Oriented enstatite inclusions in natural diamond.

Detalhes bibliográficos
Autor(a) principal: Leite, C. R.
Data de Publicação: 1984
Outros Autores: Barelli, N., Sardela, I. A.
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da UNESP
Texto Completo: http://www.minersoc.org/pages/Archive-MM/Volume_48/48-348-459.pdf
http://hdl.handle.net/11449/63653
Resumo: Six 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.
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spelling Oriented enstatite inclusions in natural diamond.Six 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.Universidade Estadual Paulista (Unesp)Leite, C. R.Barelli, N.Sardela, I. A.2014-05-26T22:07:29Z2014-05-26T22:07:29Z1984-01-01info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/article459-461application/pdfhttp://www.minersoc.org/pages/Archive-MM/Volume_48/48-348-459.pdfMineralogical Magazine, v. 48, n. 3, p. 459-461, 1984.0026-461Xhttp://hdl.handle.net/11449/636532-s2.0-00213381152-s2.0-0021338115.pdfScopusreponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPengMineralogical Magazine1.744info:eu-repo/semantics/openAccess2023-10-04T06:05:44Zoai:repositorio.unesp.br:11449/63653Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462023-10-04T06:05:44Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false
dc.title.none.fl_str_mv Oriented enstatite inclusions in natural diamond.
title Oriented enstatite inclusions in natural diamond.
spellingShingle Oriented enstatite inclusions in natural diamond.
Leite, C. R.
title_short Oriented enstatite inclusions in natural diamond.
title_full Oriented enstatite inclusions in natural diamond.
title_fullStr Oriented enstatite inclusions in natural diamond.
title_full_unstemmed Oriented enstatite inclusions in natural diamond.
title_sort Oriented enstatite inclusions in natural diamond.
author Leite, C. R.
author_facet Leite, C. R.
Barelli, N.
Sardela, I. A.
author_role author
author2 Barelli, N.
Sardela, I. A.
author2_role author
author
dc.contributor.none.fl_str_mv Universidade Estadual Paulista (Unesp)
dc.contributor.author.fl_str_mv Leite, C. R.
Barelli, N.
Sardela, I. A.
description Six 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.
publishDate 1984
dc.date.none.fl_str_mv 1984-01-01
2014-05-26T22:07:29Z
2014-05-26T22:07:29Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://www.minersoc.org/pages/Archive-MM/Volume_48/48-348-459.pdf
Mineralogical Magazine, v. 48, n. 3, p. 459-461, 1984.
0026-461X
http://hdl.handle.net/11449/63653
2-s2.0-0021338115
2-s2.0-0021338115.pdf
url http://www.minersoc.org/pages/Archive-MM/Volume_48/48-348-459.pdf
http://hdl.handle.net/11449/63653
identifier_str_mv Mineralogical Magazine, v. 48, n. 3, p. 459-461, 1984.
0026-461X
2-s2.0-0021338115
2-s2.0-0021338115.pdf
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv Mineralogical Magazine
1.744
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv 459-461
application/pdf
dc.source.none.fl_str_mv Scopus
reponame:Repositório Institucional da UNESP
instname:Universidade Estadual Paulista (UNESP)
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instname_str Universidade Estadual Paulista (UNESP)
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reponame_str Repositório Institucional da UNESP
collection Repositório Institucional da UNESP
repository.name.fl_str_mv Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)
repository.mail.fl_str_mv
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