Sage, F., Beslier, M.-O., Thinon, I., Larroque, C., Dessa, J.-X., Migeon, S., Angelier, J., Guennoc, P., Schreiber, D., Michaud, F., Stephan, J.-F. and Sonnette, L. (2011) Structure And Evolution of a Passive Margin in a Compressive Environment: Example of the South-Western Alps-Ligurian Basin Junction during the Cenozoic. Marine Petroleum Geology, 28, 1263-1282.
https://doi.org/10.1016/j.marpetgeo.2011.03.012

has been cited by the following article:

• TITLE: Seismotectonics of the Padanian Region and Surrounding Belts: Which Driving Mechanism?

  AUTHORS: Marcello Viti, Enzo Mantovani, Daniele Babbucci, Caterina Tamburelli, Nicola Cenni

  KEYWORDS: Seismotectonics, Geodynamics, GPS, Mediterranean, Padanian

  JOURNAL NAME: International Journal of Geosciences, Vol.7 No.12, December 29, 2016

  ABSTRACT: It is argued that the complex tectonic pattern observed in the study area can plausibly be explained as an effect of the kinematics of the Iberia and Adria blocks, induced by the NNE ward motion of Africa and the roughly westward motion of the Anatolian-Aegean system with respect to Eurasia. These boundary conditions cause the constrictional regime which is responsible for the observed shortening processes in the Padanian region and Western Alps. The proposed dynamic context can plausibly account for the peculiar distribution of major seismic sources, located in the northern Apennines, the Giudicarie fault system, the offshore of the western Ligurian coast and the Swiss Alps. The observed tectonic pattern in Western Europe and the study area can hardly be reconciled with the implications of the roughly NWward convergence between Africa and Eurasia proposed by global kinematic models, whereas it is compatible with the alternative Africa-Eurasia kinematics and plate mosaic proposed by [1].