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• W2146244036 abstract "Metamorphic studies in the cover sequences of the Bitlis complex allow the thermal evolution of the massif to be constrained using metamorphic index minerals. Regi onally distributed metamorphic index minerals such as glaucophane, carpholite, relics of carpholite in chloritoid-bearing schists and pseudomorphs aft er aragonite in marbles record a LT-HP evolution. Th that the Bitlis complex was subducted and stacked to form a nappe complex during the closure of the Neo-Tethys. During late Cretaceous to Cenozoic evolution the Bitlis complex experienced peak metamorphism of 1.0-1.1 GPa at 350-400°C. During the retrograde evolution temperatures remained below 460°C. 39 Ar/ 40 Ar dating of white mica in diff erent parageneses from the Bitlis complex reveals a 74-79 Ma (Campanian) date of peak metamorphism and rapid exhumation to an almost isothermal greenschist stage at 67-70 Ma (Maastrichtian). Th e HP Eocene fl ysch escaped the greenschist facies stage and were exhumed under very cold conditions. Th ese single stage evolutions contrast with the multistage evolution reported further north from the Amassia-Stepanavan Suture in Armenia. Petrological investigations and isotopic dating sho w that the collision of Arabia with Eurasia resulted in an assemblage of diff erent blocks derived from the northern as well as from the southern plate and a set of subduction zones producing HP rocks with diverse exhumation histories." @default.
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• W2146244036 date "2012-01-01" @default.
• W2146244036 modified "2023-09-28" @default.
• W2146244036 title "Dating Subduction Events in East Anatolia, Turkey" @default.
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