{"@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/1361699994598157440.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1111/j.1945-5100.1988.tb00916.x"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1945-5100.1988.tb00916.x"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1945-5100.1988.tb00916.x"}}],"dc:title":[{"@value":"The Tuxtuac, Mexico, Meteorite, an LL5 Chondrite Fall"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p><jats:bold>Abstract—</jats:bold> The Tuxtuac meteorite fell in Zacatecas state, Mexico, on 16 October 1975, at 1820 hours. Two partly crusted masses, weighing 1924 g and 2340 g, were recovered. The stone is an ordinary chondrite, LL5, with olivine Fa<jats:sub>30</jats:sub> and 19.22 weight % total iron. The silicates contain numerous voids and a froth‐like mesostasis is present within some chondrules. Metal phases present are kamacite (5.7–6.4% Ni, 6–7% Co) and high nickel metal (taenite 37–41% Ni, 1.7 ± 0.3% Co; tetrataenite 47–52% Ni, 0.8–1.4% Co). The stone is unusual for an LL‐group chondrite in that it exhibits neither large‐scale brecciation features nor dark veins.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699994598157443","@type":"Researcher","foaf:name":[{"@value":"A. L. Graham"}]},{"@id":"https://cir.nii.ac.jp/crid/1380298342970597888","@type":"Researcher","foaf:name":[{"@value":"M. Christophe Michel‐Levy"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994598157442","@type":"Researcher","foaf:name":[{"@value":"J. Danon"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994598157440","@type":"Researcher","foaf:name":[{"@value":"A. J. Easton"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00261114"}],"prism:publicationName":[{"@value":"Meteoritics"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"1988-12","prism:volume":"23","prism:number":"4","prism:startingPage":"321","prism:endingPage":"323"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1945-5100.1988.tb00916.x"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1945-5100.1988.tb00916.x"}],"createdAt":"2012-06-15","modifiedAt":"2023-10-21","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=General%20Earth%20and%20Planetary%20Sciences","dc:title":"General Earth and Planetary Sciences"},{"@id":"https://cir.nii.ac.jp/all?q=General%20Environmental%20Science","dc:title":"General Environmental Science"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360848657096825216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Nanomorphology of Itokawa regolith particles: Application to space-weathering processes affecting the Itokawa asteroid"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317070230784","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mineralogy of four Itokawa particles collected from the first touchdown site"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1111/j.1945-5100.1988.tb00916.x"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2016.05.011_references_DOI_WvjY1rRncTar8N9O3NOaCpeUBFX"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-124_references_DOI_WvjY1rRncTar8N9O3NOaCpeUBFX"}]}