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  Information - SSP26 Cenozoic basin evolution and uplift of the Eastern Alps and the Pannonian basin (co-listed in TS)

Event Information
The Cenozoic, especially the Neogene, constitutes the final stage of
development of the Eastern 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, sedimentology and paleontology of
basin fills, and the interplay of exhumation, uplift, erosion and deposition
are highly welcome.

Preliminary List of Solicited Speakers


General Statement
The information contained hereafter has been compiled and uploaded by the Session Organizers via the "Organizer Session Form". The Session Organizers have therefore the sole responsibility that this information is true and accurate at the date of publication, and the conference organizer cannot accept any legal responsibility for any errors or omissions that may be made, and he makes no warranty, expressed or implied, with regard to the material published.

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