{"@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/1360848660728024192.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1111/maps.12738"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fmaps.12738"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/maps.12738"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Shock‐induced thermal history of an <scp>EH</scp>3 chondrite, Asuka 10164"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>Shock‐induced features are abundantly observed in meteorites. Especially, shock veins, including high‐pressure minerals, characterize many kinds of heavily shocked meteorite. On the other hand, no high‐pressure phases have been yet reported from enstatite chondrites. We studied a heavily shocked <jats:styled-content style=\"fixed-case\">EH</jats:styled-content>3 chondrite, Asuka 10164, containing a vein, which comprises fragments of fine‐grained silicate and opaque minerals, and chondrules. In this vein, we found a silica polymorph, coesite. This is the first discovery of a high‐pressure phase in enstatite chondrites. Other high‐pressure polymorphs were not observed in the vein. The assemblages and chemical compositions of minerals, and the occurrence of coesite indicate that the vein was subjected to the high‐pressure and temperature condition at about 3–10 <jats:styled-content style=\"fixed-case\">GP</jats:styled-content>a and 1000 °C. The host also experienced heating for a short time under lower temperature conditions, from ~700 to ~1000 °C, based on the opaque minerals typical of <jats:styled-content style=\"fixed-case\">EH</jats:styled-content> chondrites and textural features. Although the pressure condition of the vein in this chondrite is much lower than those in the other meteorites, our results suggest that all major meteorite groups contain high‐pressure polymorphs. Heavy shock events commonly took place in the solar system.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380576118714924945","@type":"Researcher","foaf:name":[{"@value":"M. Kimura"}],"jpcoar:affiliationName":[{"@value":"Faculty of Science Ibaraki University Mito 310‐8512 Japan"},{"@value":"National Institute of Polar Research Tokyo 190‐8518 Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380848660728024072","@type":"Researcher","foaf:name":[{"@value":"A. Yamaguchi"}],"jpcoar:affiliationName":[{"@value":"National Institute of Polar Research Tokyo 190‐8518 Japan"},{"@value":"Department of Polar Science School of Multidisciplinary Science SOKENDAI (The Graduate University for Advanced Studies) Tokyo 173‐8518 Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380848660728024064","@type":"Researcher","foaf:name":[{"@value":"M. Miyahara"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Systems Science Graduate School of Science Hiroshima University Higashi‐Hiroshima 739‐8526 Japan"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"10869379"},{"@type":"EISSN","@value":"19455100"}],"prism:publicationName":[{"@value":"Meteoritics & Planetary Science"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"2016-09-26","prism:volume":"52","prism:number":"1","prism:startingPage":"24","prism:endingPage":"35"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fmaps.12738"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/maps.12738"}],"createdAt":"2016-09-26","modifiedAt":"2023-10-02","project":[{"@id":"https://cir.nii.ac.jp/crid/1040000782297954816","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"26400510"},{"@type":"JGN","@value":"JP26400510"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-26400510/"}],"notation":[{"@language":"ja","@value":"隕石及び惑星物質の比較鉱物学"},{"@language":"en","@value":"Comparative mineralogy of meteorites and planetary materials"}]},{"@id":"https://cir.nii.ac.jp/crid/1040000782439947904","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"15H05748"},{"@type":"JGN","@value":"JP15H05748"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-15H05748/"}],"notation":[{"@language":"ja","@value":"地球核の最適モデルの創出"},{"@language":"en","@value":"Creation of the best model of the Earth's core"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257170171008","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"24244088"},{"@type":"JGN","@value":"JP24244088"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-24244088/"}],"notation":[{"@language":"ja","@value":"大気の無い天体表面で何が起きているか：イトカワ試料詳細分析と宇宙風化研究の新展開"},{"@language":"en","@value":"Reaction on the surface of air-less bodies: Detailed analyses of Itokawa grains and new progress of space weathering study"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050291768123568000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"An Almahata Sitta EL3 fragment: Implications for the complex thermal history of enstatite chondrites"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004235936359296","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Curious kinetic behavior in silica polymorphs solves seifertite puzzle in shocked meteorite"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142423893120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The most primitive CM chondrites, Asuka 12085, 12169, and 12236, of subtypes 3.0–2.8: Their characteristic features and classification"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017280630230400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Chondritic breccias: An optical microscopic classification"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182119961856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Shock-induced deformation of Shergottites: Shock-pressures and perturbations of magmatic ages on Mars"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640787589248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The unequilibrated enstatite 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/1360848658217832576","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Posteucritic magmatism on Vesta: Evidence from the petrology and thermal history of diogenites"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848660690645888","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Petrology and Raman spectroscopy of high pressure phases in the Gujba CB chondrite and the shock history of the CB parent body"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848663334856064","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Discovery of stishovite in Apollo 15299 sample"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855569873361280","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Impact features of enstatite-rich meteorites"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570992740224","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The effect of pressure on the eutectic in the system Fe-FeS"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137046101839232","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Formation of high-pressure minerals in shocked L6 chondrite Yamato 791384: constraints on shock conditions and parent body size"}]},{"@id":"https://cir.nii.ac.jp/crid/1361699995738062336","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Majorite-Pyrope + Magnesiowüstite Assemblage: Constraints on the History of Shock Veins in Chondrites"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943780612992","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Shock metamorphism of enstatite chondrites"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544419360387072","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Phase Diagrams of Earth-Forming Minerals"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544421080224640","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"FeO‐rich silicates in the Sahara 97159 (EH3) enstatite chondrite: Mineralogy, oxygen isotopic compositions, and origin"}]},{"@id":"https://cir.nii.ac.jp/crid/1362825896256499840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Discovery of coesite and stishovite in eucrite"}]},{"@id":"https://cir.nii.ac.jp/crid/1363107369135886336","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Formation of feldspathic and metallic melts by shock in enstatite chondrite Reckling Peak A80259"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845242226048","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Partial melting of the Indarch (EH4) meteorite: A textural, chemical, and phase relations view of melting and melt migration"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845337154304","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Abee and related EH chondrite impact-melt breccias"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388845794455424","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The ternary phase diagram, Fe-Ni-P"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388846218393216","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"First discovery of stishovite in an iron meteorite"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670321335969408","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Phase Relations in the System Cr-Fe-S"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794536016768","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Petrographic and mineralogical study of new EH melt rocks and a new enstatite chondrite grouplet"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794748979968","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Normal and reverse zoning in niningerite: A novel key parameter to the thermal histories of EH-chondrites"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795147276672","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A comparative study of opaque phases in Qingzhen (EH3) and MacAlpine Hills 88136 (EL3): Representatives of EH and EL parent bodies"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795760039808","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Formation of niningerite by silicate sulfidation in EH3 enstatite chondrites"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233270526654336","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Thermal history of the enstatite chondrites from silica polymorphs"}]},{"@id":"https://cir.nii.ac.jp/crid/1370848660728024064","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Meteorite Newsletter"}]},{"@id":"https://cir.nii.ac.jp/crid/1370861287341368448","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Petrochemical study of the Yamato‐691 enstatite chondrite (E3). III: Descriptions and mineral compositions of chondrules"}]},{"@id":"https://cir.nii.ac.jp/crid/1370861287341368449","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Coesite and stishovite in a shocked lunar meteorite, Asuka‐881757, and impact events in lunar surface"}]},{"@id":"https://cir.nii.ac.jp/crid/1390572174850021120","@type":"Article","resourceType":"紀要論文(departmental bulletin paper)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Qingzhen and Yamato-691: A tentative alphabet for the EH chondrites"},{"@value":"Qingzhen and Yamato‐691: A tentative alphabet for the EH chondrites"}]},{"@id":"https://cir.nii.ac.jp/crid/1570854174663873408","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Solid solutions of the type(Ca, Mg, Mn, Fe)S and their use as geothermometers for the enstatite chondrites"},{"@value":"Solid solutions of the type (Ca, Mg, Mn, Fe)S and their use as geothermometer for the enstatite chondrites"}]},{"@id":"https://cir.nii.ac.jp/crid/1573668924359550080","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Petrological and mineralogical study of enstatite chondrites with reference to their thermal histories."}]},{"@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":"10.1111/maps.12738"},{"@type":"KAKEN","@value":"PRODUCT-21068967"},{"@type":"KAKEN","@value":"PRODUCT-20763869"},{"@type":"KAKEN","@value":"PRODUCT-20792541"},{"@type":"OPENAIRE","@value":"doi_dedup___::82b343cd35ea92371eb41f576ae742b3"},{"@type":"CROSSREF","@value":"10.1016/j.polar.2020.100565_references_DOI_Y20rt2Rf5Gi7LSUdDzfqTTSay5U"},{"@type":"CROSSREF","@value":"10.1016/j.polar.2022.100847_references_DOI_Y20rt2Rf5Gi7LSUdDzfqTTSay5U"},{"@type":"CROSSREF","@value":"10.1186/s40645-021-00447-2_references_DOI_Y20rt2Rf5Gi7LSUdDzfqTTSay5U"},{"@type":"CROSSREF","@value":"10.1111/maps.12902_references_DOI_Y20rt2Rf5Gi7LSUdDzfqTTSay5U"},{"@type":"CROSSREF","@value":"10.1186/s40645-021-00451-6_references_DOI_Y20rt2Rf5Gi7LSUdDzfqTTSay5U"}]}