LiInSiO4: a new monovalent-trivalent olivine.
Identifieur interne : 003280 ( Main/Exploration ); précédent : 003279; suivant : 003281LiInSiO4: a new monovalent-trivalent olivine.
Auteurs : RBID : pubmed:12743383Abstract
The structure of the olivine LiInSiO(4) (lithium indium silicate) is isotypic with LiScSiO(4) and MgMgSiO(4) (forsterite). The main differences between the title compound and the divalent-divalent olivines are found for the bond lengths and angles opposite common edges between the tetrahedron and the Li(+) and In(3+) ion sites. The tetrahedron shares one common edge with the Li(+) site and two common edges with the In(3+) site. The tetrahedron is distinctly distorted, as are the Li(+) and In(3+) sites.
PubMed: 12743383
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<author><name sortKey="Redhammer, G J" uniqKey="Redhammer G">G J Redhammer</name>
<affiliation wicri:level="3"><nlm:affiliation>Institute for Crystallography, Rheinisch-Wesfälisch Technische Hochschule Aachen, Jägerstrasse 17/19, D-52056 Aachen, Germany. guenther.redhammer@aon.at</nlm:affiliation>
<country xml:lang="fr">Allemagne</country>
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<author><name sortKey="Roth, G" uniqKey="Roth G">G Roth</name>
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<front><div type="abstract" xml:lang="en">The structure of the olivine LiInSiO(4) (lithium indium silicate) is isotypic with LiScSiO(4) and MgMgSiO(4) (forsterite). The main differences between the title compound and the divalent-divalent olivines are found for the bond lengths and angles opposite common edges between the tetrahedron and the Li(+) and In(3+) ion sites. The tetrahedron shares one common edge with the Li(+) site and two common edges with the In(3+) site. The tetrahedron is distinctly distorted, as are the Li(+) and In(3+) sites.</div>
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<Title>Acta crystallographica. Section C, Crystal structure communications</Title>
<ISOAbbreviation>Acta Crystallogr C</ISOAbbreviation>
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<ArticleTitle>LiInSiO4: a new monovalent-trivalent olivine.</ArticleTitle>
<Pagination><MedlinePgn>i38-40</MedlinePgn>
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<Abstract><AbstractText>The structure of the olivine LiInSiO(4) (lithium indium silicate) is isotypic with LiScSiO(4) and MgMgSiO(4) (forsterite). The main differences between the title compound and the divalent-divalent olivines are found for the bond lengths and angles opposite common edges between the tetrahedron and the Li(+) and In(3+) ion sites. The tetrahedron shares one common edge with the Li(+) site and two common edges with the In(3+) site. The tetrahedron is distinctly distorted, as are the Li(+) and In(3+) sites.</AbstractText>
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