Molasse basins of Europe: a tectonic assessment

@inproceedings{Friend1985MolasseBO,
  title={Molasse basins of Europe: a tectonic assessment},
  author={Peter Furneaux Friend},
  year={1985}
}
Sedimentary basins are structures that formed either by subsidence of an area relative to its surroundings, or by uplift of the surroundings. The basin is defined by its sedimentary fill, and the vertical kinematics of the fill are reflected by stratal wedging, unconformities and, or, faulting. The following basin mechanisms are distinguished: locally (a) stretch, (b) thrust and piggy-back, (c) local uplift, and regionally (d) stretch-and-cool, (e) load-and-flex and (f) cratonic uplift. Basin… CONTINUE READING

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