The Tertiary geological history of Germany was mainly characterized by basin deposition in restricted tectonic settings, either as graben structures or as the molasse-filled foreland foredeep of the Alps. The most prominent basin structure of the Tertiary is the N-S...
CITATION STYLE
Meschede, M., & Warr, L. N. (2019). Tertiary Basins (pp. 209–231). https://doi.org/10.1007/978-3-319-76102-2_13
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