Abstract: Decoupled Upper and Lower Crustal Deformation Mechanisms in the Pamir Mountains: Implications for Lower Crustal Flow in Orogenic Plateaus (2016 AGU Fall Meeting)

Decoupled Upper and Lower Crustal Deformation Mechanisms in the Pamir Mountains: Implications for Lower Crustal Flow in Orogenic Plateaus

James Chapman¹, Alexander C Robinson², Barbara Carrapa³, Paul A Kapp⁴, James Worthington¹, Dustin Patrick Villarreal², Mustafo Gadoev⁵ and Ilhomjon Oimahmadov⁵, (1)University of Arizona, Tucson, AZ, United States, (2)University of Houston, Department of Earth and Atmospheric Sciences, Houston, TX, United States, (3)University of Arizona, Geosciences, Tucson, United States, (4)University of Arizona, Department of Geosciences, Tucson, AZ, United States, (5)Earthquake Enginering and Seismology, Academy of the Republic of Tajikistan, Institute of Geology, Dushanbe, Tajikistan

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