A Técnica de Difração de Elétrons Retro-Espalhados (EBSD) em Microscópio Eletrônico de Varredura (MEV) e sua Aplicação no Estudo de Rochas Deformadas

dc.contributoren-US
dc.contributorpt-BR
dc.creatorMORALES, LUIZ FERNANDO GRAFULHA
dc.creatorHINRICHS, RUTH
dc.creatorFERNANDES, LUÍS ALBERTO D’ÁVILA
dc.date2007-06-30
dc.date.accessioned2018-11-07T21:58:36Z
dc.date.available2018-11-07T21:58:36Z
dc.identifierhttps://seer.ufrgs.br/PesquisasemGeociencias/article/view/19459
dc.identifier10.22456/1807-9806.19459
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/2192271
dc.descriptionThe electron backscattered diffraction technique in the scanning electron microscope (EBSD/SEM) is based on the diffraction of a high-energy electron beam by the crystalline structure of a given material, in all possible directions within the sample. Some of the diffracted electrons escape from the specimen with virtually the same initial energy, interact with a phosphorescent screen and the generated EBSP pattern can be picked up with a low-luminosity charge couple device (CCD) camera. These patterns can be indexed using pre-determined patterns for a large variety of minerals, which allows the determination of complete orientation of each single mineral within an aggregate. In this paper we briefly discuss the physical aspects related to the diffraction of an electron beam by crystalline matter and how the EBSP patterns are generated. We also present a short introduction of the necessary instruments to acquire EBSD data, as well as the calibration procedures, acquisition and indexing software of EBSPs. The pitfalls of the technique and possible error sources are also discussed with examples. Considering the scarce availability of literature on geological sample preparation, the polishing method of silicate-rich rocks for EBSP is described in detail in the last part of this paper.en-US
dc.descriptionThe electron backscattered diffraction technique in the scanning electron microscope (EBSD/SEM) is based on the diffraction of a high-energy electron beam by the crystalline structure of a given material, in all possible directions within the sample. Some of the diffracted electrons escape from the specimen with virtually the same initial energy, interact with a phosphorescent screen and the generated EBSP pattern can be picked up with a low-luminosity charge couple device (CCD) camera. These patterns can be indexed using pre-determined patterns for a large variety of minerals, which allows the determination of complete orientation of each single mineral within an aggregate. In this paper we briefly discuss the physical aspects related to the diffraction of an electron beam by crystalline matter and how the EBSP patterns are generated. We also present a short introduction of the necessary instruments to acquire EBSD data, as well as the calibration procedures, acquisition and indexing software of EBSPs. The pitfalls of the technique and possible error sources are also discussed with examples. Considering the scarce availability of literature on geological sample preparation, the polishing method of silicate-rich rocks for EBSP is described in detail in the last part of this paper.pt-BR
dc.formatapplication/pdf
dc.languagepor
dc.publisherInstituto de Geociências /Universidade Federal do Rio Grande do Sulpt-BR
dc.relationhttps://seer.ufrgs.br/PesquisasemGeociencias/article/view/19459/pdf
dc.sourcePesquisas em Geociências; v. 34, n. 1 (2007): Pesquisas em Geociências; 19-34pt-BR
dc.source1807-9806
dc.source1518-2398
dc.subjecten-US
dc.subjectEBSD; deformed rocks; specimen preparation.en-US
dc.subjectpt-BR
dc.subjectpt-BR
dc.subjectGeociênciaspt-BR
dc.titleThe electron backscaterred diffraction technique -EBSD- in a scanning eletronic microscope and its application in the study of deformed rocksen-US
dc.titleA Técnica de Difração de Elétrons Retro-Espalhados (EBSD) em Microscópio Eletrônico de Varredura (MEV) e sua Aplicação no Estudo de Rochas Deformadaspt-BR
dc.typeArtículos de revistas
dc.typeArtículos de revistas
dc.coveragept-BR
dc.coveragept-BR
dc.coveragept-BR


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