Cretaceous extensional and contractional stages in the Colombian Andes unraveled by a source-to-sink geochronological and thermochronological study in the Upper Magdalena Basin (2024)
- Authors:
- Autor USP: AMEZQUITA, MAURICIO PARRA - IGC
- Unidade: IGC
- DOI: 10.1016/j.tecto.2024.230303
- Subjects: TERMOCRONOLOGIA; EVOLUÇÃO TECTÔNICA; CRETÁCEO
- Agências de fomento:
- Language: Inglês
- Imprenta:
- Publisher: Elsevier BV
- Date published: 2024
- Source:
- Título: Tectonophysics
- ISSN: 0040-1951
- Volume/Número/Paginação/Ano: v. 878, n. , p. 230303-, May 2024
- Este periódico é de acesso aberto
- Este artigo NÃO é de acesso aberto
-
ABNT
CALDERON-DIAZ, Laura Cristina et al. Cretaceous extensional and contractional stages in the Colombian Andes unraveled by a source-to-sink geochronological and thermochronological study in the Upper Magdalena Basin. Tectonophysics, v. 878, n. , p. 230303-, 2024Tradução . . Disponível em: https://doi.org/10.1016/j.tecto.2024.230303. Acesso em: 22 fev. 2026. -
APA
Calderon-Diaz, L. C., Zapata, S., Cardona, A., Parra, M., Sobel, E., Patiño, A. M., et al. (2024). Cretaceous extensional and contractional stages in the Colombian Andes unraveled by a source-to-sink geochronological and thermochronological study in the Upper Magdalena Basin. Tectonophysics, 878( ), 230303-. doi:10.1016/j.tecto.2024.230303 -
NLM
Calderon-Diaz LC, Zapata S, Cardona A, Parra M, Sobel E, Patiño AM, Valencia VA, Jaramillo-Rios JS, Glodny J. Cretaceous extensional and contractional stages in the Colombian Andes unraveled by a source-to-sink geochronological and thermochronological study in the Upper Magdalena Basin [Internet]. Tectonophysics. 2024 ; 878( ): 230303-.[citado 2026 fev. 22 ] Available from: https://doi.org/10.1016/j.tecto.2024.230303 -
Vancouver
Calderon-Diaz LC, Zapata S, Cardona A, Parra M, Sobel E, Patiño AM, Valencia VA, Jaramillo-Rios JS, Glodny J. Cretaceous extensional and contractional stages in the Colombian Andes unraveled by a source-to-sink geochronological and thermochronological study in the Upper Magdalena Basin [Internet]. Tectonophysics. 2024 ; 878( ): 230303-.[citado 2026 fev. 22 ] Available from: https://doi.org/10.1016/j.tecto.2024.230303 - 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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Informações sobre o DOI: 10.1016/j.tecto.2024.230303 (Fonte: oaDOI API)
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