Anatolian Plateau Uplift Along the Southern Central Margin from Structural Analysis, CRN Dating, and Low-Temperature Thermochronology (original) (raw)

Abstract

Bounding flanks of orogenic plateaus are among the most sensitive features for recording the tectonic drivers for and geomorphic responses to surface uplift. Here, processes from the base of the lithosphere to the surface of the crust are integrated in the geologic record, providing key constraints for deciphering the geodynamic processes that drive orogen growth. The southern margin of the

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