Abstract: Evidence for dynamic relationship between faulting and Neogene-Quaternary volcanism in post-collisional Central Anatolia (Turkey): Implications for shallow slab subduction and rollback. (AGU Fall Meeting 2018)

Evidence for dynamic relationship between faulting and Neogene-Quaternary volcanism in post-collisional Central Anatolia (Turkey): Implications for shallow slab subduction and rollback.

W. Kirk Schleiffarth¹, Paul J Umhoefer², Michael A Cosca³, Mary R Reid², Jonathan R Delph⁴, Daniel Evan Portner⁵, Susan L Beck⁶, Bizhan Abgarmi⁷ and Arda Özacar⁷, (1)Northern Arizona University, School of Earth Sciences and Environmental Sustainability, Flagstaff, AZ, United States, (2)Northern Arizona Univ, Flagstaff, AZ, United States, (3)USGS, Denver, CO, United States, (4)Purdue University, Earth, Atmospheric, and Planetary Sciences, West Lafayette, IN, United States, (5)University of North Carolina at Chapel Hill, Olney, United States, (6)University of Arizona, Department of Geosciences, Tucson, AZ, United States, (7)Middle East Technical University, Ankara, Turkey

Back to: Postcollisional Extensional Tectonics and Basin Evolution in the Gulf of Mexico and Elsewhere I