Source: Journal of South American Earth Sciences. Unidade: IGC
Subjects: HIDROTERMALISMO, INTRUSÃO, ISÓTOPOS ESTÁVEIS
ABNT
SANTOS, Roberto Ventura et al. Hydrothermal alteration related to a deep mantle source controlled by a Cambrian intracontinental strike-slip fault: evidence for the Meruoca felsic intrusion associated with the Transbraziliano Lineament, Northeastern Brazil. Journal of South American Earth Sciences, v. 43, p. 33-41, 2013Tradução . . Disponível em: https://doi.org/10.1016/j.jsames.2012.12.005. Acesso em: 11 set. 2024.APA
Santos, R. V., Oliveira, C. G. de, Parente, C. V., Garcia, M. G. M., & Dantas, E. L. (2013). Hydrothermal alteration related to a deep mantle source controlled by a Cambrian intracontinental strike-slip fault: evidence for the Meruoca felsic intrusion associated with the Transbraziliano Lineament, Northeastern Brazil. Journal of South American Earth Sciences, 43, 33-41. doi:10.1016/j.jsames.2012.12.005NLM
Santos RV, Oliveira CG de, Parente CV, Garcia MGM, Dantas EL. Hydrothermal alteration related to a deep mantle source controlled by a Cambrian intracontinental strike-slip fault: evidence for the Meruoca felsic intrusion associated with the Transbraziliano Lineament, Northeastern Brazil [Internet]. Journal of South American Earth Sciences. 2013 ; 43 33-41.[citado 2024 set. 11 ] Available from: https://doi.org/10.1016/j.jsames.2012.12.005Vancouver
Santos RV, Oliveira CG de, Parente CV, Garcia MGM, Dantas EL. Hydrothermal alteration related to a deep mantle source controlled by a Cambrian intracontinental strike-slip fault: evidence for the Meruoca felsic intrusion associated with the Transbraziliano Lineament, Northeastern Brazil [Internet]. Journal of South American Earth Sciences. 2013 ; 43 33-41.[citado 2024 set. 11 ] Available from: https://doi.org/10.1016/j.jsames.2012.12.005