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

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• 作者：Zeynep Oner Baran^a ; ^{zeynep.baran@sdsmt.edu} ; Yildirim Dilek^b ; Daniel Stockli^c
• 关键词：Menderes Massif ; Alasehir detachment ; Exhumation ; Cooling rates ; (U-Th)/He thermochronology ; Cenozoic extension
• 刊名：Tectonophysics
• 出版年：2017
• 出版时间：2 January 2017
• 年：2017
• 卷：694
• 期：Complete
• 页码：181-196
• 全文大小：3208 K
• 卷排序：694

文摘

Faster exhumation and higher cooling rates of the Central Menderes A minimum slip rate of 12.5 km/myr along the Alasehir detachment (~14 ° dip angle) The denudation rates between 1.75 km/myr and 3.25 km/myr between 4 Ma and 2 Ma Cooling rates of the central sub-massif between 53 °C/myr and 128 °C/myr Menderes Massif has had a diachronous uplift and cooling history