Foreland flexure rigidity and lithospheric thickness in Eastern Cordillera and the Llanos Orientales basin from receiver functions analysis
The Colombian territory is strongly influenced by tectonic and orogenic processes that have shaped the Andean orogenic belt. This study focuses on the Eastern Cordillera (EC) and the adjacent Llanos Orientales foreland basin, where contrasting flexural lithospheric responses have been suggested. Pre...
- Autores:
-
Herrera Báez, Jaime Andrés
- Tipo de recurso:
- Trabajo de grado de pregrado
- Fecha de publicación:
- 2025
- Institución:
- Universidad de los Andes
- Repositorio:
- Séneca: repositorio Uniandes
- Idioma:
- eng
- OAI Identifier:
- oai:repositorio.uniandes.edu.co:1992/76340
- Acceso en línea:
- https://hdl.handle.net/1992/76340
- Palabra clave:
- S-to-P receiver functions
Lithospheric flexure
Lithospheric thickness
Eastern Cordillera
Llanos basin
Geociencias
- Rights
- openAccess
- License
- Attribution 4.0 International
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|
dc.title.eng.fl_str_mv |
Foreland flexure rigidity and lithospheric thickness in Eastern Cordillera and the Llanos Orientales basin from receiver functions analysis |
title |
Foreland flexure rigidity and lithospheric thickness in Eastern Cordillera and the Llanos Orientales basin from receiver functions analysis |
spellingShingle |
Foreland flexure rigidity and lithospheric thickness in Eastern Cordillera and the Llanos Orientales basin from receiver functions analysis S-to-P receiver functions Lithospheric flexure Lithospheric thickness Eastern Cordillera Llanos basin Geociencias |
title_short |
Foreland flexure rigidity and lithospheric thickness in Eastern Cordillera and the Llanos Orientales basin from receiver functions analysis |
title_full |
Foreland flexure rigidity and lithospheric thickness in Eastern Cordillera and the Llanos Orientales basin from receiver functions analysis |
title_fullStr |
Foreland flexure rigidity and lithospheric thickness in Eastern Cordillera and the Llanos Orientales basin from receiver functions analysis |
title_full_unstemmed |
Foreland flexure rigidity and lithospheric thickness in Eastern Cordillera and the Llanos Orientales basin from receiver functions analysis |
title_sort |
Foreland flexure rigidity and lithospheric thickness in Eastern Cordillera and the Llanos Orientales basin from receiver functions analysis |
dc.creator.fl_str_mv |
Herrera Báez, Jaime Andrés |
dc.contributor.advisor.none.fl_str_mv |
Nitescu, Bogdan Poveda Nuñez, Hugo Esteban |
dc.contributor.author.none.fl_str_mv |
Herrera Báez, Jaime Andrés |
dc.contributor.jury.none.fl_str_mv |
León Loya, Rodrigo Alejandro |
dc.subject.keyword.eng.fl_str_mv |
S-to-P receiver functions Lithospheric flexure Lithospheric thickness Eastern Cordillera Llanos basin |
topic |
S-to-P receiver functions Lithospheric flexure Lithospheric thickness Eastern Cordillera Llanos basin Geociencias |
dc.subject.themes.spa.fl_str_mv |
Geociencias |
description |
The Colombian territory is strongly influenced by tectonic and orogenic processes that have shaped the Andean orogenic belt. This study focuses on the Eastern Cordillera (EC) and the adjacent Llanos Orientales foreland basin, where contrasting flexural lithospheric responses have been suggested. Previous research indicates that the northeastern part of the foreland lithosphere in the Llanos Orientales basin experiences significant flexure, possibly related to a reduced thickness, while in the southwestern region of the foreland basin the lithosphere is more rigid and more resistant to flexing. Using S-wave receiver function analysis (SRF’S), this project estimates the lithospheric thickness and examines the flexural response within the study area. S-to-P receiver functions were analyzed to detect the depth of the lithosphere-asthenosphere boundary (LAB) beneath several seismic stations in the Eastern Cordillera and the Llanos Orientales foreland basin. Results show LAB depths between 97 and 110 km in the southern and central EC, increasing to about 120 km near the northeastern station TAM, and depths around 105 km in the Llanos Basin. These spatial variations in LAB depth may reflect variations in the flexure of the foreland lithosphere and the amount of crustal shortening and orogenic loading along the Eastern Cordillera. Deep seismicity patterns further suggest a steeply dipping subducting slab beneath the northern EC, which may also influence the lithospheric structure. Despite limitations related to station coverage and event distribution, future studies could benefit from expanding the seismic network and increasing the dataset to improve spatial resolution and confidence in lithospheric thickness estimates. |
publishDate |
2025 |
dc.date.accessioned.none.fl_str_mv |
2025-06-19T14:19:53Z |
dc.date.available.none.fl_str_mv |
2025-06-19T14:19:53Z |
dc.date.issued.none.fl_str_mv |
2025-03 |
dc.type.none.fl_str_mv |
Trabajo de grado - Pregrado |
dc.type.driver.none.fl_str_mv |
info:eu-repo/semantics/bachelorThesis |
dc.type.version.none.fl_str_mv |
info:eu-repo/semantics/acceptedVersion |
dc.type.coar.none.fl_str_mv |
http://purl.org/coar/resource_type/c_7a1f |
dc.type.content.none.fl_str_mv |
Text |
dc.type.redcol.none.fl_str_mv |
http://purl.org/redcol/resource_type/TP |
format |
http://purl.org/coar/resource_type/c_7a1f |
status_str |
acceptedVersion |
dc.identifier.uri.none.fl_str_mv |
https://hdl.handle.net/1992/76340 |
dc.identifier.instname.none.fl_str_mv |
instname:Universidad de los Andes |
dc.identifier.reponame.none.fl_str_mv |
reponame:Repositorio Institucional Séneca |
dc.identifier.repourl.none.fl_str_mv |
repourl:https://repositorio.uniandes.edu.co/ |
url |
https://hdl.handle.net/1992/76340 |
identifier_str_mv |
instname:Universidad de los Andes reponame:Repositorio Institucional Séneca repourl:https://repositorio.uniandes.edu.co/ |
dc.language.iso.none.fl_str_mv |
eng |
language |
eng |
dc.rights.en.fl_str_mv |
Attribution 4.0 International |
dc.rights.uri.none.fl_str_mv |
http://creativecommons.org/licenses/by/4.0/ |
dc.rights.accessrights.none.fl_str_mv |
info:eu-repo/semantics/openAccess |
dc.rights.coar.none.fl_str_mv |
http://purl.org/coar/access_right/c_abf2 |
rights_invalid_str_mv |
Attribution 4.0 International http://creativecommons.org/licenses/by/4.0/ http://purl.org/coar/access_right/c_abf2 |
eu_rights_str_mv |
openAccess |
dc.format.extent.none.fl_str_mv |
38 páginas |
dc.format.mimetype.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Universidad de los Andes |
dc.publisher.program.none.fl_str_mv |
Geociencias |
dc.publisher.faculty.none.fl_str_mv |
Facultad de Ciencias |
dc.publisher.department.none.fl_str_mv |
Departamento de Geociencias |
publisher.none.fl_str_mv |
Universidad de los Andes |
institution |
Universidad de los Andes |
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Nitescu, Bogdanvirtual::24290-1Poveda Nuñez, Hugo Estebanvirtual::24291-1Herrera Báez, Jaime AndrésLeón Loya, Rodrigo Alejandro2025-06-19T14:19:53Z2025-06-19T14:19:53Z2025-03https://hdl.handle.net/1992/76340instname:Universidad de los Andesreponame:Repositorio Institucional Sénecarepourl:https://repositorio.uniandes.edu.co/The Colombian territory is strongly influenced by tectonic and orogenic processes that have shaped the Andean orogenic belt. This study focuses on the Eastern Cordillera (EC) and the adjacent Llanos Orientales foreland basin, where contrasting flexural lithospheric responses have been suggested. Previous research indicates that the northeastern part of the foreland lithosphere in the Llanos Orientales basin experiences significant flexure, possibly related to a reduced thickness, while in the southwestern region of the foreland basin the lithosphere is more rigid and more resistant to flexing. Using S-wave receiver function analysis (SRF’S), this project estimates the lithospheric thickness and examines the flexural response within the study area. S-to-P receiver functions were analyzed to detect the depth of the lithosphere-asthenosphere boundary (LAB) beneath several seismic stations in the Eastern Cordillera and the Llanos Orientales foreland basin. Results show LAB depths between 97 and 110 km in the southern and central EC, increasing to about 120 km near the northeastern station TAM, and depths around 105 km in the Llanos Basin. These spatial variations in LAB depth may reflect variations in the flexure of the foreland lithosphere and the amount of crustal shortening and orogenic loading along the Eastern Cordillera. Deep seismicity patterns further suggest a steeply dipping subducting slab beneath the northern EC, which may also influence the lithospheric structure. 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