Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4687681 | Geomorphology | 2006 | 12 Pages |
Abstract
The fault zone at the SE flank of the NDpr (Prokopi-Pelion fault zone) may be very important in terms of earthquake segmentation of the active NW-SE Dirfys fault zone that controls the Aegean coast of northern Evia, given that the intersection between the two presents striking morpho-structural similarities with the intersection of two fault zones with the same directions on the mainland (the Atalanti and Hyampolis fault zones), which is known to have acted as a barrier to the propagation of the Atalanti earthquake ruptures in 1894.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Nikolaos Palyvos, Ioannis Bantekas, Haralambos Kranis,