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Please use this identifier to cite or link to this item: http://acervodigital.unesp.br/handle/11449/63653
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dc.contributor.authorLeite, C. R.-
dc.contributor.authorBarelli, N.-
dc.contributor.authorSardela, I. A.-
dc.date.accessioned2014-05-26T22:07:29Z-
dc.date.accessioned2016-10-25T18:11:48Z-
dc.date.available2014-05-26T22:07:29Z-
dc.date.available2016-10-25T18:11:48Z-
dc.date.issued1984-01-01-
dc.identifierhttp://www.minersoc.org/pages/Archive-MM/Volume_48/48-348-459.pdf-
dc.identifier.citationMineralogical Magazine, v. 48, n. 3, p. 459-461, 1984.-
dc.identifier.issn0026-461X-
dc.identifier.urihttp://hdl.handle.net/11449/63653-
dc.identifier.urihttp://acervodigital.unesp.br/handle/11449/63653-
dc.description.abstractSix crystal inclusions in a twinned diamond from the Tibagi River deposits near Telemaco Borba, Parana State, Brazil, were identified as forsterite (prismatic crystals) and enstatite (tabular crystals, with a 18.17, b 8.81, c 5.17 A). The prismatic forsterite inclusions are oriented along the <110> directions of the host diamond; the main direction of the tabular enstatite crystals is in the same orientation. The identity and orientation of the inclusions were obtained by X-ray precession camera. Enstatite (210) is nearly parallel with the (111) octahedral layer of diamond; a possible epitaxial relationship is discussed.-R.A.H.en
dc.format.extent459-461-
dc.language.isoeng-
dc.sourceScopus-
dc.titleOriented enstatite inclusions in natural diamond.en
dc.typeoutro-
dc.contributor.institutionUniversidade Estadual Paulista (UNESP)-
dc.rights.accessRightsAcesso aberto-
dc.identifier.file2-s2.0-0021338115.pdf-
dc.relation.ispartofMineralogical Magazine-
dc.identifier.scopus2-s2.0-0021338115-
Appears in Collections:Artigos, TCCs, Teses e Dissertações da Unesp

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