"NRID","@value":"9000270176587"},{"@type":"NRID","@value":"9000406040018"},{"@type":"NRID","@value":"9000002250151"},{"@type":"NRID","@value":"9000002255540"},{"@type":"NRID","@value":"9000335567974"},{"@type":"NRID","@value":"9000370281580"},{"@type":"NRID","@value":"9000002250835"},{"@type":"NRID","@value":"9000335567904"},{"@type":"NRID","@value":"9000002255440"},{"@type":"NRID","@value":"9000002250365"},{"@type":"NRID","@value":"9000002250431"},{"@type":"NRID","@value":"9000339174496"},{"@type":"NRID","@value":"9000406037720"},{"@type":"NRID","@value":"9000258417829"},{"@type":"NRID","@value":"9000021529987"},{"@type":"NRID","@value":"9000018228469"},{"@type":"NRID","@value":"9000010715536"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0169673"}],"foaf:name":[{"@value":"Makoto 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BV"}],"prism:publicationDate":"2011-07","prism:volume":"307","prism:number":"3-4","prism:startingPage":"361","prism:endingPage":"368"},"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:S0012821X11002810?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0012821X11002810?httpAccept=text/plain"}],"createdAt":"2011-06-06","modifiedAt":"2025-09-15","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782100825600","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"22000002"},{"@type":"JGN","@value":"JP22000002"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-22000002/"}],"notation":[{"@language":"ja","@value":"地球惑星中心領域の超高圧物質科学"},{"@language":"en","@value":"Ultrahigh-Pressure Material Science of the central regions of the Earth and Planets"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000782120089216","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"22540488"},{"@type":"JGN","@value":"JP22540488"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-22540488/"}],"notation":[{"@language":"ja","@value":"コンドライト形成過程の復元に関する鉱物科学的研究"},{"@language":"en","@value":"Mineralogical study on the formation process of chondrites"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050587981426597504","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Formation and decomposition of vacancy-rich clinopyroxene in a shocked eucrite : New insights for multiple impact events"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002217131060608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Coesite and stishovite in a shocked lunar meteorite, 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