The camaquã basin modelling : tectonostratigraphy through integration of geophysical (gravimetry, well log) and remote sensing data

A tectonostratigraphic study of the Camaquã Basin, formed by Neoproterozoic to Eopaleozoic volcano-sedimentary units, is herein presented. Based on lineaments obtained through LANDSATTM images and geophysical methods, four structural domains were recognized. The depositional and deformational sequen...

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Autores:
Kazmierczak1, Thais de Souza
Castillo, Luis A.
Chemale Jr, Farid
de Souza, Sérgio Florêncio
Gómez Londoño, Ernesto
Tipo de recurso:
Article of journal
Fecha de publicación:
2007
Institución:
Universidad Nacional de Colombia
Repositorio:
Universidad Nacional de Colombia
Idioma:
spa
OAI Identifier:
oai:repositorio.unal.edu.co:unal/34015
Acceso en línea:
https://repositorio.unal.edu.co/handle/unal/34015
http://bdigital.unal.edu.co/24095/
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openAccess
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Atribución-NoComercial 4.0 Internacional
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spelling Atribución-NoComercial 4.0 InternacionalDerechos reservados - Universidad Nacional de Colombiahttp://creativecommons.org/licenses/by-nc/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Kazmierczak1, Thais de Souza115da815-926c-4ed5-bcb3-a66dcd6bd82c300Castillo, Luis A.f3a2fc50-f8ed-4a87-ba63-7b062ea5ff83300Chemale Jr, Farid0df41196-ef5e-4139-bca0-29939e01c6b6300de Souza, Sérgio Florêncio48aa45b8-3843-4132-adf3-42a4615fcbe0300Gómez Londoño, Ernestob3b6802b-cd27-464b-854d-49c74f8e77de3002019-06-27T23:09:52Z2019-06-27T23:09:52Z2007https://repositorio.unal.edu.co/handle/unal/34015http://bdigital.unal.edu.co/24095/A tectonostratigraphic study of the Camaquã Basin, formed by Neoproterozoic to Eopaleozoic volcano-sedimentary units, is herein presented. Based on lineaments obtained through LANDSATTM images and geophysical methods, four structural domains were recognized. The depositional and deformational sequences of the Guaritas and the Bom Jardim Formations were identified onwell logs, where the fluvial deltaic system and brittle to brittle-ductile tectonic evidence is preserved. Differential compaction of sedimentary rocks was recognized using geophysical information (electrical (well log) and potential methods (gravimetry)). The sedimentary package presents variable thickness, increasing to the NE portion of the basin, and a compartmentalization in echelon subbasins, delimited by NW-trending structures is observed. A 3D schematic model of the Camaquã Basin was built based on the geophysical and satellite image data integrated to the Digital Terrane Model.application/pdfspaUNIVERSIDAD NACIONAL DE COLOMBIAhttp://revistas.unal.edu.co/index.php/esrj/article/view/21209Universidad Nacional de Colombia Revistas electrónicas UN Earth Sciences Research JournalEarth Sciences Research JournalEarth Sciences Research Journal; Vol. 11, núm. 1 (2007); 45-55 Earth Sciences Research Journal; Vol. 11, núm. 1 (2007); 45-55 2339-3459 1794-6190Kazmierczak1, Thais de Souza and Castillo, Luis A. and Chemale Jr, Farid and de Souza, Sérgio Florêncio and Gómez Londoño, Ernesto (2007) The camaquã basin modelling : tectonostratigraphy through integration of geophysical (gravimetry, well log) and remote sensing data. Earth Sciences Research Journal; Vol. 11, núm. 1 (2007); 45-55 Earth Sciences Research Journal; Vol. 11, núm. 1 (2007); 45-55 2339-3459 1794-6190 .The camaquã basin modelling : tectonostratigraphy through integration of geophysical (gravimetry, well log) and remote sensing dataArtículo de revistainfo:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501http://purl.org/coar/resource_type/c_2df8fbb1http://purl.org/coar/version/c_970fb48d4fbd8a85Texthttp://purl.org/redcol/resource_type/ARTORIGINAL21209-71977-1-PB.pdfapplication/pdf5200386https://repositorio.unal.edu.co/bitstream/unal/34015/1/21209-71977-1-PB.pdff37fcda632e934c79c55507db419d518MD51THUMBNAIL21209-71977-1-PB.pdf.jpg21209-71977-1-PB.pdf.jpgGenerated Thumbnailimage/jpeg7745https://repositorio.unal.edu.co/bitstream/unal/34015/2/21209-71977-1-PB.pdf.jpgb40dfb1d19f820a52d27b0191c83a28bMD52unal/34015oai:repositorio.unal.edu.co:unal/340152022-12-29 23:03:09.737Repositorio Institucional Universidad Nacional de Colombiarepositorio_nal@unal.edu.co
dc.title.spa.fl_str_mv The camaquã basin modelling : tectonostratigraphy through integration of geophysical (gravimetry, well log) and remote sensing data
title The camaquã basin modelling : tectonostratigraphy through integration of geophysical (gravimetry, well log) and remote sensing data
spellingShingle The camaquã basin modelling : tectonostratigraphy through integration of geophysical (gravimetry, well log) and remote sensing data
title_short The camaquã basin modelling : tectonostratigraphy through integration of geophysical (gravimetry, well log) and remote sensing data
title_full The camaquã basin modelling : tectonostratigraphy through integration of geophysical (gravimetry, well log) and remote sensing data
title_fullStr The camaquã basin modelling : tectonostratigraphy through integration of geophysical (gravimetry, well log) and remote sensing data
title_full_unstemmed The camaquã basin modelling : tectonostratigraphy through integration of geophysical (gravimetry, well log) and remote sensing data
title_sort The camaquã basin modelling : tectonostratigraphy through integration of geophysical (gravimetry, well log) and remote sensing data
dc.creator.fl_str_mv Kazmierczak1, Thais de Souza
Castillo, Luis A.
Chemale Jr, Farid
de Souza, Sérgio Florêncio
Gómez Londoño, Ernesto
dc.contributor.author.spa.fl_str_mv Kazmierczak1, Thais de Souza
Castillo, Luis A.
Chemale Jr, Farid
de Souza, Sérgio Florêncio
Gómez Londoño, Ernesto
description A tectonostratigraphic study of the Camaquã Basin, formed by Neoproterozoic to Eopaleozoic volcano-sedimentary units, is herein presented. Based on lineaments obtained through LANDSATTM images and geophysical methods, four structural domains were recognized. The depositional and deformational sequences of the Guaritas and the Bom Jardim Formations were identified onwell logs, where the fluvial deltaic system and brittle to brittle-ductile tectonic evidence is preserved. Differential compaction of sedimentary rocks was recognized using geophysical information (electrical (well log) and potential methods (gravimetry)). The sedimentary package presents variable thickness, increasing to the NE portion of the basin, and a compartmentalization in echelon subbasins, delimited by NW-trending structures is observed. A 3D schematic model of the Camaquã Basin was built based on the geophysical and satellite image data integrated to the Digital Terrane Model.
publishDate 2007
dc.date.issued.spa.fl_str_mv 2007
dc.date.accessioned.spa.fl_str_mv 2019-06-27T23:09:52Z
dc.date.available.spa.fl_str_mv 2019-06-27T23:09:52Z
dc.type.spa.fl_str_mv Artículo de revista
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url https://repositorio.unal.edu.co/handle/unal/34015
http://bdigital.unal.edu.co/24095/
dc.language.iso.spa.fl_str_mv spa
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dc.relation.spa.fl_str_mv http://revistas.unal.edu.co/index.php/esrj/article/view/21209
dc.relation.ispartof.spa.fl_str_mv Universidad Nacional de Colombia Revistas electrónicas UN Earth Sciences Research Journal
Earth Sciences Research Journal
dc.relation.ispartofseries.none.fl_str_mv Earth Sciences Research Journal; Vol. 11, núm. 1 (2007); 45-55 Earth Sciences Research Journal; Vol. 11, núm. 1 (2007); 45-55 2339-3459 1794-6190
dc.relation.references.spa.fl_str_mv Kazmierczak1, Thais de Souza and Castillo, Luis A. and Chemale Jr, Farid and de Souza, Sérgio Florêncio and Gómez Londoño, Ernesto (2007) The camaquã basin modelling : tectonostratigraphy through integration of geophysical (gravimetry, well log) and remote sensing data. Earth Sciences Research Journal; Vol. 11, núm. 1 (2007); 45-55 Earth Sciences Research Journal; Vol. 11, núm. 1 (2007); 45-55 2339-3459 1794-6190 .
dc.rights.spa.fl_str_mv Derechos reservados - Universidad Nacional de Colombia
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dc.rights.license.spa.fl_str_mv Atribución-NoComercial 4.0 Internacional
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dc.rights.accessrights.spa.fl_str_mv info:eu-repo/semantics/openAccess
rights_invalid_str_mv Atribución-NoComercial 4.0 Internacional
Derechos reservados - Universidad Nacional de Colombia
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eu_rights_str_mv openAccess
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dc.publisher.spa.fl_str_mv UNIVERSIDAD NACIONAL DE COLOMBIA
institution Universidad Nacional de Colombia
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