TURKISH JOURNAL OF EARTH SCIENCES, cilt.17, sa.4, ss.653-672, 2008 (SCI-Expanded)
Central Anatolia, located on the immense Alpine-Himalayan orogenic belt, has a complicated neotectonic evolution, and NE-SW-trending Neogene horsts-graben systems that rejuvenate pre-existing palaeostructures are among the most important structures which help us understand the tectonic evolution of Central Anatolia.