Depósitos de alexandrita de Malacacheta, Minas Gerais.
Autor(a) principal: | |
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Data de Publicação: | 2000 |
Outros Autores: | , |
Tipo de documento: | Artigo |
Idioma: | por |
Título da fonte: | Repositório Institucional da UFOP |
Texto Completo: | http://www.repositorio.ufop.br/handle/123456789/8230 https://doi.org/10.18285/geonomos.v8i1.147 |
Resumo: | Since 1975, alexandrite [Be(Al2-xCrx)2O4], the chromium-bearing crysoberyl variety, has been exploited from alluvial and paleo-alluvial deposits in the Malacacheta region. The alluvial deposits consist of resedimented gravel along the present drainage streams. The paleo-alluvial deposits are richer in alexandrite, and show well-developed soil horizons covering the alexandrite-bearing gravel layer. Alexandrite grains show angular shapes with very sharp edges, suggesting transport for short distances. The country rocks are quartz-mica schist and peraluminous mica schist (Salinas Formation), covered by alternating mica schist and quartzite layers (Capelinha Formation). Both formations are of Neoproterozoic age. They host tectonic slabs of metaultramafic rocks, and are cut by intrusive granites of Cambrian age. No alexandrite-bearing rock has been found in the area, probably due to the intense tropical weathering. However, some of the mapped rocks are sources for Be (granites), Cr (metaultramafics) and Al (peraluminous schists), the essential elements for alexandrite crystallization. We suggest a metasomatic system of Cambrian age for alexandrite genesis in the area, involving the interaction of granite-related Be-rich fluids with metaultramafic rocks and peraluminous schists. |
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Basílio, Márcio SilvaSoares, Antônio Carlos PedrosaEvangelista, Hanna Jordt2017-07-13T12:59:05Z2017-07-13T12:59:05Z2000BASÍLIO, M. S.; SOARES, A. C. P.; EVANGELISTA, H. J. Depósitos de alexandrita de Malacacheta, Minas Gerais. Geonomos, Belo Horizonte, v. 8, n.1, p. 47-54, 2000. Disponível em: <https://periodicos.ufmg.br/index.php/revistageonomos/article/view/11581>. Acesso em: 20 de jun. 2017.0104-4486http://www.repositorio.ufop.br/handle/123456789/8230https://doi.org/10.18285/geonomos.v8i1.147Since 1975, alexandrite [Be(Al2-xCrx)2O4], the chromium-bearing crysoberyl variety, has been exploited from alluvial and paleo-alluvial deposits in the Malacacheta region. The alluvial deposits consist of resedimented gravel along the present drainage streams. The paleo-alluvial deposits are richer in alexandrite, and show well-developed soil horizons covering the alexandrite-bearing gravel layer. Alexandrite grains show angular shapes with very sharp edges, suggesting transport for short distances. The country rocks are quartz-mica schist and peraluminous mica schist (Salinas Formation), covered by alternating mica schist and quartzite layers (Capelinha Formation). Both formations are of Neoproterozoic age. They host tectonic slabs of metaultramafic rocks, and are cut by intrusive granites of Cambrian age. No alexandrite-bearing rock has been found in the area, probably due to the intense tropical weathering. However, some of the mapped rocks are sources for Be (granites), Cr (metaultramafics) and Al (peraluminous schists), the essential elements for alexandrite crystallization. We suggest a metasomatic system of Cambrian age for alexandrite genesis in the area, involving the interaction of granite-related Be-rich fluids with metaultramafic rocks and peraluminous schists.Os direitos autorais dos trabalhos publicados na Geonomos são do autor, com direitos de primeira publicação para a revista. Fonte: Geonomos <https://periodicos.ufmg.br/index.php/revistageonomos/about/submissions>. Acesso em: 24 set. 2019.info:eu-repo/semantics/openAccessDepósitos de alexandrita de Malacacheta, Minas Gerais.info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleporreponame:Repositório Institucional da UFOPinstname:Universidade Federal de Ouro Preto (UFOP)instacron:UFOPLICENSElicense.txtlicense.txttext/plain; charset=utf-8924http://www.repositorio.ufop.br/bitstream/123456789/8230/2/license.txt62604f8d955274beb56c80ce1ee5dcaeMD52ORIGINALARTIGO_DepósitosAlexandritaMalacacheta.pdfARTIGO_DepósitosAlexandritaMalacacheta.pdfapplication/pdf359329http://www.repositorio.ufop.br/bitstream/123456789/8230/1/ARTIGO_Dep%c3%b3sitosAlexandritaMalacacheta.pdf023ad64a1ffb3a588747a69245c5ff9bMD51123456789/82302019-12-13 11:34:30.008oai:localhost:123456789/8230RGVjbGFyYcOnw6NvIGRlIGRpc3RyaWJ1acOnw6NvIG7Do28tZXhjbHVzaXZhCgpPIHJlZmVyaWRvIGF1dG9yOgoKYSlEZWNsYXJhIHF1ZSBvIGRvY3VtZW50byBlbnRyZWd1ZSDDqSBzZXUgdHJhYmFsaG8gb3JpZ2luYWwgZSBxdWUgZGV0w6ltIG8gZGlyZWl0byBkZSBjb25jZWRlciBvcyBkaXJlaXRvcyBjb250aWRvcyBuZXN0YSBsaWNlbsOnYS4gRGVjbGFyYSB0YW1iw6ltIHF1ZSBhIGVudHJlZ2EgZG8gZG9jdW1lbnRvIG7Do28gaW5mcmluZ2UsIHRhbnRvIHF1YW50byBsaGUgw6kgcG9zc8OtdmVsIHNhYmVyLCBvcyBkaXJlaXRvcyBkZSBxdWFscXVlciBwZXNzb2Egb3UgZW50aWRhZGUuCgpiKVNlIG8gZG9jdW1lbnRvIGVudHJlZ3VlIGNvbnTDqW0gbWF0ZXJpYWwgZG8gcXVhbCBuw6NvIGRldMOpbSBvcyBkaXJlaXRvcyBkZSBhdXRvciwgZGVjbGFyYSBxdWUgb2J0ZXZlIGF1dG9yaXphw6fDo28gZG8gZGV0ZW50b3IgZG9zIGRpcmVpdG9zIGRlIGF1dG9yIHBhcmEgY29uY2VkZXIgw6AgVW5pdmVyc2lkYWRlIEZlZGVyYWwgZGUgT3VybyBQcmV0by9VRk9QIG9zIGRpcmVpdG9zIHJlcXVlcmlkb3MgcG9yIGVzdGEgbGljZW7Dp2EgZSBxdWUgZXNzZSBtYXRlcmlhbCwgY3Vqb3MgZGlyZWl0b3Mgc8OjbyBkZSB0ZXJjZWlyb3MsIGVzdMOhIGNsYXJhbWVudGUgaWRlbnRpZmljYWRvIGUgcmVjb25oZWNpZG8gbm8gdGV4dG8gb3UgY29udGXDumRvcyBkbyBkb2N1bWVudG8gZW50cmVndWUuCgpjKVNlIG8gZG9jdW1lbnRvIGVudHJlZ3VlIMOpIGJhc2VhZG8gZW0gdHJhYmFsaG8gZmluYW5jaWFkbyBvdSBhcG9pYWRvIHBvciBvdXRyYSBpbnN0aXR1acOnw6NvIHF1ZSBuw6NvIGEgVUZPUCwgZGVjbGFyYSBxdWUgY3VtcHJpdSBxdWFpc3F1ZXIgb2JyaWdhw6fDtWVzIGV4aWdpZGFzIHBlbG8gY29udHJhdG8gb3UgYWNvcmRvLgoKRepositório InstitucionalPUBhttp://www.repositorio.ufop.br/oai/requestrepositorio@ufop.edu.bropendoar:32332019-12-13T16:34:30Repositório Institucional da UFOP - Universidade Federal de Ouro Preto (UFOP)false |
dc.title.pt_BR.fl_str_mv |
Depósitos de alexandrita de Malacacheta, Minas Gerais. |
title |
Depósitos de alexandrita de Malacacheta, Minas Gerais. |
spellingShingle |
Depósitos de alexandrita de Malacacheta, Minas Gerais. Basílio, Márcio Silva |
title_short |
Depósitos de alexandrita de Malacacheta, Minas Gerais. |
title_full |
Depósitos de alexandrita de Malacacheta, Minas Gerais. |
title_fullStr |
Depósitos de alexandrita de Malacacheta, Minas Gerais. |
title_full_unstemmed |
Depósitos de alexandrita de Malacacheta, Minas Gerais. |
title_sort |
Depósitos de alexandrita de Malacacheta, Minas Gerais. |
author |
Basílio, Márcio Silva |
author_facet |
Basílio, Márcio Silva Soares, Antônio Carlos Pedrosa Evangelista, Hanna Jordt |
author_role |
author |
author2 |
Soares, Antônio Carlos Pedrosa Evangelista, Hanna Jordt |
author2_role |
author author |
dc.contributor.author.fl_str_mv |
Basílio, Márcio Silva Soares, Antônio Carlos Pedrosa Evangelista, Hanna Jordt |
description |
Since 1975, alexandrite [Be(Al2-xCrx)2O4], the chromium-bearing crysoberyl variety, has been exploited from alluvial and paleo-alluvial deposits in the Malacacheta region. The alluvial deposits consist of resedimented gravel along the present drainage streams. The paleo-alluvial deposits are richer in alexandrite, and show well-developed soil horizons covering the alexandrite-bearing gravel layer. Alexandrite grains show angular shapes with very sharp edges, suggesting transport for short distances. The country rocks are quartz-mica schist and peraluminous mica schist (Salinas Formation), covered by alternating mica schist and quartzite layers (Capelinha Formation). Both formations are of Neoproterozoic age. They host tectonic slabs of metaultramafic rocks, and are cut by intrusive granites of Cambrian age. No alexandrite-bearing rock has been found in the area, probably due to the intense tropical weathering. However, some of the mapped rocks are sources for Be (granites), Cr (metaultramafics) and Al (peraluminous schists), the essential elements for alexandrite crystallization. We suggest a metasomatic system of Cambrian age for alexandrite genesis in the area, involving the interaction of granite-related Be-rich fluids with metaultramafic rocks and peraluminous schists. |
publishDate |
2000 |
dc.date.issued.fl_str_mv |
2000 |
dc.date.accessioned.fl_str_mv |
2017-07-13T12:59:05Z |
dc.date.available.fl_str_mv |
2017-07-13T12:59:05Z |
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info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
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format |
article |
status_str |
publishedVersion |
dc.identifier.citation.fl_str_mv |
BASÍLIO, M. S.; SOARES, A. C. P.; EVANGELISTA, H. J. Depósitos de alexandrita de Malacacheta, Minas Gerais. Geonomos, Belo Horizonte, v. 8, n.1, p. 47-54, 2000. Disponível em: <https://periodicos.ufmg.br/index.php/revistageonomos/article/view/11581>. Acesso em: 20 de jun. 2017. |
dc.identifier.uri.fl_str_mv |
http://www.repositorio.ufop.br/handle/123456789/8230 |
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0104-4486 |
dc.identifier.doi.none.fl_str_mv |
https://doi.org/10.18285/geonomos.v8i1.147 |
identifier_str_mv |
BASÍLIO, M. S.; SOARES, A. C. P.; EVANGELISTA, H. J. Depósitos de alexandrita de Malacacheta, Minas Gerais. Geonomos, Belo Horizonte, v. 8, n.1, p. 47-54, 2000. Disponível em: <https://periodicos.ufmg.br/index.php/revistageonomos/article/view/11581>. Acesso em: 20 de jun. 2017. 0104-4486 |
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http://www.repositorio.ufop.br/handle/123456789/8230 https://doi.org/10.18285/geonomos.v8i1.147 |
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