Source: Antarctic Science. Unidades: EACH, IGC
Subjects: PALEOCLIMATOLOGIA, PALEOGEOGRAFIA
ABNT
ROCHA-CAMPOS, A. C. et al. A (tidal-marine) boulder pavement in the late cenozoic of seymour Island, west antarctica: contribution to the palaeogeographical and palaeoclimatic evolution of west antarctica. Antarctic Science, v. 29, n. 6, p. 555-559, 2017Tradução . . Disponível em: https://doi.org/10.1017/S0954102017000335. Acesso em: 05 nov. 2024.APA
Rocha-Campos, A. C., Kuchenbecker, M., Duleba, W., Santos, P. R. dos, & Canile, F. M. (2017). A (tidal-marine) boulder pavement in the late cenozoic of seymour Island, west antarctica: contribution to the palaeogeographical and palaeoclimatic evolution of west antarctica. Antarctic Science, 29( 6), 555-559. doi:10.1017/S0954102017000335NLM
Rocha-Campos AC, Kuchenbecker M, Duleba W, Santos PR dos, Canile FM. A (tidal-marine) boulder pavement in the late cenozoic of seymour Island, west antarctica: contribution to the palaeogeographical and palaeoclimatic evolution of west antarctica [Internet]. Antarctic Science. 2017 ; 29( 6): 555-559.[citado 2024 nov. 05 ] Available from: https://doi.org/10.1017/S0954102017000335Vancouver
Rocha-Campos AC, Kuchenbecker M, Duleba W, Santos PR dos, Canile FM. A (tidal-marine) boulder pavement in the late cenozoic of seymour Island, west antarctica: contribution to the palaeogeographical and palaeoclimatic evolution of west antarctica [Internet]. Antarctic Science. 2017 ; 29( 6): 555-559.[citado 2024 nov. 05 ] Available from: https://doi.org/10.1017/S0954102017000335