A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas
ABNT
SRIVASTAVA, Priyeshu et al. Red clays indicate sub‑aerial exposure of the Rio Grande Rise during the Eocene volcanic episode. Scientific Reports, v. 13, p. 01-13, 2023Tradução . . Disponível em: http://dx.doi.org/10.1038/s41598-023-46273-y. Acesso em: 17 nov. 2024.
APA
Srivastava, P., Murton, B. J., Sant`Anna, L. G., Florindo, F., Hassan, M. B., Guerra, J. T. M., et al. (2023). Red clays indicate sub‑aerial exposure of the Rio Grande Rise during the Eocene volcanic episode. Scientific Reports, 13, 01-13. doi:10.1038/s41598-023-46273-y
NLM
Srivastava P, Murton BJ, Sant`Anna LG, Florindo F, Hassan MB, Guerra JTM, Janasi V de A, Jovane L. Red clays indicate sub‑aerial exposure of the Rio Grande Rise during the Eocene volcanic episode [Internet]. Scientific Reports. 2023 ; 13 01-13.[citado 2024 nov. 17 ] Available from: http://dx.doi.org/10.1038/s41598-023-46273-y
Vancouver
Srivastava P, Murton BJ, Sant`Anna LG, Florindo F, Hassan MB, Guerra JTM, Janasi V de A, Jovane L. Red clays indicate sub‑aerial exposure of the Rio Grande Rise during the Eocene volcanic episode [Internet]. Scientific Reports. 2023 ; 13 01-13.[citado 2024 nov. 17 ] Available from: http://dx.doi.org/10.1038/s41598-023-46273-y
A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas
ABNT
SAVIAN, Jairo F et al. The Barremian-Aptian boundary in the Poggio le Guaine core (central Italy): evidence for magnetic polarity Chron M0r and oceanic anoxic event 1a. The stratigraphic record of Gubbio: integrated stratigraphy of the late Cretaceous-Paleogene Umbria-Marche Pelagic Basin. Tradução . Boulder, CO: The Geological Society of America, 2016. . Disponível em: https://doi.org/10.1130/2016.2524(05). Acesso em: 17 nov. 2024.
APA
Savian, J. F., Trindade, R. I. F. da, Janikian, L., Jovane, L., Almeida, R. P. de, Coccioni, R., et al. (2016). The Barremian-Aptian boundary in the Poggio le Guaine core (central Italy): evidence for magnetic polarity Chron M0r and oceanic anoxic event 1a. In The stratigraphic record of Gubbio: integrated stratigraphy of the late Cretaceous-Paleogene Umbria-Marche Pelagic Basin. Boulder, CO: The Geological Society of America. doi:10.1130/2016.2524(05)
NLM
Savian JF, Trindade RIF da, Janikian L, Jovane L, Almeida RP de, Coccioni R, Frontalini F, Sideri M, Figueiredo M, Tedeschi LR, Jenkyns HC. The Barremian-Aptian boundary in the Poggio le Guaine core (central Italy): evidence for magnetic polarity Chron M0r and oceanic anoxic event 1a [Internet]. In: The stratigraphic record of Gubbio: integrated stratigraphy of the late Cretaceous-Paleogene Umbria-Marche Pelagic Basin. Boulder, CO: The Geological Society of America; 2016. [citado 2024 nov. 17 ] Available from: https://doi.org/10.1130/2016.2524(05)
Vancouver
Savian JF, Trindade RIF da, Janikian L, Jovane L, Almeida RP de, Coccioni R, Frontalini F, Sideri M, Figueiredo M, Tedeschi LR, Jenkyns HC. The Barremian-Aptian boundary in the Poggio le Guaine core (central Italy): evidence for magnetic polarity Chron M0r and oceanic anoxic event 1a [Internet]. In: The stratigraphic record of Gubbio: integrated stratigraphy of the late Cretaceous-Paleogene Umbria-Marche Pelagic Basin. Boulder, CO: The Geological Society of America; 2016. [citado 2024 nov. 17 ] Available from: https://doi.org/10.1130/2016.2524(05)