Structural blocks as flood control in Brazilian Pantanal
Autor(a) principal: | |
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Data de Publicação: | 2018 |
Outros Autores: | , , , , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Repositório Institucional da UNESP |
Texto Completo: | http://dx.doi.org/10.11137/2018_3_434_444 http://hdl.handle.net/11449/190244 |
Resumo: | The Pantanal basin formation and evolution are not well known and explained. This work brings new information showing the structural control over the physical environment of the Pantanal, one of the most important regions all around the world due to its biodiversity. We used different data sets from remote sensing data, the first set is a corrected SRTM (shuttle radar topographic mission) altimetric data and the second is a map of the major lineaments of Pantanal extracted from photointerpretation of satellite images. Both sets were confronted with the official borderlines of Pantanal and to other two limits defined by phytogeography and remote sensing images. It is possible to show that there is a good match between the internal limits of Pantanal and the interpreted lineaments. The altitudes decrease from N to S and from E to W and the slope analysis shows that this declivity is not homogeneous on these directions. The height difference between adjacent blocks is about 3 or 4 meters. Moreover, different regions have different mean altitudes and slope, although the slope inside each block is homogeneous. Considering Pantanal as a Cenozoic active basin, this paper proposes that the neotectonic controls these blocks and so the water flow in the basin, which in turn controls the fauna and flora of the region. |
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Structural blocks as flood control in Brazilian PantanalBlocos estruturais como controle da inundação no Pantanal BrasileiroDEMRemote sensingSub-regionsTectonicsThe Pantanal basin formation and evolution are not well known and explained. This work brings new information showing the structural control over the physical environment of the Pantanal, one of the most important regions all around the world due to its biodiversity. We used different data sets from remote sensing data, the first set is a corrected SRTM (shuttle radar topographic mission) altimetric data and the second is a map of the major lineaments of Pantanal extracted from photointerpretation of satellite images. Both sets were confronted with the official borderlines of Pantanal and to other two limits defined by phytogeography and remote sensing images. It is possible to show that there is a good match between the internal limits of Pantanal and the interpreted lineaments. The altitudes decrease from N to S and from E to W and the slope analysis shows that this declivity is not homogeneous on these directions. The height difference between adjacent blocks is about 3 or 4 meters. Moreover, different regions have different mean altitudes and slope, although the slope inside each block is homogeneous. Considering Pantanal as a Cenozoic active basin, this paper proposes that the neotectonic controls these blocks and so the water flow in the basin, which in turn controls the fauna and flora of the region.Universidade Federal de Mato Grosso do Sul Faculdade de Engenharias Arquitetura e Urbanismo e Geografia Laboratório de Geoprocessamento para Aplicações Ambientais Cidade Universitária, Unidade 7A. Campo Grande, MSLaboratório de Geotecnologias Núcleo de Pesquisa em Produção e Conservação do Cerrado Universidade Federal de Mato Grosso (NUPEC) Campus Universitário de Rondonópolis, MT 270 km 06, Universidade Federal de Mato GrossoUniversidade de São Paulo Instituto de Geociências, Rua do Lago, 562, ButantãUniversidade Estadual Paulista - UNESP Departamento de Geologia Aplicada, Avenida 24 a , 1515Universidade Federal de Mato Grosso do Sul Faculdade de Engenharias Arquitetura e Urbanismo e Geografia UFMS Laboratório da Paisagem Cidade Universitária, s/n°, Caixa Postal 549Universidade Estadual Paulista - UNESP Departamento de Geologia Aplicada, Avenida 24 a , 1515Universidade Federal de Mato Grosso do Sul (UFMS)Universidade Federal de Mato Grosso (NUPEC)Universidade de São Paulo (USP)Universidade Estadual Paulista (Unesp)Ribeiro, Alisson AndréMioto, Camila LeonardoMachado, RômuloAssine, Mario Luis [UNESP]Guaraldo, ElianeFilho, Antonio Conceição Paranhos2019-10-06T17:06:53Z2019-10-06T17:06:53Z2018-01-01info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/article434-444http://dx.doi.org/10.11137/2018_3_434_444Anuario do Instituto de Geociencias, v. 41, n. 3, p. 434-444, 2018.1982-39080101-9759http://hdl.handle.net/11449/19024410.11137/2018_3_434_4442-s2.0-850637555630471102133658128Scopusreponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPengAnuario do Instituto de Geocienciasinfo:eu-repo/semantics/openAccess2021-10-23T19:49:55Zoai:repositorio.unesp.br:11449/190244Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462024-08-05T20:24:55.305424Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false |
dc.title.none.fl_str_mv |
Structural blocks as flood control in Brazilian Pantanal Blocos estruturais como controle da inundação no Pantanal Brasileiro |
title |
Structural blocks as flood control in Brazilian Pantanal |
spellingShingle |
Structural blocks as flood control in Brazilian Pantanal Ribeiro, Alisson André DEM Remote sensing Sub-regions Tectonics |
title_short |
Structural blocks as flood control in Brazilian Pantanal |
title_full |
Structural blocks as flood control in Brazilian Pantanal |
title_fullStr |
Structural blocks as flood control in Brazilian Pantanal |
title_full_unstemmed |
Structural blocks as flood control in Brazilian Pantanal |
title_sort |
Structural blocks as flood control in Brazilian Pantanal |
author |
Ribeiro, Alisson André |
author_facet |
Ribeiro, Alisson André Mioto, Camila Leonardo Machado, Rômulo Assine, Mario Luis [UNESP] Guaraldo, Eliane Filho, Antonio Conceição Paranhos |
author_role |
author |
author2 |
Mioto, Camila Leonardo Machado, Rômulo Assine, Mario Luis [UNESP] Guaraldo, Eliane Filho, Antonio Conceição Paranhos |
author2_role |
author author author author author |
dc.contributor.none.fl_str_mv |
Universidade Federal de Mato Grosso do Sul (UFMS) Universidade Federal de Mato Grosso (NUPEC) Universidade de São Paulo (USP) Universidade Estadual Paulista (Unesp) |
dc.contributor.author.fl_str_mv |
Ribeiro, Alisson André Mioto, Camila Leonardo Machado, Rômulo Assine, Mario Luis [UNESP] Guaraldo, Eliane Filho, Antonio Conceição Paranhos |
dc.subject.por.fl_str_mv |
DEM Remote sensing Sub-regions Tectonics |
topic |
DEM Remote sensing Sub-regions Tectonics |
description |
The Pantanal basin formation and evolution are not well known and explained. This work brings new information showing the structural control over the physical environment of the Pantanal, one of the most important regions all around the world due to its biodiversity. We used different data sets from remote sensing data, the first set is a corrected SRTM (shuttle radar topographic mission) altimetric data and the second is a map of the major lineaments of Pantanal extracted from photointerpretation of satellite images. Both sets were confronted with the official borderlines of Pantanal and to other two limits defined by phytogeography and remote sensing images. It is possible to show that there is a good match between the internal limits of Pantanal and the interpreted lineaments. The altitudes decrease from N to S and from E to W and the slope analysis shows that this declivity is not homogeneous on these directions. The height difference between adjacent blocks is about 3 or 4 meters. Moreover, different regions have different mean altitudes and slope, although the slope inside each block is homogeneous. Considering Pantanal as a Cenozoic active basin, this paper proposes that the neotectonic controls these blocks and so the water flow in the basin, which in turn controls the fauna and flora of the region. |
publishDate |
2018 |
dc.date.none.fl_str_mv |
2018-01-01 2019-10-06T17:06:53Z 2019-10-06T17:06:53Z |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
http://dx.doi.org/10.11137/2018_3_434_444 Anuario do Instituto de Geociencias, v. 41, n. 3, p. 434-444, 2018. 1982-3908 0101-9759 http://hdl.handle.net/11449/190244 10.11137/2018_3_434_444 2-s2.0-85063755563 0471102133658128 |
url |
http://dx.doi.org/10.11137/2018_3_434_444 http://hdl.handle.net/11449/190244 |
identifier_str_mv |
Anuario do Instituto de Geociencias, v. 41, n. 3, p. 434-444, 2018. 1982-3908 0101-9759 10.11137/2018_3_434_444 2-s2.0-85063755563 0471102133658128 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
Anuario do Instituto de Geociencias |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
434-444 |
dc.source.none.fl_str_mv |
Scopus reponame:Repositório Institucional da UNESP instname:Universidade Estadual Paulista (UNESP) instacron:UNESP |
instname_str |
Universidade Estadual Paulista (UNESP) |
instacron_str |
UNESP |
institution |
UNESP |
reponame_str |
Repositório Institucional da UNESP |
collection |
Repositório Institucional da UNESP |
repository.name.fl_str_mv |
Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP) |
repository.mail.fl_str_mv |
|
_version_ |
1808129199343403008 |