Condicionantes morfoestruturais na evolução da paisagem no oeste do Paraná e suas interações com os latossolos vermelhos
Autor(a) principal: | |
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Data de Publicação: | 2021 |
Tipo de documento: | Tese |
Idioma: | por |
Título da fonte: | Biblioteca Digital de Teses e Dissertações do UNIOESTE |
Texto Completo: | https://tede.unioeste.br/handle/tede/5926 |
Resumo: | The evolution dynamic of the landscapes of the Basalt Plateau of the Paraná Sedimentary Basin remain little understood, especially regarding the influence of lithostructural, tectonic, and pedogeomorphic interaction. The hypotheses of this thesis propose that lithostructural factors acted in the differential control of relief dissection, as tectonic pulses interrupted the stability of the landscape during the Cenozoic. In addition, the evolution of the Ferralsols would be conditioned to this dynamic that contributed to the input of allochtonous parent material to the Ferralsols on more recent sectors of the landscape. Therefore, this thesis investigates the factors that acted on the elaboration of the relief and its forms, and on the genesis and evolution of Ferralsols found on the landscape of West Paraná, having the hydrographic basins of the São Francisco Verdadeiro and São Francisco Falso Rivers, left-hand tributaries of the Paraná River, as spatial outline. The methodology was based on the attainment of data in the field, office, and laboratory. In the field, a survey of tectonic structures was carried out, in addition to differentiation of the lithological members, identification of geomorphic surfaces, soil description and sample collection from six Ferralsols profiles for subsequent investigation of their physical, chemical, mineralogical, geochemical, and macro-micromorphological attributes. In the office, the structural data served as a basis for the elaboration of stereograms and for the analysis of paleostress. Cartographic products of the geology (lithostructure and faults), modelled types, elevation, knickpoint density, relief rugosity, swath profiles, and the spatialization of geomorphic surfaces were also elaborated. Morphometric techniques related to the longitudinal profile of the rivers, slope-length index, and basin asymmetry factor were used to demonstrate the tecto-lithostructural control on the geomorphic configuration of the studied river basins. In the laboratory, the physical, chemical, mineralogical, geochemical, and micromorphological attributes of the Ferralsols were investigated. From the statistical evaluation of Principal Components Analysis, it was possible to differentiate the Ferralsols into two main groups, while the macro and micromorphology indicated important evidence of allochtony in profiles P.1, P.3, and P.6. In general, the results enable identification of the lithostructural variations between the lithological members of the Serra Geral Group that outcrop in the study area, these being composed of massive tabular flood basalts and vesicular compounds, which controlled the uneven dissection of the relief, as well as the occurrence of strike-slip faults, mainly NW-SE and NE-SW, which directed the sculpting of the relief forms and the elaboration of the geomorphic surfaces. Two tectonic pulses were recorded that reactivated the transcurrent faults (NE-SW, NW-SE, N-S and E-W) and dismantled the pre-Neogene, geomorphic surface S1, and contributed to the elaboration of surfaces S4 and S5, during the Quartenary. These pulses appear to have been decisive for interrupting the evolution of the Ferralsols and partially removing the most varied weathering profiles, generating allochtonous material for the transitional (P.3) and more subsided sectors of the landscape (P.1 and P.6), where less weathered Ferralsols developed. It has been demonstrated that, in addition to climatic influence, there was an overlap of lithostructural and tectonic controls on the evolution of the regional landscape, which triggered important geomorphic processes of base level change, processes of etching/stripping, and slope retreat in the studied basins. Furthermore, the results enable the conclusion that the evolution of Ferralsols was conditioned to the polygenetic dynamic of the landscape, reflecting in soils developed from autochtonous parent materials (P.2, P.4, and P.5) and allochtonous parent materials (P.1, P.3 e P.6) over the five geomorphic surfaces identified in the basins of the São Francisco Verdadeiro and São Francisco Falso Rivers. |
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Calegari, Marcia Reginahttp://lattes.cnpq.br/7608085294604450Calegari, Marcia Reginahttp://lattes.cnpq.br/7608085294604450Pontelli, Marga Elizhttp://lattes.cnpq.br/5909311662921266Fujita, Rafaela Harumihttp://lattes.cnpq.br/7601930634370502Nobrega, Maria Teresahttp://lattes.cnpq.br/7208438239950541Oliveira Junior, Jairo Calderari dehttp://lattes.cnpq.br/6180955246357517http://lattes.cnpq.br/6802917878641223Silva, Bruno Aparecido da2022-03-24T14:50:37Z2021-11-26SILVA, Bruno Aparecido da. Condicionantes morfoestruturais na evolução da paisagem no oeste do Paraná e suas interações com os latossolos vermelhos. 2021. 185 f. Tese (Doutorado em Geografia) - Universidade Estadual do Oeste do Paraná, Francisco Beltrão, 2021.https://tede.unioeste.br/handle/tede/5926The evolution dynamic of the landscapes of the Basalt Plateau of the Paraná Sedimentary Basin remain little understood, especially regarding the influence of lithostructural, tectonic, and pedogeomorphic interaction. The hypotheses of this thesis propose that lithostructural factors acted in the differential control of relief dissection, as tectonic pulses interrupted the stability of the landscape during the Cenozoic. In addition, the evolution of the Ferralsols would be conditioned to this dynamic that contributed to the input of allochtonous parent material to the Ferralsols on more recent sectors of the landscape. Therefore, this thesis investigates the factors that acted on the elaboration of the relief and its forms, and on the genesis and evolution of Ferralsols found on the landscape of West Paraná, having the hydrographic basins of the São Francisco Verdadeiro and São Francisco Falso Rivers, left-hand tributaries of the Paraná River, as spatial outline. The methodology was based on the attainment of data in the field, office, and laboratory. In the field, a survey of tectonic structures was carried out, in addition to differentiation of the lithological members, identification of geomorphic surfaces, soil description and sample collection from six Ferralsols profiles for subsequent investigation of their physical, chemical, mineralogical, geochemical, and macro-micromorphological attributes. In the office, the structural data served as a basis for the elaboration of stereograms and for the analysis of paleostress. Cartographic products of the geology (lithostructure and faults), modelled types, elevation, knickpoint density, relief rugosity, swath profiles, and the spatialization of geomorphic surfaces were also elaborated. Morphometric techniques related to the longitudinal profile of the rivers, slope-length index, and basin asymmetry factor were used to demonstrate the tecto-lithostructural control on the geomorphic configuration of the studied river basins. In the laboratory, the physical, chemical, mineralogical, geochemical, and micromorphological attributes of the Ferralsols were investigated. From the statistical evaluation of Principal Components Analysis, it was possible to differentiate the Ferralsols into two main groups, while the macro and micromorphology indicated important evidence of allochtony in profiles P.1, P.3, and P.6. In general, the results enable identification of the lithostructural variations between the lithological members of the Serra Geral Group that outcrop in the study area, these being composed of massive tabular flood basalts and vesicular compounds, which controlled the uneven dissection of the relief, as well as the occurrence of strike-slip faults, mainly NW-SE and NE-SW, which directed the sculpting of the relief forms and the elaboration of the geomorphic surfaces. Two tectonic pulses were recorded that reactivated the transcurrent faults (NE-SW, NW-SE, N-S and E-W) and dismantled the pre-Neogene, geomorphic surface S1, and contributed to the elaboration of surfaces S4 and S5, during the Quartenary. These pulses appear to have been decisive for interrupting the evolution of the Ferralsols and partially removing the most varied weathering profiles, generating allochtonous material for the transitional (P.3) and more subsided sectors of the landscape (P.1 and P.6), where less weathered Ferralsols developed. It has been demonstrated that, in addition to climatic influence, there was an overlap of lithostructural and tectonic controls on the evolution of the regional landscape, which triggered important geomorphic processes of base level change, processes of etching/stripping, and slope retreat in the studied basins. Furthermore, the results enable the conclusion that the evolution of Ferralsols was conditioned to the polygenetic dynamic of the landscape, reflecting in soils developed from autochtonous parent materials (P.2, P.4, and P.5) and allochtonous parent materials (P.1, P.3 e P.6) over the five geomorphic surfaces identified in the basins of the São Francisco Verdadeiro and São Francisco Falso Rivers.A dinâmica de evolução das paisagens do Planalto Basáltico da Bacia Sedimentar do Paraná (PBBSP) ainda permanece pouco compreendida, sobretudo no que tange à influência da interação litoestrutural, tectônica e pedogeomórfica. As hipóteses desta tese propõem que fatores litoestruturais atuaram no controle diferencial da dissecação do relevo, à medida que pulsos tectônicos interromperam a estabilidade da paisagem ao longo do Cenozoico. Adicionalmente, a evolução dos Latossolos Vermelhos (LV) estaria condicionada à essa dinâmica que contribuiu para o aporte de material parental alóctone aos LV dos setores mais recentes da paisagem. Isto posto, nesta tese são investigados os fatores que atuaram na elaboração do relevo, e suas formas, e na gênese e evolução de LV encontrados na paisagem do oeste do Paraná, tendo como recorte espacial as bacias hidrográficas dos rios São Francisco Verdadeiro (SFV) e São Francisco Falso (SFF), tributários esquerdos do rio Paraná. A metodologia se baseou na obtenção de dados em campo, gabinete e laboratório. Em campo, foi realizado o levantamento de estruturas tectônicas, bem como a diferenciação dos membros litológicos, identificação de superfícies geomórficas, descrição e coleta de amostras de solos em seis perfis de LV para posterior investigação de seus atributos físicos e químicos, mineralógicos, geoquímicos e macro-micromorfológicos. Em gabinete, os dados estruturais serviram de base para a elaboração de estereogramas e para a análise de paleostress. Também foram elaborados produtos cartográficos de geologia (litoestrutura e falhas), tipos de modelados, elevação do terreno, densidade de knickpoints, rugosidade do relevo e perfis topográficos de varredura e a espacialização das superfícies geomórficas. Técnicas morfométricas relacionadas ao perfil longitudinal dos rios, relação declividade-extensão (RDE) e fator de assimetria das bacias (FA) foram usadas para demonstrar o controle tecto-litoestrutural na configuração geomórfica das bacias hidrográficas estudadas. Em laboratório foram investigados os atributos físicos e químicos, mineralógicos e geoquímicos e micromorfológicos dos LV. A partir da avaliação estatística de Análise de Componentes Principais (ACP), foi possível diferenciar os LV em dois principais grupos, enquanto que a macro e micromorfologia indicou importantes evidências de alóctonia nos perfis P.1, P.3 e P.6. De modo geral, os resultados permitiram identificar as variações litoestruturais entre os membros litológicos do Grupo Serra Geral que afloram na área do estudo, compostos por derrames basálticos tabulares maciços e compostos vesiculares, que controlaram a dissecação desigual do relevo, assim como a ocorrência de falhas transcorrentes, principalmente NW-SE e NE-SW que direcionaram a esculturação das formas de relevo e elaboração das superfícies geomórficas. Foram registrados dois pulsos tectônicos que reativaram falhas transcorrentes (NE-SW, NW-SE, N-S e E-W) e desmantelaram a superfície geomórfica S1, pré-Neógeno, e contribuíram para a elaboração das superfícies S4 e S5, ao longo do Quaternário. Tais pulsos parecem ter sido decisivos para interromper a evolução dos LV e remover parcialmente os mais variados perfis de intemperismo, gerando materiais alóctones para os setores transicionais (P.3) e mais rebaixados da paisagem (P.1 e P.6), onde LV menos intemperizados se desenvolveram. Ficou demonstrado que houve uma sobreposição de controles litoestruturais e tectônicos na evolução da paisagem regional, e também climáticos, que desencadearam importantes processos geomórficos de mudança do nível de base, processos de etching/stripping e recuo de vertentes nas bacias estudadas. Adicionalmente, os resultados permitem concluir que a evolução dos LV foi condicionada à essa dinâmica poligenética da paisagem, refletindo em solos desenvolvidos a partir de materiais parentais autóctones (P.2, P.4 e P.5) e alóctones (P.1, P.3 e P.6) ao longo de cinco superfícies geomórficas identificadas na área das bacias dos rios SFV e SFF.Submitted by Sandra Mendonça (sandra.mendonca@unioeste.br) on 2022-03-24T14:50:37Z No. of bitstreams: 2 Bruno_Aparecido_Silva_2021.pdf: 16158465 bytes, checksum: 54aff39f53bcc141ab5952a90e3df17d (MD5) license_rdf: 0 bytes, checksum: d41d8cd98f00b204e9800998ecf8427e (MD5)Made available in DSpace on 2022-03-24T14:50:37Z (GMT). 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dc.title.por.fl_str_mv |
Condicionantes morfoestruturais na evolução da paisagem no oeste do Paraná e suas interações com os latossolos vermelhos |
dc.title.alternative.eng.fl_str_mv |
Morphostructural determinants in the evolution of the landscape in west Paraná and their interactions with ferralsols |
title |
Condicionantes morfoestruturais na evolução da paisagem no oeste do Paraná e suas interações com os latossolos vermelhos |
spellingShingle |
Condicionantes morfoestruturais na evolução da paisagem no oeste do Paraná e suas interações com os latossolos vermelhos Silva, Bruno Aparecido da Tectônica Solos cauliníticos Materiais de origem Alóctonia Tectonics Kaolinitic soils Parent materials Allochtony GEOGRAFIA FISICA::GEOMORFOLOGIA |
title_short |
Condicionantes morfoestruturais na evolução da paisagem no oeste do Paraná e suas interações com os latossolos vermelhos |
title_full |
Condicionantes morfoestruturais na evolução da paisagem no oeste do Paraná e suas interações com os latossolos vermelhos |
title_fullStr |
Condicionantes morfoestruturais na evolução da paisagem no oeste do Paraná e suas interações com os latossolos vermelhos |
title_full_unstemmed |
Condicionantes morfoestruturais na evolução da paisagem no oeste do Paraná e suas interações com os latossolos vermelhos |
title_sort |
Condicionantes morfoestruturais na evolução da paisagem no oeste do Paraná e suas interações com os latossolos vermelhos |
author |
Silva, Bruno Aparecido da |
author_facet |
Silva, Bruno Aparecido da |
author_role |
author |
dc.contributor.advisor1.fl_str_mv |
Calegari, Marcia Regina |
dc.contributor.advisor1Lattes.fl_str_mv |
http://lattes.cnpq.br/7608085294604450 |
dc.contributor.referee1.fl_str_mv |
Calegari, Marcia Regina |
dc.contributor.referee1Lattes.fl_str_mv |
http://lattes.cnpq.br/7608085294604450 |
dc.contributor.referee2.fl_str_mv |
Pontelli, Marga Eliz |
dc.contributor.referee2Lattes.fl_str_mv |
http://lattes.cnpq.br/5909311662921266 |
dc.contributor.referee3.fl_str_mv |
Fujita, Rafaela Harumi |
dc.contributor.referee3Lattes.fl_str_mv |
http://lattes.cnpq.br/7601930634370502 |
dc.contributor.referee4.fl_str_mv |
Nobrega, Maria Teresa |
dc.contributor.referee4Lattes.fl_str_mv |
http://lattes.cnpq.br/7208438239950541 |
dc.contributor.referee5.fl_str_mv |
Oliveira Junior, Jairo Calderari de |
dc.contributor.referee5Lattes.fl_str_mv |
http://lattes.cnpq.br/6180955246357517 |
dc.contributor.authorLattes.fl_str_mv |
http://lattes.cnpq.br/6802917878641223 |
dc.contributor.author.fl_str_mv |
Silva, Bruno Aparecido da |
contributor_str_mv |
Calegari, Marcia Regina Calegari, Marcia Regina Pontelli, Marga Eliz Fujita, Rafaela Harumi Nobrega, Maria Teresa Oliveira Junior, Jairo Calderari de |
dc.subject.por.fl_str_mv |
Tectônica Solos cauliníticos Materiais de origem Alóctonia |
topic |
Tectônica Solos cauliníticos Materiais de origem Alóctonia Tectonics Kaolinitic soils Parent materials Allochtony GEOGRAFIA FISICA::GEOMORFOLOGIA |
dc.subject.eng.fl_str_mv |
Tectonics Kaolinitic soils Parent materials Allochtony |
dc.subject.cnpq.fl_str_mv |
GEOGRAFIA FISICA::GEOMORFOLOGIA |
description |
The evolution dynamic of the landscapes of the Basalt Plateau of the Paraná Sedimentary Basin remain little understood, especially regarding the influence of lithostructural, tectonic, and pedogeomorphic interaction. The hypotheses of this thesis propose that lithostructural factors acted in the differential control of relief dissection, as tectonic pulses interrupted the stability of the landscape during the Cenozoic. In addition, the evolution of the Ferralsols would be conditioned to this dynamic that contributed to the input of allochtonous parent material to the Ferralsols on more recent sectors of the landscape. Therefore, this thesis investigates the factors that acted on the elaboration of the relief and its forms, and on the genesis and evolution of Ferralsols found on the landscape of West Paraná, having the hydrographic basins of the São Francisco Verdadeiro and São Francisco Falso Rivers, left-hand tributaries of the Paraná River, as spatial outline. The methodology was based on the attainment of data in the field, office, and laboratory. In the field, a survey of tectonic structures was carried out, in addition to differentiation of the lithological members, identification of geomorphic surfaces, soil description and sample collection from six Ferralsols profiles for subsequent investigation of their physical, chemical, mineralogical, geochemical, and macro-micromorphological attributes. In the office, the structural data served as a basis for the elaboration of stereograms and for the analysis of paleostress. Cartographic products of the geology (lithostructure and faults), modelled types, elevation, knickpoint density, relief rugosity, swath profiles, and the spatialization of geomorphic surfaces were also elaborated. Morphometric techniques related to the longitudinal profile of the rivers, slope-length index, and basin asymmetry factor were used to demonstrate the tecto-lithostructural control on the geomorphic configuration of the studied river basins. In the laboratory, the physical, chemical, mineralogical, geochemical, and micromorphological attributes of the Ferralsols were investigated. From the statistical evaluation of Principal Components Analysis, it was possible to differentiate the Ferralsols into two main groups, while the macro and micromorphology indicated important evidence of allochtony in profiles P.1, P.3, and P.6. In general, the results enable identification of the lithostructural variations between the lithological members of the Serra Geral Group that outcrop in the study area, these being composed of massive tabular flood basalts and vesicular compounds, which controlled the uneven dissection of the relief, as well as the occurrence of strike-slip faults, mainly NW-SE and NE-SW, which directed the sculpting of the relief forms and the elaboration of the geomorphic surfaces. Two tectonic pulses were recorded that reactivated the transcurrent faults (NE-SW, NW-SE, N-S and E-W) and dismantled the pre-Neogene, geomorphic surface S1, and contributed to the elaboration of surfaces S4 and S5, during the Quartenary. These pulses appear to have been decisive for interrupting the evolution of the Ferralsols and partially removing the most varied weathering profiles, generating allochtonous material for the transitional (P.3) and more subsided sectors of the landscape (P.1 and P.6), where less weathered Ferralsols developed. It has been demonstrated that, in addition to climatic influence, there was an overlap of lithostructural and tectonic controls on the evolution of the regional landscape, which triggered important geomorphic processes of base level change, processes of etching/stripping, and slope retreat in the studied basins. Furthermore, the results enable the conclusion that the evolution of Ferralsols was conditioned to the polygenetic dynamic of the landscape, reflecting in soils developed from autochtonous parent materials (P.2, P.4, and P.5) and allochtonous parent materials (P.1, P.3 e P.6) over the five geomorphic surfaces identified in the basins of the São Francisco Verdadeiro and São Francisco Falso Rivers. |
publishDate |
2021 |
dc.date.issued.fl_str_mv |
2021-11-26 |
dc.date.accessioned.fl_str_mv |
2022-03-24T14:50:37Z |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/doctoralThesis |
format |
doctoralThesis |
status_str |
publishedVersion |
dc.identifier.citation.fl_str_mv |
SILVA, Bruno Aparecido da. Condicionantes morfoestruturais na evolução da paisagem no oeste do Paraná e suas interações com os latossolos vermelhos. 2021. 185 f. Tese (Doutorado em Geografia) - Universidade Estadual do Oeste do Paraná, Francisco Beltrão, 2021. |
dc.identifier.uri.fl_str_mv |
https://tede.unioeste.br/handle/tede/5926 |
identifier_str_mv |
SILVA, Bruno Aparecido da. Condicionantes morfoestruturais na evolução da paisagem no oeste do Paraná e suas interações com os latossolos vermelhos. 2021. 185 f. Tese (Doutorado em Geografia) - Universidade Estadual do Oeste do Paraná, Francisco Beltrão, 2021. |
url |
https://tede.unioeste.br/handle/tede/5926 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.program.fl_str_mv |
5677331228603424138 |
dc.relation.confidence.fl_str_mv |
600 600 600 600 |
dc.relation.department.fl_str_mv |
1964243308973517033 |
dc.relation.cnpq.fl_str_mv |
7875981787116932492 |
dc.relation.sponsorship.fl_str_mv |
623134973106312664 |
dc.rights.driver.fl_str_mv |
http://creativecommons.org/licenses/by-nc-nd/4.0/ info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
http://creativecommons.org/licenses/by-nc-nd/4.0/ |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Universidade Estadual do Oeste do Paraná Francisco Beltrão |
dc.publisher.program.fl_str_mv |
Programa de Pós-Graduação em Geografia |
dc.publisher.initials.fl_str_mv |
UNIOESTE |
dc.publisher.country.fl_str_mv |
Brasil |
dc.publisher.department.fl_str_mv |
Centro de Ciências Humanas |
publisher.none.fl_str_mv |
Universidade Estadual do Oeste do Paraná Francisco Beltrão |
dc.source.none.fl_str_mv |
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Universidade Estadual do Oeste do Paraná (UNIOESTE) |
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UNIOESTE |
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UNIOESTE |
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Biblioteca Digital de Teses e Dissertações do UNIOESTE |
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Biblioteca Digital de Teses e Dissertações do UNIOESTE |
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http://tede.unioeste.br:8080/tede/bitstream/tede/5926/5/Bruno_Aparecido_Silva_2021.pdf http://tede.unioeste.br:8080/tede/bitstream/tede/5926/2/license_url http://tede.unioeste.br:8080/tede/bitstream/tede/5926/3/license_text http://tede.unioeste.br:8080/tede/bitstream/tede/5926/4/license_rdf http://tede.unioeste.br:8080/tede/bitstream/tede/5926/1/license.txt |
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Biblioteca Digital de Teses e Dissertações do UNIOESTE - Universidade Estadual do Oeste do Paraná (UNIOESTE) |
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biblioteca.repositorio@unioeste.br |
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