Diachronous uplift and cooling history of the Menderes core complex, western Anatolia (Turkey), based on new Zircon (U-Th)/He ages

作者：Baran Zeynep Oner^*; Dilek Yildirim; Stockli Daniel

来源：Tectonophysics, 2017, 694: 181-196.

DOI：10.1016/j.tecto.2016.12.005

• Menderes Massif
• Alasehir detachment
• Exhumation
• Cooling rates
• (U-Th)/He thermochronology
• Cenozoic extension

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 12.5 km/Myr along the Alasehir detachment (similar to 14 degrees dip angle) and denudation rates between 1.75 km/Myr and 325 km/Myr between 4 Ma and 2 Ma. These values suggest relatively fast exhumation of the Central sub-massif, associated with cooling rates between 53 degrees C/Myr and 128 degrees C/Myr, which are higher than the estimated footwall cooling rates (60 degrees C/Myr to 120 degrees C/Myr) from the Northern sub-massif. Based on the initial crystallization ages of the syn-extensional granitoid intrusions and their exhumation-related cooling ages, our thermochronological findings suggest that the Central sub-massif in Menderes underwent accelerated uplift and faster exhumation in the latest Cenozoic than the Northern and Southern sub-massifs. This latest doming and rapid extension of the Central sub-massif was associated with the asthenospheric upwelling beneath the region and the related Na-alkaline, Kula volcanism. Our results indicate that the Menderes Massif has had a diachronous uplift and cooling history during its extensional tectonic evolution in the late Cenozoic Thermal Weakening of the young orogenic crust in western Anatolia via both lithospheric and asthenospheric melting episodes and magmatism produced higher than normal geothermal gradients and played a significant role in core complex formation. Published by Elsevier B.V.

• 出版日期2017-1-2