GEOPHYSICAL JOURNAL INTERNATIONAL, vol.108, no.2, pp.589-588, 1992 (Journal Indexed in SCI)
It is now widely accepted that the rapid extension observed in western Turkey is mainly accommodated by large active normal faults which control the geomorphology. The NE-SW trending Burdur, Acigol and Baklan basins bounded by large faults form a system of half-graben whose orientation is evident in both the topography and the tilting of Neogene sediments adjacent to them.