Are Present-day Deformation and Seismicity in the Alps and the Pyrenees Examples of Super-slow Plate Boundary? Constraints from a New Analysis of GNSS Data.


Christine Masson1, Philippe Vernant2, Stephane Mazzotti3, Jean Chery4, Giorgi Khazaradze5 and Doerflinger Erik3, (1)Géosciences Montpellier, Montpellier, France, (2)Laboratoire Geosciences, Montpellier, France, (3)Géosciences Montpellier, Montpellier Cedex 05, France, (4)CNRS, Paris Cedex 16, France, (5)University of Barcelona, Department of Earth and Ocean Dynamics, Barcelona, Spain
Back to: Plate Motion, Continental Deformation, and Interseismic Strain Accumulation I