O meteorito condrítico Saulo Gomes
| Autor(a) principal: | |
|---|---|
| Data de Publicação: | 2011 |
| Outros Autores: | , , |
| Tipo de documento: | Artigo |
| Idioma: | eng por |
| Título da fonte: | Repositório Institucional da UNESP |
| Texto Completo: | http://www.periodicos.rc.biblioteca.unesp.br/index.php/geociencias/article/view/5536 http://hdl.handle.net/11449/73048 |
Resumo: | This paper aims to present the results of petrographic and lithochemical studies obtained in one of the three artifacts, which fell on the farm Buritis in Buritizal County in August 1967, which were collected and stored until the present by reporter Saulo Gomes. The petrographic analysis showed that the artifact is composed by spherical and irregular chondrules with serial granulometry and size averaging around 1 mm and the largest reaching about 6 mm in diameter. The chondrules are made of olivine, ortho and clinopyroxene, crystallite glass, nickel iron alloy and troillite (kamacite and/or taenite/tetrataenite) and inter chondrules glassy material occurs in association with troillite, nickel and other alloy iron-based compounds. The lithochemical data show excellent correlation with the C chondrite, noting only small differences above or between them. The study made it possible to classify the artifact as type L3 and L4 ordinary chondrite. |
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O meteorito condrítico Saulo GomesThe chondritic meteorite Saulo GomesChemical compositionChondriteChondrulesCity of BuritizalMineralogyPetrographychemical compositionchondritedata setdiametergranulometrylithologymeteoritemineralogypetrographyBrazilThis paper aims to present the results of petrographic and lithochemical studies obtained in one of the three artifacts, which fell on the farm Buritis in Buritizal County in August 1967, which were collected and stored until the present by reporter Saulo Gomes. The petrographic analysis showed that the artifact is composed by spherical and irregular chondrules with serial granulometry and size averaging around 1 mm and the largest reaching about 6 mm in diameter. The chondrules are made of olivine, ortho and clinopyroxene, crystallite glass, nickel iron alloy and troillite (kamacite and/or taenite/tetrataenite) and inter chondrules glassy material occurs in association with troillite, nickel and other alloy iron-based compounds. The lithochemical data show excellent correlation with the C chondrite, noting only small differences above or between them. The study made it possible to classify the artifact as type L3 and L4 ordinary chondrite.O presente texto tem o objetivo de apresentar os resultados petrográficos e litoquímicos obtidos em um dos três artefatos que caíram na fazenda Buritis, município de Buritizal, em agosto de 1967, os quais foram coletados e guardados até a presente data pelo repórter Saulo Gomes. A análise petrográfica mostrou que o artefato é constituído por côndrulos esféricos a irregulares, granulometria serial com média ao redor de 1 mm e o maior valor atingindo cerca de 6 mm de diâmetro. Os côndrulos são constituídos por olivina, orto e clinopiroxênio, vidro com cristalitos, troillita e liga ferro níquel (kamacita e/ou taenita/tetrataenita). Inter côndrulos ocorre material vítreo em associação com troillita, liga ferro níquel e outros compostos a base de ferro. Os dados litoquímicos mostram ótima correlação com o condrito C, observando-se apenas pequenas diferenças. O estudo possibilitou classificar o artefato como condrito ordinário, tipo L3 a L4.Departamento de Petrologia e Metalogenia Instituto de Geociências e Ciências Exatas Universidade Estadual Paulista, UNESP, Campus de Rio Claro. Avenida 24-A, 1515 - Bela Vista, CEP 13506-900. Rio Claro, SPInstituto de Geociências e Ciências Exatas Universidade Estadual Paulista, UNESP, Campus de Rio Claro. Avenida 24-A, 1515 - Bela Vista, CEP 13506-900. Rio Claro, SPInstituto de Geociências e Ciências Exatas Universidade Estadual Paulista,UNESP, Campus de Rio Claro. Avenida 24-A, 1515 - Bela Vista, CEP 13506-900. Rio Claro, SPInstituto de Ciência e Tecnologia Núcleo de Engenharia de Minas Universidade Federal de Alfenas, UNIFAL, Campus Av. de Pocos de Caldas. Rod. Jose Aurelio Vilela, Cidade Universitaria, CEP 37715-400. Pocos de Caldas, MGDepartamento de Petrologia e Metalogenia Instituto de Geociências e Ciências Exatas Universidade Estadual Paulista, UNESP, Campus de Rio Claro. Avenida 24-A, 1515 - Bela Vista, CEP 13506-900. Rio Claro, SPInstituto de Geociências e Ciências Exatas Universidade Estadual Paulista, UNESP, Campus de Rio Claro. Avenida 24-A, 1515 - Bela Vista, CEP 13506-900. Rio Claro, SPInstituto de Geociências e Ciências Exatas Universidade Estadual Paulista,UNESP, Campus de Rio Claro. Avenida 24-A, 1515 - Bela Vista, CEP 13506-900. Rio Claro, SPUniversidade Estadual Paulista (Unesp)Universidade Federal de Alfenas (UNIFAL)Zanardo, Antenor [UNESP]Navarro, Guillermo Rafael Beltram [UNESP]Del Roveri, Carolina [UNESP]Morales, Norberto [UNESP]2014-05-27T11:26:19Z2014-05-27T11:26:19Z2011-12-06info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/article195-205application/pdfhttp://www.periodicos.rc.biblioteca.unesp.br/index.php/geociencias/article/view/5536Geociencias, v. 30, n. 2, p. 195-205, 2011.0101-90821980-900Xhttp://hdl.handle.net/11449/730482-s2.0-825551731082-s2.0-82555173108.pdf689327290017405951365945723478650000-0003-2781-586XScopusreponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPengporGeociências0,230info:eu-repo/semantics/openAccess2023-10-07T06:04:19Zoai:repositorio.unesp.br:11449/73048Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462024-08-05T14:14:41.478742Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false |
| dc.title.none.fl_str_mv |
O meteorito condrítico Saulo Gomes The chondritic meteorite Saulo Gomes |
| title |
O meteorito condrítico Saulo Gomes |
| spellingShingle |
O meteorito condrítico Saulo Gomes Zanardo, Antenor [UNESP] Chemical composition Chondrite Chondrules City of Buritizal Mineralogy Petrography chemical composition chondrite data set diameter granulometry lithology meteorite mineralogy petrography Brazil |
| title_short |
O meteorito condrítico Saulo Gomes |
| title_full |
O meteorito condrítico Saulo Gomes |
| title_fullStr |
O meteorito condrítico Saulo Gomes |
| title_full_unstemmed |
O meteorito condrítico Saulo Gomes |
| title_sort |
O meteorito condrítico Saulo Gomes |
| author |
Zanardo, Antenor [UNESP] |
| author_facet |
Zanardo, Antenor [UNESP] Navarro, Guillermo Rafael Beltram [UNESP] Del Roveri, Carolina [UNESP] Morales, Norberto [UNESP] |
| author_role |
author |
| author2 |
Navarro, Guillermo Rafael Beltram [UNESP] Del Roveri, Carolina [UNESP] Morales, Norberto [UNESP] |
| author2_role |
author author author |
| dc.contributor.none.fl_str_mv |
Universidade Estadual Paulista (Unesp) Universidade Federal de Alfenas (UNIFAL) |
| dc.contributor.author.fl_str_mv |
Zanardo, Antenor [UNESP] Navarro, Guillermo Rafael Beltram [UNESP] Del Roveri, Carolina [UNESP] Morales, Norberto [UNESP] |
| dc.subject.por.fl_str_mv |
Chemical composition Chondrite Chondrules City of Buritizal Mineralogy Petrography chemical composition chondrite data set diameter granulometry lithology meteorite mineralogy petrography Brazil |
| topic |
Chemical composition Chondrite Chondrules City of Buritizal Mineralogy Petrography chemical composition chondrite data set diameter granulometry lithology meteorite mineralogy petrography Brazil |
| description |
This paper aims to present the results of petrographic and lithochemical studies obtained in one of the three artifacts, which fell on the farm Buritis in Buritizal County in August 1967, which were collected and stored until the present by reporter Saulo Gomes. The petrographic analysis showed that the artifact is composed by spherical and irregular chondrules with serial granulometry and size averaging around 1 mm and the largest reaching about 6 mm in diameter. The chondrules are made of olivine, ortho and clinopyroxene, crystallite glass, nickel iron alloy and troillite (kamacite and/or taenite/tetrataenite) and inter chondrules glassy material occurs in association with troillite, nickel and other alloy iron-based compounds. The lithochemical data show excellent correlation with the C chondrite, noting only small differences above or between them. The study made it possible to classify the artifact as type L3 and L4 ordinary chondrite. |
| publishDate |
2011 |
| dc.date.none.fl_str_mv |
2011-12-06 2014-05-27T11:26:19Z 2014-05-27T11:26:19Z |
| dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
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info:eu-repo/semantics/article |
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article |
| status_str |
publishedVersion |
| dc.identifier.uri.fl_str_mv |
http://www.periodicos.rc.biblioteca.unesp.br/index.php/geociencias/article/view/5536 Geociencias, v. 30, n. 2, p. 195-205, 2011. 0101-9082 1980-900X http://hdl.handle.net/11449/73048 2-s2.0-82555173108 2-s2.0-82555173108.pdf 6893272900174059 5136594572347865 0000-0003-2781-586X |
| url |
http://www.periodicos.rc.biblioteca.unesp.br/index.php/geociencias/article/view/5536 http://hdl.handle.net/11449/73048 |
| identifier_str_mv |
Geociencias, v. 30, n. 2, p. 195-205, 2011. 0101-9082 1980-900X 2-s2.0-82555173108 2-s2.0-82555173108.pdf 6893272900174059 5136594572347865 0000-0003-2781-586X |
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eng por |
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eng por |
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Geociências 0,230 |
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info:eu-repo/semantics/openAccess |
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openAccess |
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195-205 application/pdf |
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Scopus reponame:Repositório Institucional da UNESP instname:Universidade Estadual Paulista (UNESP) instacron:UNESP |
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Universidade Estadual Paulista (UNESP) |
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UNESP |
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UNESP |
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Repositório Institucional da UNESP |
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Repositório Institucional da UNESP |
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Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP) |
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1808128335070363648 |