In the last fifty years, the Messinian Salinity Crisis (MSC) has been widely investigated in the Mediterranean Sea, but a major basin remains fewly explored in terms of MSC thematic: the Western Tyrrhenian Basin. The rifting of this back-arc basin is considered to occur between the Middle-Miocene and the Early-Pliocene, thus including the MSC,...
-
April 1, 2018 (v1)Journal articleUploaded on: December 4, 2022
-
2018 (v1)Book section
International audience
Uploaded on: December 4, 2022 -
December 15, 2014 (v1)Conference paper
International audience
Uploaded on: December 4, 2022 -
2018 (v1)Book section
International audience
Uploaded on: December 4, 2022 -
December 2, 2021 (v1)Journal article
The Algerian continental margin in the western Mediterranean formed as a back-arc basin and is today reactivated by the convergence between the African and Eurasian plates. It is one of the very rare examples of passive margins undergoing inversion expressed in a moderate seismicity of the margin and is possibly giving way for future...
Uploaded on: December 3, 2022