Abstract
The Thrace Basin which is a geological and geographical feature located in southeastern Europe, is the largest and thickest Cenozoic sedimentary basin in Turkey. Various geophysical methods have been used to investigate the basin's properties, tectonic evolution and gain insights into its formation. Within the contexts we applied receiver function method to provide insights on the crustal thicknesses and Vp/Vs ratio beneath Thrace Basin. More than 100 events with magnitudes greater than 6.3 recorded between 2007 and 2022 are evaluated and crustal thickness and Vp/Vs ratio are inferred from H-k analysis. Due to a thick sedimentary fill the average Moho depth is ∼30 km and the average Vp/Vs ratio is ∼1.77 in the Thrace basin which are consistent with the previous studies.
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