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...

Full description

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
id UNIANDES2_4d27ed1d93db531f34a02e3aae61b07d
oai_identifier_str oai:repositorio.uniandes.edu.co:1992/76340
network_acronym_str UNIANDES2
network_name_str Séneca: repositorio Uniandes
repository_id_str
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
bitstream.url.fl_str_mv https://repositorio.uniandes.edu.co/bitstreams/f6e77164-a4f6-462d-9e43-9403ab7ab749/download
https://repositorio.uniandes.edu.co/bitstreams/dd5ad6b8-7fa5-487a-9e7f-11da924079d8/download
https://repositorio.uniandes.edu.co/bitstreams/e96272f4-f170-497b-a54c-e94de80f8ff7/download
https://repositorio.uniandes.edu.co/bitstreams/a98567e0-0f80-4b90-93b4-b9d77b7ced60/download
https://repositorio.uniandes.edu.co/bitstreams/66989f36-798f-476b-bcbc-34036239a1c1/download
https://repositorio.uniandes.edu.co/bitstreams/fe36fa0c-6e64-4b16-9e70-ba521267dda9/download
https://repositorio.uniandes.edu.co/bitstreams/2fb140a3-4fc3-4671-88b3-5ea5acc88153/download
https://repositorio.uniandes.edu.co/bitstreams/3e91e36b-e57c-4740-97bc-93cae1b9ce92/download
bitstream.checksum.fl_str_mv 173a36ec21239d9093dfc65c1b8d32c0
606f856172da5163a719a9a77092856f
0175ea4a2d4caec4bbcc37e300941108
ae9e573a68e7f92501b6913cc846c39f
3a34363becc1e2ac05e16759d8a649f4
8ee2c5f68ca50d186ac5c92d70db763f
c3e9dc6230c6da7075990eef7f430485
53a894533de2051b00c9b6e81100fc75
bitstream.checksumAlgorithm.fl_str_mv MD5
MD5
MD5
MD5
MD5
MD5
MD5
MD5
repository.name.fl_str_mv Repositorio institucional Séneca
repository.mail.fl_str_mv adminrepositorio@uniandes.edu.co
_version_ 1837005117911465984
spelling 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. 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.Pregrado38 páginasapplication/pdfengUniversidad de los AndesGeocienciasFacultad de CienciasDepartamento de GeocienciasAttribution 4.0 Internationalhttp://creativecommons.org/licenses/by/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Foreland flexure rigidity and lithospheric thickness in Eastern Cordillera and the Llanos Orientales basin from receiver functions analysisTrabajo de grado - Pregradoinfo:eu-repo/semantics/bachelorThesisinfo:eu-repo/semantics/acceptedVersionhttp://purl.org/coar/resource_type/c_7a1fTexthttp://purl.org/redcol/resource_type/TPS-to-P receiver functionsLithospheric flexureLithospheric thicknessEastern CordilleraLlanos basinGeociencias202121580Publication120615dc-2a5a-4c66-9a42-8e426e8a66eevirtual::24290-120a88af1-28ca-4b43-b9f4-6b256930260dvirtual::24291-1120615dc-2a5a-4c66-9a42-8e426e8a66eevirtual::24290-120a88af1-28ca-4b43-b9f4-6b256930260dvirtual::24291-1ORIGINALForeland flexure rigidity and lithospheric thickness in Eastern Cordillera and the Llanos Orientales basin from receiver functions analysis.pdfForeland flexure rigidity and lithospheric thickness in Eastern Cordillera and the Llanos Orientales basin from receiver functions analysis.pdfapplication/pdf3548917https://repositorio.uniandes.edu.co/bitstreams/f6e77164-a4f6-462d-9e43-9403ab7ab749/download173a36ec21239d9093dfc65c1b8d32c0MD51Formato_autorizacion_tesis_Jaime_EP_BN.pdfFormato_autorizacion_tesis_Jaime_EP_BN.pdfHIDEapplication/pdf427567https://repositorio.uniandes.edu.co/bitstreams/dd5ad6b8-7fa5-487a-9e7f-11da924079d8/download606f856172da5163a719a9a77092856fMD52CC-LICENSElicense_rdflicense_rdfapplication/rdf+xml; charset=utf-8908https://repositorio.uniandes.edu.co/bitstreams/e96272f4-f170-497b-a54c-e94de80f8ff7/download0175ea4a2d4caec4bbcc37e300941108MD53LICENSElicense.txtlicense.txttext/plain; charset=utf-82535https://repositorio.uniandes.edu.co/bitstreams/a98567e0-0f80-4b90-93b4-b9d77b7ced60/downloadae9e573a68e7f92501b6913cc846c39fMD54TEXTForeland flexure rigidity and lithospheric thickness in Eastern Cordillera and the Llanos Orientales basin from receiver functions analysis.pdf.txtForeland flexure rigidity and lithospheric thickness in Eastern Cordillera and the Llanos Orientales basin from receiver functions analysis.pdf.txtExtracted texttext/plain56578https://repositorio.uniandes.edu.co/bitstreams/66989f36-798f-476b-bcbc-34036239a1c1/download3a34363becc1e2ac05e16759d8a649f4MD55Formato_autorizacion_tesis_Jaime_EP_BN.pdf.txtFormato_autorizacion_tesis_Jaime_EP_BN.pdf.txtExtracted texttext/plain2054https://repositorio.uniandes.edu.co/bitstreams/fe36fa0c-6e64-4b16-9e70-ba521267dda9/download8ee2c5f68ca50d186ac5c92d70db763fMD57THUMBNAILForeland flexure rigidity and lithospheric thickness in Eastern Cordillera and the Llanos Orientales basin from receiver functions analysis.pdf.jpgForeland flexure rigidity and lithospheric thickness in Eastern Cordillera and the Llanos Orientales basin from receiver functions analysis.pdf.jpgIM Thumbnailimage/jpeg11626https://repositorio.uniandes.edu.co/bitstreams/2fb140a3-4fc3-4671-88b3-5ea5acc88153/downloadc3e9dc6230c6da7075990eef7f430485MD56Formato_autorizacion_tesis_Jaime_EP_BN.pdf.jpgFormato_autorizacion_tesis_Jaime_EP_BN.pdf.jpgIM Thumbnailimage/jpeg14772https://repositorio.uniandes.edu.co/bitstreams/3e91e36b-e57c-4740-97bc-93cae1b9ce92/download53a894533de2051b00c9b6e81100fc75MD581992/76340oai:repositorio.uniandes.edu.co:1992/763402025-06-20 04:02:45.641http://creativecommons.org/licenses/by/4.0/Attribution 4.0 Internationalopen.accesshttps://repositorio.uniandes.edu.coRepositorio institucional Sénecaadminrepositorio@uniandes.edu.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