The influence of the characteristics of quartz and mineral deterioration on the strength of granitic dimensional stones

Detalhes bibliográficos
Autor(a) principal: Sousa, LMO
Data de Publicação: 2013
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://hdl.handle.net/10348/3040
Resumo: It is important to have a thorough knowledge of the petrographic characteristics of rocks to evaluate and understand their mechanical behavior. This paper deals with the influence of the texture and the mineral characteristics of nine Portuguese granites employed as dimensional stones. This study evaluates different mineral characteristics, such as mineral deterioration, grain size, quartz fissuration and the contacts between quartz and others mineral groups. The main differences in the studied granites were identified, clarifying the relationship between the petrographic characteristics. The consequences on their respective mechanical behavior were subsequently evaluated. The physical and textural characteristics of quartz in the studied granites have proven to be very important for understanding the behavior of granitic rocks under compressive stress. Uniaxial compressive strength values are not proportional to the quartz–feldspar ratio or quartz content and there is a tendency for strength to decrease with the increase in quartz. This could be related to the increase in quartz-quartz contacts and the decrease in the rock capacity for accommodating the deformation.
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spelling The influence of the characteristics of quartz and mineral deterioration on the strength of granitic dimensional stonesGranitePetrophysicsMineral deteriorationQuartz fissurationUniaxial compressive strengthIt is important to have a thorough knowledge of the petrographic characteristics of rocks to evaluate and understand their mechanical behavior. This paper deals with the influence of the texture and the mineral characteristics of nine Portuguese granites employed as dimensional stones. This study evaluates different mineral characteristics, such as mineral deterioration, grain size, quartz fissuration and the contacts between quartz and others mineral groups. The main differences in the studied granites were identified, clarifying the relationship between the petrographic characteristics. The consequences on their respective mechanical behavior were subsequently evaluated. The physical and textural characteristics of quartz in the studied granites have proven to be very important for understanding the behavior of granitic rocks under compressive stress. Uniaxial compressive strength values are not proportional to the quartz–feldspar ratio or quartz content and there is a tendency for strength to decrease with the increase in quartz. This could be related to the increase in quartz-quartz contacts and the decrease in the rock capacity for accommodating the deformation.Springer2014-03-26T10:52:19Z2013-06-01T00:00:00Z2013-06info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10348/3040eng1866-6280Sousa, LMOinfo:eu-repo/semantics/embargoedAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2024-02-02T12:49:30Zoai:repositorio.utad.pt:10348/3040Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-20T02:04:52.238637Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse
dc.title.none.fl_str_mv The influence of the characteristics of quartz and mineral deterioration on the strength of granitic dimensional stones
title The influence of the characteristics of quartz and mineral deterioration on the strength of granitic dimensional stones
spellingShingle The influence of the characteristics of quartz and mineral deterioration on the strength of granitic dimensional stones
Sousa, LMO
Granite
Petrophysics
Mineral deterioration
Quartz fissuration
Uniaxial compressive strength
title_short The influence of the characteristics of quartz and mineral deterioration on the strength of granitic dimensional stones
title_full The influence of the characteristics of quartz and mineral deterioration on the strength of granitic dimensional stones
title_fullStr The influence of the characteristics of quartz and mineral deterioration on the strength of granitic dimensional stones
title_full_unstemmed The influence of the characteristics of quartz and mineral deterioration on the strength of granitic dimensional stones
title_sort The influence of the characteristics of quartz and mineral deterioration on the strength of granitic dimensional stones
author Sousa, LMO
author_facet Sousa, LMO
author_role author
dc.contributor.author.fl_str_mv Sousa, LMO
dc.subject.por.fl_str_mv Granite
Petrophysics
Mineral deterioration
Quartz fissuration
Uniaxial compressive strength
topic Granite
Petrophysics
Mineral deterioration
Quartz fissuration
Uniaxial compressive strength
description It is important to have a thorough knowledge of the petrographic characteristics of rocks to evaluate and understand their mechanical behavior. This paper deals with the influence of the texture and the mineral characteristics of nine Portuguese granites employed as dimensional stones. This study evaluates different mineral characteristics, such as mineral deterioration, grain size, quartz fissuration and the contacts between quartz and others mineral groups. The main differences in the studied granites were identified, clarifying the relationship between the petrographic characteristics. The consequences on their respective mechanical behavior were subsequently evaluated. The physical and textural characteristics of quartz in the studied granites have proven to be very important for understanding the behavior of granitic rocks under compressive stress. Uniaxial compressive strength values are not proportional to the quartz–feldspar ratio or quartz content and there is a tendency for strength to decrease with the increase in quartz. This could be related to the increase in quartz-quartz contacts and the decrease in the rock capacity for accommodating the deformation.
publishDate 2013
dc.date.none.fl_str_mv 2013-06-01T00:00:00Z
2013-06
2014-03-26T10:52:19Z
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