Oriented enstatite inclusions in natural diamond.
dc.contributor.author | Leite, C. R. | |
dc.contributor.author | Barelli, N. | |
dc.contributor.author | Sardela, I. A. | |
dc.contributor.institution | Universidade Estadual Paulista (Unesp) | |
dc.date.accessioned | 2014-05-26T22:07:29Z | |
dc.date.available | 2014-05-26T22:07:29Z | |
dc.date.issued | 1984-01-01 | |
dc.description.abstract | 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. | en |
dc.format.extent | 459-461 | |
dc.identifier | http://www.minersoc.org/pages/Archive-MM/Volume_48/48-348-459.pdf | |
dc.identifier.citation | Mineralogical Magazine, v. 48, n. 3, p. 459-461, 1984. | |
dc.identifier.file | 2-s2.0-0021338115.pdf | |
dc.identifier.issn | 0026-461X | |
dc.identifier.scopus | 2-s2.0-0021338115 | |
dc.identifier.uri | http://hdl.handle.net/11449/63653 | |
dc.language.iso | eng | |
dc.relation.ispartof | Mineralogical Magazine | |
dc.relation.ispartofjcr | 1.744 | |
dc.rights.accessRights | Acesso aberto | |
dc.source | Scopus | |
dc.title | Oriented enstatite inclusions in natural diamond. | en |
dc.type | Artigo | |
dcterms.license | http://www.minersoc.org/open-access.html |
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