Caracterização cristaloquímica, mineralógica e gemológica do berilo do pegmatito mendonça, Distrito de Berilândia, Quixeramobim/CE.

Detalhes bibliográficos
Ano de defesa: 2017
Autor(a) principal: Cavalcanti, Débora Ezequiel
Orientador(a): Nogueira Neto, José de Araújo
Banca de defesa: Não Informado pela instituição
Tipo de documento: Dissertação
Tipo de acesso: Acesso aberto
Idioma: por
Instituição de defesa: Não Informado pela instituição
Programa de Pós-Graduação: Não Informado pela instituição
Departamento: Não Informado pela instituição
País: Não Informado pela instituição
Palavras-chave em Português:
Link de acesso: http://www.repositorio.ufc.br/handle/riufc/26695
Resumo: Beryl samples from Mendonça pegmatite, located in the district of Berilândia, Quixeramobim-CE, were analyzed. This pegmatite belonging to the Pegmatitic District of Solonópole-Banabuiú (DPSB), is located in the center-west portion of the State of Ceará, and embedded in the paragneiss basement of the Borborema Province, Ceará Central Domain. It is a pegmatite type mixed, differentiated, complexed, little fertile and its mineralogy presents industrial and gem minerals composition variety, among which, aquamarine, a variety of the beryl group that occurs in blue and green colors, is the focus of this work. The highest concentrations of industrial beryl occur forming pockets. The aquamarine does not occur forming isolated crystals, but rather as dispersed cores and included in the crystals of industrial beryl. A crystallochemical, mineralogical and gemological characterization of blue and green beryls was carried out, where their intrinsic characteristics were analyzed, from the most basic, such as physical properties, to more advanced ones, such as crystalline structure, unit cell parameters, fluid components (H2O types I II and III, CO2, CH4), chromophores elements/ color causes, chemical composition, as well as the presence and nature of impurities, and substitutions in its structure. The methodology used in its characterization was refractometer, hydrostatic balance, optical and gemological microscopes, single-crystal and powder x-ray diffraction (DRX), micro energy dispersive x-ray fluorescence (EDXRF), molecular absorption spectroscopy in the infrared region by Fourier transform (FTIR), Molecular absorption spectroscopy in the ultraviolet-visible-near infrared region (UV-Vis-NIR) and raman spectroscopy. According to the substitutions in its crystalline structure, it was possible to verify the presence of fluid components of H2O type I, II, III and CO2, and the data necessary to determine the polytypes of beryl. Bands attributed to chromophores as well as their ionic charge and positions were also demonstrated. In the chemical compositional analysis, alkaline elements such as Cs, Rb and Na were detected in the channels. The presence of iron as a chromophore element in the beryl structure, resulting in its blue coloration, allows us to call blue beryl samples of aquamarines, even if they do not present an ideal gemological quality for market standards.
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spelling Cavalcanti, Débora EzequielMattos, Irani ClezarNogueira Neto, José de Araújo2017-10-18T15:52:22Z2017-10-18T15:52:22Z2017CAVALCANTI, Débora Ezequiel. Caracterização cristaloquímica, mineralógica e gemológica do berilo do pegmatito mendonça, Distrito de Berilândia, Quixeramobim/CE. 2017. 134 f. Dissertação (Dissertação em Geologia) - Universidade Federal do Ceará, Fortaleza, 2017.http://www.repositorio.ufc.br/handle/riufc/26695Beryl samples from Mendonça pegmatite, located in the district of Berilândia, Quixeramobim-CE, were analyzed. This pegmatite belonging to the Pegmatitic District of Solonópole-Banabuiú (DPSB), is located in the center-west portion of the State of Ceará, and embedded in the paragneiss basement of the Borborema Province, Ceará Central Domain. It is a pegmatite type mixed, differentiated, complexed, little fertile and its mineralogy presents industrial and gem minerals composition variety, among which, aquamarine, a variety of the beryl group that occurs in blue and green colors, is the focus of this work. The highest concentrations of industrial beryl occur forming pockets. The aquamarine does not occur forming isolated crystals, but rather as dispersed cores and included in the crystals of industrial beryl. A crystallochemical, mineralogical and gemological characterization of blue and green beryls was carried out, where their intrinsic characteristics were analyzed, from the most basic, such as physical properties, to more advanced ones, such as crystalline structure, unit cell parameters, fluid components (H2O types I II and III, CO2, CH4), chromophores elements/ color causes, chemical composition, as well as the presence and nature of impurities, and substitutions in its structure. The methodology used in its characterization was refractometer, hydrostatic balance, optical and gemological microscopes, single-crystal and powder x-ray diffraction (DRX), micro energy dispersive x-ray fluorescence (EDXRF), molecular absorption spectroscopy in the infrared region by Fourier transform (FTIR), Molecular absorption spectroscopy in the ultraviolet-visible-near infrared region (UV-Vis-NIR) and raman spectroscopy. According to the substitutions in its crystalline structure, it was possible to verify the presence of fluid components of H2O type I, II, III and CO2, and the data necessary to determine the polytypes of beryl. Bands attributed to chromophores as well as their ionic charge and positions were also demonstrated. In the chemical compositional analysis, alkaline elements such as Cs, Rb and Na were detected in the channels. The presence of iron as a chromophore element in the beryl structure, resulting in its blue coloration, allows us to call blue beryl samples of aquamarines, even if they do not present an ideal gemological quality for market standards.Foram analisadas amostras de berilo, oriundas do Pegmatito Mendonça, localizado no distrito de Berilândia, município de Quixeramobim-CE. Esse pegmatito pertencente ao Distrito Pegmatítico de Solonópole-Banabuiú (DPSB) e está localizado na porção centro-oeste do Estado do Ceará, encaixado no embasamento paragnáissico da Província Borborema, Domínio Ceará Central. É um pegmatito do tipo misto, diferenciado, complexo, pouco fértil, apresentando em sua composição mineralógica minerais industriais e minerais gema, dentre os quais, a água-marinha, uma variedade do grupo do berilo, que ocorre nas cores azul e verde e que é foco do presente trabalho. As maiores concentrações do berilo industrial ocorrem formando bolsões. A água-marinha não ocorre formando cristais isolados, mas sim como núcleos dispersos e inclusos nos cristais de berilo industrial. Foi realizada uma caracterização cristaloquímica, mineralógica e gemológica dos berilos azuis e verdes, onde foram analisadas suas características intrínsecas, desde as mais básicas, como propriedades físicas, até as mais avançadas, como estrutura cristalina, parâmetros de cela unitária, componentes fluidos (H2O tipos I II e III, CO2, CH4), elementos cromóforos/causas de cor, composição química, bem como presença e natureza de impurezas e substituições na sua estrutura. A metodologia utilizada na sua caracterização foi refratômetro, balança hidrostática, microscópios óptico e gemológico, difração de raios-X (DRX) pelos métodos do pó e monocristal, micro fluorescência de raios-X por energia dispersiva (micro-EDXRF), espectroscopia de absorção molecular na região do infravermelho, por transformada de Fourier (FTIR), espectroscopia de absorção molecular na região ultravioleta-visível-infravermelho proximal (UV-Vis-NIR) e espectroscopia raman. Foi evidenciada a presença dos componentes fluidos H2O tipos I, II e III e CO2, bem como foram fornecidos dados para determinação dos politipos de berilo, segundo suas substituições na estrutura cristalina. Bandas atribuídas aos elementos cromóforos, bem como sua carga iônica e posição na estrutura cristalina também foram demonstradas. Na análise da composição química dos berilos foram detectados elementos alcalinos tais como Cs, Rb e Na nos canais. A presença de ferro como elemento cromóforo na estrutura do berilo, resultando na sua coloração azul, permite-nos chamar as amostras de berilo azul de águas-marinhas, mesmo que essas não apresentem uma qualidade gemológica ideal para os padrões mercadológicos.BeriloÁgua-marinhaCristaloquímicaCaracterização cristaloquímica, mineralógica e gemológica do berilo do pegmatito mendonça, Distrito de Berilândia, Quixeramobim/CE.Crystallochemical, mineralogical and gemological characterization of the beryl of the pegmatite mendonça, Berilândia District, Quixeramobim /Ce.info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/masterThesisporreponame:Repositório Institucional da Universidade Federal do Ceará (UFC)instname:Universidade Federal do Ceará (UFC)instacron:UFCinfo:eu-repo/semantics/openAccessLICENSElicense.txtlicense.txttext/plain; charset=utf-81748http://repositorio.ufc.br/bitstream/riufc/26695/2/license.txt8a4605be74aa9ea9d79846c1fba20a33MD52ORIGINAL2017_dis_decavalcanti.pdf2017_dis_decavalcanti.pdfapplication/pdf8974915http://repositorio.ufc.br/bitstream/riufc/26695/3/2017_dis_decavalcanti.pdf72816be50e8bae5713754402ec93081aMD53riufc/266952019-10-03 10:16:39.543oai:repositorio.ufc.br:riufc/26695Tk9URTogUExBQ0UgWU9VUiBPV04gTElDRU5TRSBIRVJFClRoaXMgc2FtcGxlIGxpY2Vuc2UgaXMgcHJvdmlkZWQgZm9yIGluZm9ybWF0aW9uYWwgcHVycG9zZXMgb25seS4KCk5PTi1FWENMVVNJVkUgRElTVFJJQlVUSU9OIExJQ0VOU0UKCkJ5IHNpZ25pbmcgYW5kIHN1Ym1pdHRpbmcgdGhpcyBsaWNlbnNlLCB5b3UgKHRoZSBhdXRob3Iocykgb3IgY29weXJpZ2h0Cm93bmVyKSBncmFudHMgdG8gRFNwYWNlIFVuaXZlcnNpdHkgKERTVSkgdGhlIG5vbi1leGNsdXNpdmUgcmlnaHQgdG8gcmVwcm9kdWNlLAp0cmFuc2xhdGUgKGFzIGRlZmluZWQgYmVsb3cpLCBhbmQvb3IgZGlzdHJpYnV0ZSB5b3VyIHN1Ym1pc3Npb24gKGluY2x1ZGluZwp0aGUgYWJzdHJhY3QpIHdvcmxkd2lkZSBpbiBwcmludCBhbmQgZWxlY3Ryb25pYyBmb3JtYXQgYW5kIGluIGFueSBtZWRpdW0sCmluY2x1ZGluZyBidXQgbm90IGxpbWl0ZWQgdG8gYXVkaW8gb3IgdmlkZW8uCgpZb3UgYWdyZWUgdGhhdCBEU1UgbWF5LCB3aXRob3V0IGNoYW5naW5nIHRoZSBjb250ZW50LCB0cmFuc2xhdGUgdGhlCnN1Ym1pc3Npb24gdG8gYW55IG1lZGl1bSBvciBmb3JtYXQgZm9yIHRoZSBwdXJwb3NlIG9mIHByZXNlcnZhdGlvbi4KCllvdSBhbHNvIGFncmVlIHRoYXQgRFNVIG1heSBrZWVwIG1vcmUgdGhhbiBvbmUgY29weSBvZiB0aGlzIHN1Ym1pc3Npb24gZm9yCnB1cnBvc2VzIG9mIHNlY3VyaXR5LCBiYWNrLXVwIGFuZCBwcmVzZXJ2YXRpb24uCgpZb3UgcmVwcmVzZW50IHRoYXQgdGhlIHN1Ym1pc3Npb24gaXMgeW91ciBvcmlnaW5hbCB3b3JrLCBhbmQgdGhhdCB5b3UgaGF2ZQp0aGUgcmlnaHQgdG8gZ3JhbnQgdGhlIHJpZ2h0cyBjb250YWluZWQgaW4gdGhpcyBsaWNlbnNlLiBZb3UgYWxzbyByZXByZXNlbnQKdGhhdCB5b3VyIHN1Ym1pc3Npb24gZG9lcyBub3QsIHRvIHRoZSBiZXN0IG9mIHlvdXIga25vd2xlZGdlLCBpbmZyaW5nZSB1cG9uCmFueW9uZSdzIGNvcHlyaWdodC4KCklmIHRoZSBzdWJtaXNzaW9uIGNvbnRhaW5zIG1hdGVyaWFsIGZvciB3aGljaCB5b3UgZG8gbm90IGhvbGQgY29weXJpZ2h0LAp5b3UgcmVwcmVzZW50IHRoYXQgeW91IGhhdmUgb2J0YWluZWQgdGhlIHVucmVzdHJpY3RlZCBwZXJtaXNzaW9uIG9mIHRoZQpjb3B5cmlnaHQgb3duZXIgdG8gZ3JhbnQgRFNVIHRoZSByaWdodHMgcmVxdWlyZWQgYnkgdGhpcyBsaWNlbnNlLCBhbmQgdGhhdApzdWNoIHRoaXJkLXBhcnR5IG93bmVkIG1hdGVyaWFsIGlzIGNsZWFybHkgaWRlbnRpZmllZCBhbmQgYWNrbm93bGVkZ2VkCndpdGhpbiB0aGUgdGV4dCBvciBjb250ZW50IG9mIHRoZSBzdWJtaXNzaW9uLgoKSUYgVEhFIFNVQk1JU1NJT04gSVMgQkFTRUQgVVBPTiBXT1JLIFRIQVQgSEFTIEJFRU4gU1BPTlNPUkVEIE9SIFNVUFBPUlRFRApCWSBBTiBBR0VOQ1kgT1IgT1JHQU5JWkFUSU9OIE9USEVSIFRIQU4gRFNVLCBZT1UgUkVQUkVTRU5UIFRIQVQgWU9VIEhBVkUKRlVMRklMTEVEIEFOWSBSSUdIVCBPRiBSRVZJRVcgT1IgT1RIRVIgT0JMSUdBVElPTlMgUkVRVUlSRUQgQlkgU1VDSApDT05UUkFDVCBPUiBBR1JFRU1FTlQuCgpEU1Ugd2lsbCBjbGVhcmx5IGlkZW50aWZ5IHlvdXIgbmFtZShzKSBhcyB0aGUgYXV0aG9yKHMpIG9yIG93bmVyKHMpIG9mIHRoZQpzdWJtaXNzaW9uLCBhbmQgd2lsbCBub3QgbWFrZSBhbnkgYWx0ZXJhdGlvbiwgb3RoZXIgdGhhbiBhcyBhbGxvd2VkIGJ5IHRoaXMKbGljZW5zZSwgdG8geW91ciBzdWJtaXNzaW9uLgo=Repositório InstitucionalPUBhttp://www.repositorio.ufc.br/ri-oai/requestbu@ufc.br || repositorio@ufc.bropendoar:2019-10-03T13:16:39Repositório Institucional da Universidade Federal do Ceará (UFC) - Universidade Federal do Ceará (UFC)false
dc.title.pt_BR.fl_str_mv Caracterização cristaloquímica, mineralógica e gemológica do berilo do pegmatito mendonça, Distrito de Berilândia, Quixeramobim/CE.
dc.title.en.pt_BR.fl_str_mv Crystallochemical, mineralogical and gemological characterization of the beryl of the pegmatite mendonça, Berilândia District, Quixeramobim /Ce.
title Caracterização cristaloquímica, mineralógica e gemológica do berilo do pegmatito mendonça, Distrito de Berilândia, Quixeramobim/CE.
spellingShingle Caracterização cristaloquímica, mineralógica e gemológica do berilo do pegmatito mendonça, Distrito de Berilândia, Quixeramobim/CE.
Cavalcanti, Débora Ezequiel
Berilo
Água-marinha
Cristaloquímica
title_short Caracterização cristaloquímica, mineralógica e gemológica do berilo do pegmatito mendonça, Distrito de Berilândia, Quixeramobim/CE.
title_full Caracterização cristaloquímica, mineralógica e gemológica do berilo do pegmatito mendonça, Distrito de Berilândia, Quixeramobim/CE.
title_fullStr Caracterização cristaloquímica, mineralógica e gemológica do berilo do pegmatito mendonça, Distrito de Berilândia, Quixeramobim/CE.
title_full_unstemmed Caracterização cristaloquímica, mineralógica e gemológica do berilo do pegmatito mendonça, Distrito de Berilândia, Quixeramobim/CE.
title_sort Caracterização cristaloquímica, mineralógica e gemológica do berilo do pegmatito mendonça, Distrito de Berilândia, Quixeramobim/CE.
author Cavalcanti, Débora Ezequiel
author_facet Cavalcanti, Débora Ezequiel
author_role author
dc.contributor.co-advisor.none.fl_str_mv Mattos, Irani Clezar
dc.contributor.author.fl_str_mv Cavalcanti, Débora Ezequiel
dc.contributor.advisor1.fl_str_mv Nogueira Neto, José de Araújo
contributor_str_mv Nogueira Neto, José de Araújo
dc.subject.por.fl_str_mv Berilo
Água-marinha
Cristaloquímica
topic Berilo
Água-marinha
Cristaloquímica
description Beryl samples from Mendonça pegmatite, located in the district of Berilândia, Quixeramobim-CE, were analyzed. This pegmatite belonging to the Pegmatitic District of Solonópole-Banabuiú (DPSB), is located in the center-west portion of the State of Ceará, and embedded in the paragneiss basement of the Borborema Province, Ceará Central Domain. It is a pegmatite type mixed, differentiated, complexed, little fertile and its mineralogy presents industrial and gem minerals composition variety, among which, aquamarine, a variety of the beryl group that occurs in blue and green colors, is the focus of this work. The highest concentrations of industrial beryl occur forming pockets. The aquamarine does not occur forming isolated crystals, but rather as dispersed cores and included in the crystals of industrial beryl. A crystallochemical, mineralogical and gemological characterization of blue and green beryls was carried out, where their intrinsic characteristics were analyzed, from the most basic, such as physical properties, to more advanced ones, such as crystalline structure, unit cell parameters, fluid components (H2O types I II and III, CO2, CH4), chromophores elements/ color causes, chemical composition, as well as the presence and nature of impurities, and substitutions in its structure. The methodology used in its characterization was refractometer, hydrostatic balance, optical and gemological microscopes, single-crystal and powder x-ray diffraction (DRX), micro energy dispersive x-ray fluorescence (EDXRF), molecular absorption spectroscopy in the infrared region by Fourier transform (FTIR), Molecular absorption spectroscopy in the ultraviolet-visible-near infrared region (UV-Vis-NIR) and raman spectroscopy. According to the substitutions in its crystalline structure, it was possible to verify the presence of fluid components of H2O type I, II, III and CO2, and the data necessary to determine the polytypes of beryl. Bands attributed to chromophores as well as their ionic charge and positions were also demonstrated. In the chemical compositional analysis, alkaline elements such as Cs, Rb and Na were detected in the channels. The presence of iron as a chromophore element in the beryl structure, resulting in its blue coloration, allows us to call blue beryl samples of aquamarines, even if they do not present an ideal gemological quality for market standards.
publishDate 2017
dc.date.accessioned.fl_str_mv 2017-10-18T15:52:22Z
dc.date.available.fl_str_mv 2017-10-18T15:52:22Z
dc.date.issued.fl_str_mv 2017
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dc.type.driver.fl_str_mv info:eu-repo/semantics/masterThesis
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dc.identifier.citation.fl_str_mv CAVALCANTI, Débora Ezequiel. Caracterização cristaloquímica, mineralógica e gemológica do berilo do pegmatito mendonça, Distrito de Berilândia, Quixeramobim/CE. 2017. 134 f. Dissertação (Dissertação em Geologia) - Universidade Federal do Ceará, Fortaleza, 2017.
dc.identifier.uri.fl_str_mv http://www.repositorio.ufc.br/handle/riufc/26695
identifier_str_mv CAVALCANTI, Débora Ezequiel. Caracterização cristaloquímica, mineralógica e gemológica do berilo do pegmatito mendonça, Distrito de Berilândia, Quixeramobim/CE. 2017. 134 f. Dissertação (Dissertação em Geologia) - Universidade Federal do Ceará, Fortaleza, 2017.
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