{"@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/1360021396512904320.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1180/minmag.2010.074.2.277"}},{"identifier":{"@type":"URI","@value":"https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0026461X00055973"}}],"dc:title":[{"@value":"The crystal structure of Mg end-member lizardite-1<i>T</i> forming polyhedral spheres from the Lizard, Cornwall"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>The crystal structure of lizardite-1<jats:italic>T</jats:italic> from Gew-graze, Cornwall, has been refined by single-crystal X-ray diffraction to <jats:italic>R</jats:italic><jats:sub>1</jats:sub> of 0.0263 and 0.0557, for two crystals having <jats:italic>P</jats:italic>31<jats:italic>m</jats:italic> space group and lattice parameters <jats:italic>a</jats:italic> = 5.2905(5) Å, <jats:italic>c</jats:italic> = 7.2815(8) Å, and <jats:italic>a</jats:italic> = 5.3111(10) Å, <jats:italic>c</jats:italic> = 7.2907(15) Å, respectively. The Gew-graze lizardite is very close to the end-member composition, so these refinements confirm the existence of well crystallized pure Mg-lizardite and show this to be the most weakly H-bonded lizardite ever refined. With regard to its lattice parameters, Si–O bond distances and geometrical parameters controlled by interlayer interactions (i.e. H-bonding), the Gew-graze Mg end-member lizardite yields slight but observable geometrical differences compared with previous refined structures for specifically, aluminous, lizardites.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380021396512904322","@type":"Researcher","foaf:name":[{"@value":"M. Mellini"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021396512904320","@type":"Researcher","foaf:name":[{"@value":"G. Cressey"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021396512904323","@type":"Researcher","foaf:name":[{"@value":"F. J. Wicks"}]},{"@id":"https://cir.nii.ac.jp/crid/1380021396512904321","@type":"Researcher","foaf:name":[{"@value":"B. A. Cressey"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"0026461X"},{"@type":"EISSN","@value":"14718022"}],"prism:publicationName":[{"@value":"Mineralogical Magazine"}],"dc:publisher":[{"@value":"Mineralogical Society"}],"prism:publicationDate":"2010-04","prism:volume":"74","prism:number":"2","prism:startingPage":"277","prism:endingPage":"284"},"reviewed":"false","dc:rights":["https://www.cambridge.org/core/terms"],"url":[{"@id":"https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0026461X00055973"}],"createdAt":"2010-06-08","modifiedAt":"2021-02-04","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360021390747998080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Four‐dimensional‐STEM analysis of the phyllosilicate‐rich matrix of Ryugu samples"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1180/minmag.2010.074.2.277"},{"@type":"CROSSREF","@value":"10.1111/maps.14124_references_DOI_RrxuIjFWNXojuJlJkBcdFb7fIGe"}]}