W. K. Schleiffarth
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View article: The Seismic Expression and Tectonomagmatic Evolution of Subduction Termination along the Anatolian Margin 
The Seismic Expression and Tectonomagmatic Evolution of Subduction Termination along the Anatolian Margin  Open
The geological expression of subduction termination is poorly understood due to overprinting during the collisional stage of the Wilson Cycle. The Anatolian domain of the eastern Mediterranean represents a modern system where spatial varia…
View article: Melt equilibration depths as sensors of lithospheric thickness during Eurasia-Arabia collision and the uplift of the Anatolian Plateau
Melt equilibration depths as sensors of lithospheric thickness during Eurasia-Arabia collision and the uplift of the Anatolian Plateau Open
A co-investigation of mantle melting conditions and seismic structure revealed an evolutionary record of mantle dynamics accompanying the transition from subduction to collision along the Africa-Eurasia margin and the >1 km uplift of the A…
View article: Dynamics of episodic Late Cretaceous–Cenozoic magmatism across Central to Eastern Anatolia: New insights from an extensive geochronology compilation
Dynamics of episodic Late Cretaceous–Cenozoic magmatism across Central to Eastern Anatolia: New insights from an extensive geochronology compilation Open
We compiled geochronology data from 87 published studies within the Anatolia orogen (32.5°E–44°E) to investigate the spatial and temporal patterns of continental magmatism during the final stages of Neotethys Ocean closure. The number and …
View article: Shallow melting of <scp>MORB</scp>‐like mantle under hot continental lithosphere, <scp>C</scp>entral <scp>A</scp>natolia
Shallow melting of <span>MORB</span>‐like mantle under hot continental lithosphere, <span>C</span>entral <span>A</span>natolia Open
Widespread mafic volcanism, elevated crustal temperatures, and plateau‐type topography in Central Anatolia, Turkey, could collectively be the result of lithospheric delamination, mantle upwelling, and tectonic escape. We use results from 4…