
View from the eastern margin of the Nigde Massif, across the basement-basin contact, the Central Anatolian(Ecemis) fault, and the Tauride Mountains (Aladag).
|
Evolution of continental lithosphere from collision to escape: the record in the rocks and landscape of Central Anatolia
Our group has been working in central and western Turkey, using the well-exposed rocks and structures to understand metamorphic and deformation processes in different tectonic regimes. In central Turkey, metamorphic rocks are exhumed adjacent to a major strike-slip fault, the Central Anatolian fault zone (CAFZ). This structure pre-dates the more famous and seismically active North Anatolian fault, and oblique motion related to the CAFZ is recorded in exhumed mid-crustal orogenic rocks adjacent to the fault. Our research group has worked out the history of vertical motion related to the fault over the past ~90 million years, but there are interesting questions unresolved about the later vertical vs. lateral motion of this and other intracontinental strike-slip faults.
People: Erkan Toraman, Lauren Idleman, Christian Teyssier, Donna Whitney, Paul Umhoefer (NAU)
|