Abstract:Refraction microtremor (ReMi™) technique is one of the most effective techniques to obtain near-subsurface average shear wave velocity structure. This technique was used to delineate the subsurface structure of the Plio-Quaternary sediments deposited on the limestone bedrock. Transect data were collected at 130 points along the N-S profile at the northern part of the Isparta basin with a 20-m interval. The seismic velocity-depth models were produced from these data separately, and then, 2D seismic section was … Show more
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