Information - SSP7 Cenozoic basin evolution and uplift of the Paratethys basin system (co-listed in TS)
The Cenozoic constitutes the final stage of
development of the Alps, and crustal deformation was synchronous to
the formation and filling of sedimentary basins. Exhumation/uplift of rocks
and climatic feedbacks influenced not only Neogene basin fills but also
biota in the Paratethys and the Mediterranean. Contributions to Cenozoic
basin formation, source terrain evolution, stratigraphy, sedimentology and paleontology of basin fills, and the interplay of exhumation, uplift, erosion and deposition are highly welcome.
Preliminary List of Solicited Speakers
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