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New (U-Th)/He thermochronology data from the syn-extensional granitoids in the central part of the Menderes Massif in western Turkey reveal a minimum slip rate of 12.5km/Myr along the Alasehir detachment (~14° dip angle) and denudation rates between 1.75km/Myr and 3.25km/Myr between 4Ma and 2Ma. These values suggest relatively fast exhumation of the Central sub-massif, associated with cooling rates...
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