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Autor:
E. Salomon, A. Rotevatn, T. B. Kristensen, S.-A. Grundvåg, G. A. Henstra, A. N. Meckler, R. Albert, A. Gerdes
Publikováno v:
Solid Earth, Vol 11, Pp 1987-2013 (2020)
In marine rift basins, deep-water clastics (>200 m) in the hanging wall of rift- or basin-bounding fault systems are commonly juxtaposed against crystalline “basement” rocks in the footwall. A distinct feature of such fault systems is therefore
Externí odkaz:
https://doaj.org/article/f2f6b66475ee439a9e987182a1ac3fad
