Disruption of the Hellenic arc: Late Miocene extensional detachment faults and steep Pliocene-Quaternary normal faults-Or what happened at Corinth?
Author:
Affiliation:
1. Department of Geology; University of Athens; Athens; Greece
2. Department of Earth, Atmospheric, and Planetary Sciences; Massachusetts Institute of Technology; Cambridge; Massachusetts; USA
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Reference78 articles.
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3. Quaternary evolution of the Cornith Rift and its implications for the late Cenozoic evolution of the Aegean;Armijo;Geophys. J. Int.,1996
4. Westward propagation of the North Anatolian Fault into the northern Aegean: Timing and kinematics;Armijo;Geology,1999
5. Analysis of eleven years of deformation measured by GPS in the Corinth Rift Laboratory area;Avallone;C. R. Geosci.,2004
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