Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4686730 | Geomorphology | 2009 | 9 Pages |
Abstract
All these allowed us to obtain rates of 0.3Â mm/yr for the regional component of uplift and 0.1Â mm/yr for the vertical slip movements of the Ierapetra fault. Based on the obtained rates and the existence of coastal archaeological Roman ruins it is concluded that Ierapetra fault should have been reactivated sometime after the Roman period.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
K. Gaki-Papanastassiou, E. Karymbalis, D. Papanastassiou, H. Maroukian,