A proposal on the classification of systems tracts: application to the allostratigraphy and sequence stratigraphy of the cretaceous colombian basin. part 2: barremian to maastrichtian
The Barremian to Maastrichtian interval of the sedimentary succession from the Cretaceous Colombian Basin is divided in stratigraphic sequences and in several allostratigraphic units, which include the Fómeque, Une, and Chipaque Alloformations, the Guadalupe Allogroup, and the lower part of the Guad...
- Autores:
-
Guerrero, Javier
- Tipo de recurso:
- Article of journal
- Fecha de publicación:
- 2002
- Institución:
- Universidad Nacional de Colombia
- Repositorio:
- Universidad Nacional de Colombia
- Idioma:
- spa
- OAI Identifier:
- oai:repositorio.unal.edu.co:unal/42104
- Acceso en línea:
- https://repositorio.unal.edu.co/handle/unal/42104
http://bdigital.unal.edu.co/32201/
- Palabra clave:
- Geología
Ciencias de la tierra
Geociencias
Aloestratigrafía
Estratigrafía Secuencial
Cretácico
Cuenca de Retroarco
Exploración de Hidrocarburos
Litoestratigrafia
Paleogeografía y Sedimentologia
Allostratigraphy
Back-Arc Basin
Cretaceous
Hydrocarbon Exploration
Lithostratigraphy
Paleogeography
Sedimentology and Sequence Stratigraphy
- Rights
- openAccess
- License
- Atribución-NoComercial 4.0 Internacional
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| dc.title.spa.fl_str_mv |
A proposal on the classification of systems tracts: application to the allostratigraphy and sequence stratigraphy of the cretaceous colombian basin. part 2: barremian to maastrichtian |
| title |
A proposal on the classification of systems tracts: application to the allostratigraphy and sequence stratigraphy of the cretaceous colombian basin. part 2: barremian to maastrichtian |
| spellingShingle |
A proposal on the classification of systems tracts: application to the allostratigraphy and sequence stratigraphy of the cretaceous colombian basin. part 2: barremian to maastrichtian Geología Ciencias de la tierra Geociencias Aloestratigrafía Estratigrafía Secuencial Cretácico Cuenca de Retroarco Exploración de Hidrocarburos Litoestratigrafia Paleogeografía y Sedimentologia Allostratigraphy Back-Arc Basin Cretaceous Hydrocarbon Exploration Lithostratigraphy Paleogeography Sedimentology and Sequence Stratigraphy |
| title_short |
A proposal on the classification of systems tracts: application to the allostratigraphy and sequence stratigraphy of the cretaceous colombian basin. part 2: barremian to maastrichtian |
| title_full |
A proposal on the classification of systems tracts: application to the allostratigraphy and sequence stratigraphy of the cretaceous colombian basin. part 2: barremian to maastrichtian |
| title_fullStr |
A proposal on the classification of systems tracts: application to the allostratigraphy and sequence stratigraphy of the cretaceous colombian basin. part 2: barremian to maastrichtian |
| title_full_unstemmed |
A proposal on the classification of systems tracts: application to the allostratigraphy and sequence stratigraphy of the cretaceous colombian basin. part 2: barremian to maastrichtian |
| title_sort |
A proposal on the classification of systems tracts: application to the allostratigraphy and sequence stratigraphy of the cretaceous colombian basin. part 2: barremian to maastrichtian |
| dc.creator.fl_str_mv |
Guerrero, Javier |
| dc.contributor.author.spa.fl_str_mv |
Guerrero, Javier |
| dc.subject.proposal.spa.fl_str_mv |
Geología Ciencias de la tierra Geociencias Aloestratigrafía Estratigrafía Secuencial Cretácico Cuenca de Retroarco Exploración de Hidrocarburos Litoestratigrafia Paleogeografía y Sedimentologia Allostratigraphy Back-Arc Basin Cretaceous Hydrocarbon Exploration Lithostratigraphy Paleogeography Sedimentology and Sequence Stratigraphy |
| topic |
Geología Ciencias de la tierra Geociencias Aloestratigrafía Estratigrafía Secuencial Cretácico Cuenca de Retroarco Exploración de Hidrocarburos Litoestratigrafia Paleogeografía y Sedimentologia Allostratigraphy Back-Arc Basin Cretaceous Hydrocarbon Exploration Lithostratigraphy Paleogeography Sedimentology and Sequence Stratigraphy |
| description |
The Barremian to Maastrichtian interval of the sedimentary succession from the Cretaceous Colombian Basin is divided in stratigraphic sequences and in several allostratigraphic units, which include the Fómeque, Une, and Chipaque Alloformations, the Guadalupe Allogroup, and the lower part of the Guaduas Alloformation. The division is based on the recognition of regional surfaces of sedimentological discontinuity, corresponding mainly to Transgressive Surfaces (TS) located at the base of Transgressive Systems Tracts (TST), and Regressive Surfaces (RS) coincident with Sequence Boundaries (SB) and located at the base of Regressive Systems Tracts (RST). The proposed allostratigraphic units are composed of facies belts, which extend across the whole basin and include laterally adjacent and essentially synchronous lithostratigraphic units. The base of the Fómeque Alloformation is located en the Transgressive Surface (TS) at the Hauterivian/Barremian boundary. The base of the Une Alloformation is located on the Regressive Surface (RS) at the Aptian/Albian boundary. The base of the Chipaque Alloformation on the Transgressive Surface (TS) at the Cenomanian /Turonian boundary, and the base of the Guadalupe Allogroup on the Regressive Surface (RS) at the Santonian/Campanian boundary. The Une Alloformation is subdivided in allomembers, using the Transgressive Surface (TS) at the Lower Albian! Middle Albian boundary and the Regressive Surface (RS) at the Albian/Cenomanian boundary. In the same way, the Guadalupe Allogroup is subdivided in the Lower, Middle, and Upper Guadalupe Alloformations, using the Transgressive Surface (TS) at the Lower Campanian/Upper Campanian boundary and the Regressive Surface (RS) at the Campanian! Maastrichtian boundary. The succession is capped by the lower part of the Guaduas Alloformation, which is located over the Transgressive Surface (TS) at the Lower Maastrichtian/Upper Maastrichtian boundary. |
| publishDate |
2002 |
| dc.date.issued.spa.fl_str_mv |
2002 |
| dc.date.accessioned.spa.fl_str_mv |
2019-06-28T10:31:49Z |
| dc.date.available.spa.fl_str_mv |
2019-06-28T10:31:49Z |
| dc.type.spa.fl_str_mv |
Artículo de revista |
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http://purl.org/coar/resource_type/c_2df8fbb1 |
| dc.type.driver.spa.fl_str_mv |
info:eu-repo/semantics/article |
| dc.type.version.spa.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
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http://purl.org/coar/resource_type/c_6501 |
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http://purl.org/coar/version/c_970fb48d4fbd8a85 |
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Text |
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http://purl.org/redcol/resource_type/ART |
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publishedVersion |
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https://repositorio.unal.edu.co/handle/unal/42104 |
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http://bdigital.unal.edu.co/32201/ |
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https://repositorio.unal.edu.co/handle/unal/42104 http://bdigital.unal.edu.co/32201/ |
| dc.language.iso.spa.fl_str_mv |
spa |
| language |
spa |
| dc.relation.spa.fl_str_mv |
http://revistas.unal.edu.co/index.php/geocol/article/view/31581 |
| dc.relation.ispartof.spa.fl_str_mv |
Universidad Nacional de Colombia Revistas electrónicas UN Geología Colombiana Geología Colombiana |
| dc.relation.ispartofseries.none.fl_str_mv |
Geología Colombiana - An International Journal on Geosciences; Vol. 27 (2002); 27-49 Geología Colombiana; Vol. 27 (2002); 27-49 2357-3767 0072-0992 |
| dc.relation.references.spa.fl_str_mv |
Guerrero, Javier (2002) A proposal on the classification of systems tracts: application to the allostratigraphy and sequence stratigraphy of the cretaceous colombian basin. part 2: barremian to maastrichtian. Geología Colombiana - An International Journal on Geosciences; Vol. 27 (2002); 27-49 Geología Colombiana; Vol. 27 (2002); 27-49 2357-3767 0072-0992 . |
| dc.rights.spa.fl_str_mv |
Derechos reservados - Universidad Nacional de Colombia |
| dc.rights.coar.fl_str_mv |
http://purl.org/coar/access_right/c_abf2 |
| dc.rights.license.spa.fl_str_mv |
Atribución-NoComercial 4.0 Internacional |
| dc.rights.uri.spa.fl_str_mv |
http://creativecommons.org/licenses/by-nc/4.0/ |
| 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 http://creativecommons.org/licenses/by-nc/4.0/ http://purl.org/coar/access_right/c_abf2 |
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openAccess |
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application/pdf |
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Departamento de Geociencias |
| institution |
Universidad Nacional de Colombia |
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https://repositorio.unal.edu.co/bitstream/unal/42104/1/31581-114919-1-PB.pdf https://repositorio.unal.edu.co/bitstream/unal/42104/2/31581-114919-1-PB.pdf.jpg |
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1814090190694645760 |
| 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_abf2Guerrero, Javiere19fa18a-ae59-459f-80c9-0287fee403543002019-06-28T10:31:49Z2019-06-28T10:31:49Z2002https://repositorio.unal.edu.co/handle/unal/42104http://bdigital.unal.edu.co/32201/The Barremian to Maastrichtian interval of the sedimentary succession from the Cretaceous Colombian Basin is divided in stratigraphic sequences and in several allostratigraphic units, which include the Fómeque, Une, and Chipaque Alloformations, the Guadalupe Allogroup, and the lower part of the Guaduas Alloformation. The division is based on the recognition of regional surfaces of sedimentological discontinuity, corresponding mainly to Transgressive Surfaces (TS) located at the base of Transgressive Systems Tracts (TST), and Regressive Surfaces (RS) coincident with Sequence Boundaries (SB) and located at the base of Regressive Systems Tracts (RST). The proposed allostratigraphic units are composed of facies belts, which extend across the whole basin and include laterally adjacent and essentially synchronous lithostratigraphic units. The base of the Fómeque Alloformation is located en the Transgressive Surface (TS) at the Hauterivian/Barremian boundary. The base of the Une Alloformation is located on the Regressive Surface (RS) at the Aptian/Albian boundary. The base of the Chipaque Alloformation on the Transgressive Surface (TS) at the Cenomanian /Turonian boundary, and the base of the Guadalupe Allogroup on the Regressive Surface (RS) at the Santonian/Campanian boundary. The Une Alloformation is subdivided in allomembers, using the Transgressive Surface (TS) at the Lower Albian! Middle Albian boundary and the Regressive Surface (RS) at the Albian/Cenomanian boundary. In the same way, the Guadalupe Allogroup is subdivided in the Lower, Middle, and Upper Guadalupe Alloformations, using the Transgressive Surface (TS) at the Lower Campanian/Upper Campanian boundary and the Regressive Surface (RS) at the Campanian! Maastrichtian boundary. The succession is capped by the lower part of the Guaduas Alloformation, which is located over the Transgressive Surface (TS) at the Lower Maastrichtian/Upper Maastrichtian boundary.El intervalo Barremiano a Maastrichtiano de la sucesión sedimentaria de la Cuenca Cretácica Colombiana es dividido en secuencias estratigráficas y en varias unidades aloestratigráficas, que incluyen las Aloformaciones Fómeque, Une y Chipaque, el Alogrupo Guadalupe y la parte inferior de la Aloformación Guaduas. La división se basa en el reconocimiento de superficies regionales de discontinuidad sedimentológica, correspondientes principal mente a Superficies Transgresivas (TS) situadas en la base de Sistemas Transgresivos (TST), y a Superficies Regresivas (RS) coincidentes con Límites de Secuencia (SB) y situadas en la base de Sistemas Regresivos (RST). Las unidades aloestratigráficas propuestas se componen de cintas de facies que se extienden por toda la cuenca e incluyen unidades litoestratigráficas lateral mente adyacentes y esencialmente sincrónicas. La base de la Aloformación Fómeque se situa en la Superficie Transgresiva (TS) del limite Hauteriviano / Barremiano. La base de la Aloformación Une se sitúa en la Superficie Regresiva (RS) del limite Aptiano/Albiano. La base de la Aloformación Chipaque en la Superficie Transgresiva (TS) del limite Cenomaniano/Turoniano y la base del Alogrupo Guadalupe en la Superficie Regresiva (RS) del limite Santoniano/Campaniano. La Aloformación Une se subdivide en alomiembros, utilizando la Superficie Transgresiva (TS) del limite Albiano Inferior/ Albiano Medio y la Superficie Regresiva (RS) del limite Albiano/Cenomaniano. De igual manera, el Alogrupo Guadalupe se subdivide en las Aloformaciones Guadalupe Inferior, Medio y Superior utilizando la Superficie Transgresiva (TS) del límite Campaniano lnferior /Campaniano Superior y la Superficie Regresiva (RS) del limite Campaniano/Maastrichtiano. La sucesión es cubierta por la parte inferior de la Aloformación Guaduas, que se sitúa sobre la Superficie Transgresiva (TS) del limite Maastrichtiano Inferior / Maastrichtiano Superior.application/pdfspaDepartamento de Geocienciashttp://revistas.unal.edu.co/index.php/geocol/article/view/31581Universidad Nacional de Colombia Revistas electrónicas UN Geología ColombianaGeología ColombianaGeología Colombiana - An International Journal on Geosciences; Vol. 27 (2002); 27-49 Geología Colombiana; Vol. 27 (2002); 27-49 2357-3767 0072-0992Guerrero, Javier (2002) A proposal on the classification of systems tracts: application to the allostratigraphy and sequence stratigraphy of the cretaceous colombian basin. part 2: barremian to maastrichtian. Geología Colombiana - An International Journal on Geosciences; Vol. 27 (2002); 27-49 Geología Colombiana; Vol. 27 (2002); 27-49 2357-3767 0072-0992 .A proposal on the classification of systems tracts: application to the allostratigraphy and sequence stratigraphy of the cretaceous colombian basin. part 2: barremian to maastrichtianArtículo 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/ARTGeologíaCiencias de la tierraGeocienciasAloestratigrafíaEstratigrafía SecuencialCretácicoCuenca de RetroarcoExploración de HidrocarburosLitoestratigrafiaPaleogeografía y SedimentologiaAllostratigraphyBack-Arc BasinCretaceousHydrocarbon ExplorationLithostratigraphyPaleogeographySedimentology and Sequence StratigraphyORIGINAL31581-114919-1-PB.pdfapplication/pdf23984532https://repositorio.unal.edu.co/bitstream/unal/42104/1/31581-114919-1-PB.pdf2a833d61666851407df0feba407912afMD51THUMBNAIL31581-114919-1-PB.pdf.jpg31581-114919-1-PB.pdf.jpgGenerated Thumbnailimage/jpeg8296https://repositorio.unal.edu.co/bitstream/unal/42104/2/31581-114919-1-PB.pdf.jpgb50b36b797d7b85fa8f03c657fe64105MD52unal/42104oai:repositorio.unal.edu.co:unal/421042023-02-05 23:06:17.772Repositorio Institucional Universidad Nacional de Colombiarepositorio_nal@unal.edu.co |