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This research paper investigates Fault Zone Head Waves (FZHW) along the Ganos Fault in northwestern Türkiye, focusing on data collected from the MONGAN seismic network. The study identifies a bimaterial interface across the fault, with an estimated velocity contrast of 5.9%, and suggests that future earthquake ruptures will predominantly progress westward, impacting seismic risk assessments. The findings also allow for revisions of previous focal mechanisms for regional earthquakes by distinguishing FZHW fr

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