Journal
TERRA NOVA
Volume 13, Issue 4, Pages 281-288Publisher
WILEY
DOI: 10.1046/j.1365-3121.2001.00355.x
Keywords
-
Categories
Ask authors/readers for more resources
The Tertiary deformation of the Iberian plate is here interpreted as the result of changes in the coupling between the IberianAfrican plates. During the early stages of the Africa/Iberia subduction (Palaeocene), deformation was confined at the Betic plate boundary. From the Eocene, during the collision in the southern plate margin, compressional deformation delocalized and distributed throughout the Iberian plate. First, in the Pyrenees, where the main stage of thrusting occurred during the Late Eocene - Early Oligocene. Then (mainly Oligocene - Late Miocene), in the inner part of the Iberian plate, forming basement uplifts in the Iberian Chain and the Central System, in correspondence of pre-existing (Mesozoic and Variscan) structures. Finally, during the decay of compression inside the Iberian plate, extension took place the Mediterranean margin and the Alboran Sea.
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available