| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6433575 | Tectonophysics | 2015 | 4 Pages |
Abstract
â¢NE-trending Pliny-Strabo trench has envisaged being continued into Anatolia as strike-slip fault.â¢It is unproven by field map, kinematics, fault plane solutions of earthquakes and subsurface data.â¢SW Anatolia occupies an array of NE-trending extensional basins bounded by dip-slip faults.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
M. Cihat Alçiçek,