Integrated provenance evaluation of the cretaceous sedimentary record in the Upper Magdalena Valley Basin: implications in the Northern Andes Tectonic Evolution (2022)
- Authors:
- Autor USP: AMEZQUITA, MAURICIO PARRA - IGC
- Unidade: IGC
- Subjects: EVOLUÇÃO TECTÔNICA; CRETÁCEO
- Language: Inglês
- Conference titles: Semana Técnica de Geología, Ingenieria Geológica y Geociencias
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ABNT
CALDERON-DÍAZ, Laura Cristina et al. Integrated provenance evaluation of the cretaceous sedimentary record in the Upper Magdalena Valley Basin: implications in the Northern Andes Tectonic Evolution. 2022, Anais.. [S.l.]: Instituto de Geociências, Universidade de São Paulo, 2022. Disponível em: https://repositorio.usp.br/directbitstream/a90b29e8-ae09-4d0c-8ea5-6e2062ebe773/3235682.pdf. Acesso em: 12 mar. 2026. -
APA
Calderon-Díaz, L. C., Zapata, S., Cardona, A., Parra, M., Patiño, A., & Valencia, V. A. (2022). Integrated provenance evaluation of the cretaceous sedimentary record in the Upper Magdalena Valley Basin: implications in the Northern Andes Tectonic Evolution. In . Instituto de Geociências, Universidade de São Paulo. Recuperado de https://repositorio.usp.br/directbitstream/a90b29e8-ae09-4d0c-8ea5-6e2062ebe773/3235682.pdf -
NLM
Calderon-Díaz LC, Zapata S, Cardona A, Parra M, Patiño A, Valencia VA. Integrated provenance evaluation of the cretaceous sedimentary record in the Upper Magdalena Valley Basin: implications in the Northern Andes Tectonic Evolution [Internet]. 2022 ;[citado 2026 mar. 12 ] Available from: https://repositorio.usp.br/directbitstream/a90b29e8-ae09-4d0c-8ea5-6e2062ebe773/3235682.pdf -
Vancouver
Calderon-Díaz LC, Zapata S, Cardona A, Parra M, Patiño A, Valencia VA. Integrated provenance evaluation of the cretaceous sedimentary record in the Upper Magdalena Valley Basin: implications in the Northern Andes Tectonic Evolution [Internet]. 2022 ;[citado 2026 mar. 12 ] Available from: https://repositorio.usp.br/directbitstream/a90b29e8-ae09-4d0c-8ea5-6e2062ebe773/3235682.pdf - Differentiating post-magmatic cooling and erosional exhumation in the thermochronological record of the northern Chilean Forearc (22.5° and 24.5° S)
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