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Autor:
L. J. Calliari, C. A. E. Garcia, L. F. Niencheski, G. Fillmann, U. Seeliger, N. M. Gianuca, P. C. Abreu, C. Odebrecht, V. M. T. Garcia, M. Montú, I. M. Gloeden, A. K. Duarte, C. Resgalla, R. R. Capítoli, C. Sinque, J. H. Muelbert, J. P. Castello, M. Haimovici, G. Phonlor, J. C. B. Cousin, C. M. Vooren, M. C. Pinedo, J. A. Levy
Publikováno v:
Subtropical Convergence Environments ISBN: 9783642644184
The southern Brazilian continental margin is characteristic of low intensity tectonic evolution processes (Villwock 1987), which levelled the basement, formed thick sedimentary layers, and led to the development of an extensive coastal plain (Fig. 6.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::757af1f6ae3dd5541d6a7aa5e3a5cb8a
https://doi.org/10.1007/978-3-642-60467-6_6
https://doi.org/10.1007/978-3-642-60467-6_6