Dinis, Pedro A.; Fernandes, Paulo; Jorge, Raul C. G. S.; Rodrigues, Bruno; Chew, David M.; Tassinari, Colombo Celso Gaeta 
Source: Sedimentary Geology. Unidade: IGC
Subjects: GEOCRONOLOGIA, PANGÉA, PALEOGEOGRAFIA
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DINIS, Pedro A. et al. The transition from Pangea amalgamation to fragmentation: constraints from detrital zircon geochronology on West Iberia paleogeography and sediment sources. Sedimentary Geology, v. 375, p. 172-187, 2018Tradução . . Disponível em: https://doi.org/10.1016/j.sedgeo.2017.09.015. Acesso em: 04 jun. 2024.APA
Dinis, P. A., Fernandes, P., Jorge, R. C. G. S., Rodrigues, B., Chew, D. M., & Tassinari, C. C. G. (2018). The transition from Pangea amalgamation to fragmentation: constraints from detrital zircon geochronology on West Iberia paleogeography and sediment sources. Sedimentary Geology, 375, 172-187. doi:10.1016/j.sedgeo.2017.09.015NLM
Dinis PA, Fernandes P, Jorge RCGS, Rodrigues B, Chew DM, Tassinari CCG. The transition from Pangea amalgamation to fragmentation: constraints from detrital zircon geochronology on West Iberia paleogeography and sediment sources [Internet]. Sedimentary Geology. 2018 ; 375 172-187.[citado 2024 jun. 04 ] Available from: https://doi.org/10.1016/j.sedgeo.2017.09.015Vancouver
Dinis PA, Fernandes P, Jorge RCGS, Rodrigues B, Chew DM, Tassinari CCG. The transition from Pangea amalgamation to fragmentation: constraints from detrital zircon geochronology on West Iberia paleogeography and sediment sources [Internet]. Sedimentary Geology. 2018 ; 375 172-187.[citado 2024 jun. 04 ] Available from: https://doi.org/10.1016/j.sedgeo.2017.09.015
