Structural Blocks as Flood Control in Brazilian Pantanal

Detalhes bibliográficos
Autor(a) principal: Ribeiro, Alisson André
Data de Publicação: 2019
Outros Autores: Mioto, Camila Leonardo, Machado, Rômulo, Assine, Mario Luis, Guaraldo, Eliane, Filho, Antonio Conceição Paranhos
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Anuário do Instituto de Geociências (Online)
Texto Completo: https://revistas.ufrj.br/index.php/aigeo/article/view/29739
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.
id UFRJ-21_70f49780c65c82afa150320eb59b3d42
oai_identifier_str oai:www.revistas.ufrj.br:article/29739
network_acronym_str UFRJ-21
network_name_str Anuário do Instituto de Geociências (Online)
repository_id_str
spelling Structural Blocks as Flood Control in Brazilian PantanalRemote sensing; DEM; Tectonics; Sub-RegionsThe 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 do Rio de JaneiroRibeiro, Alisson AndréMioto, Camila LeonardoMachado, RômuloAssine, Mario LuisGuaraldo, ElianeFilho, Antonio Conceição Paranhos2019-10-16info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistas.ufrj.br/index.php/aigeo/article/view/2973910.11137/2018_3_434_444Anuário do Instituto de Geociências; Vol 41, No 3 (2018); 434-444Anuário do Instituto de Geociências; Vol 41, No 3 (2018); 434-4441982-39080101-9759reponame:Anuário do Instituto de Geociências (Online)instname:Universidade Federal do Rio de Janeiro (UFRJ)instacron:UFRJenghttps://revistas.ufrj.br/index.php/aigeo/article/view/29739/16746Copyright (c) 2019 Anuário do Instituto de Geociênciashttp://creativecommons.org/licenses/by/4.0info:eu-repo/semantics/openAccess2020-08-12T18:46:40Zoai:www.revistas.ufrj.br:article/29739Revistahttps://revistas.ufrj.br/index.php/aigeo/indexPUBhttps://revistas.ufrj.br/index.php/aigeo/oaianuario@igeo.ufrj.br||1982-39080101-9759opendoar:2020-08-12T18:46:40Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ)false
dc.title.none.fl_str_mv
Structural Blocks as Flood Control in Brazilian Pantanal
title Structural Blocks as Flood Control in Brazilian Pantanal
spellingShingle Structural Blocks as Flood Control in Brazilian Pantanal
Ribeiro, Alisson André
Remote sensing; DEM; Tectonics; Sub-Regions
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
Guaraldo, Eliane
Filho, Antonio Conceição Paranhos
author_role author
author2 Mioto, Camila Leonardo
Machado, Rômulo
Assine, Mario Luis
Guaraldo, Eliane
Filho, Antonio Conceição Paranhos
author2_role author
author
author
author
author
dc.contributor.none.fl_str_mv

dc.contributor.author.fl_str_mv Ribeiro, Alisson André
Mioto, Camila Leonardo
Machado, Rômulo
Assine, Mario Luis
Guaraldo, Eliane
Filho, Antonio Conceição Paranhos
dc.subject.none.fl_str_mv
dc.subject.por.fl_str_mv Remote sensing; DEM; Tectonics; Sub-Regions
topic Remote sensing; DEM; Tectonics; Sub-Regions
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 2019
dc.date.none.fl_str_mv 2019-10-16
dc.type.none.fl_str_mv

dc.type.driver.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv https://revistas.ufrj.br/index.php/aigeo/article/view/29739
10.11137/2018_3_434_444
url https://revistas.ufrj.br/index.php/aigeo/article/view/29739
identifier_str_mv 10.11137/2018_3_434_444
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv https://revistas.ufrj.br/index.php/aigeo/article/view/29739/16746
dc.rights.driver.fl_str_mv Copyright (c) 2019 Anuário do Instituto de Geociências
http://creativecommons.org/licenses/by/4.0
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Copyright (c) 2019 Anuário do Instituto de Geociências
http://creativecommons.org/licenses/by/4.0
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Universidade Federal do Rio de Janeiro
publisher.none.fl_str_mv Universidade Federal do Rio de Janeiro
dc.source.none.fl_str_mv Anuário do Instituto de Geociências; Vol 41, No 3 (2018); 434-444
Anuário do Instituto de Geociências; Vol 41, No 3 (2018); 434-444
1982-3908
0101-9759
reponame:Anuário do Instituto de Geociências (Online)
instname:Universidade Federal do Rio de Janeiro (UFRJ)
instacron:UFRJ
instname_str Universidade Federal do Rio de Janeiro (UFRJ)
instacron_str UFRJ
institution UFRJ
reponame_str Anuário do Instituto de Geociências (Online)
collection Anuário do Instituto de Geociências (Online)
repository.name.fl_str_mv Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ)
repository.mail.fl_str_mv anuario@igeo.ufrj.br||
_version_ 1797053537363951616