Information - SSP7 Cenozoic basin evolution and uplift of the Paratethys basin system (co-listed in TS)
Event Information
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
Co-Sponsorship
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.
Back