Source: Lithos. Unidades: IGC, IAG
Subjects: GEOCRONOLOGIA, PALEOMAGNETISMO
ABNT
TEIXEIRA, Wilson et al. U–Pb (ID-TIMS) baddeleyite ages and paleomagnetism of 1.79 and 1.59 Ga tholeiitic dyke swarms, and position of the Rio de la Plata Craton within the Columbia supercontinent. Lithos, v. 174, p. 157-174, 2013Tradução . . Disponível em: https://doi.org/10.1016/j.lithos.2012.09.006. Acesso em: 23 ago. 2024.APA
Teixeira, W., D'Agrella Filho, M. S., Hamilton, M. A., Ernst, R. E., Girardi, V. A. V., Mazzucchelli, M., & Bettencourt, J. S. (2013). U–Pb (ID-TIMS) baddeleyite ages and paleomagnetism of 1.79 and 1.59 Ga tholeiitic dyke swarms, and position of the Rio de la Plata Craton within the Columbia supercontinent. Lithos, 174, 157-174. doi:10.1016/j.lithos.2012.09.006NLM
Teixeira W, D'Agrella Filho MS, Hamilton MA, Ernst RE, Girardi VAV, Mazzucchelli M, Bettencourt JS. U–Pb (ID-TIMS) baddeleyite ages and paleomagnetism of 1.79 and 1.59 Ga tholeiitic dyke swarms, and position of the Rio de la Plata Craton within the Columbia supercontinent [Internet]. Lithos. 2013 ; 174 157-174.[citado 2024 ago. 23 ] Available from: https://doi.org/10.1016/j.lithos.2012.09.006Vancouver
Teixeira W, D'Agrella Filho MS, Hamilton MA, Ernst RE, Girardi VAV, Mazzucchelli M, Bettencourt JS. U–Pb (ID-TIMS) baddeleyite ages and paleomagnetism of 1.79 and 1.59 Ga tholeiitic dyke swarms, and position of the Rio de la Plata Craton within the Columbia supercontinent [Internet]. Lithos. 2013 ; 174 157-174.[citado 2024 ago. 23 ] Available from: https://doi.org/10.1016/j.lithos.2012.09.006