| Interpretıon Of The Analysıs Of Magnetıc And Gravıty Anomalıes Maps Of Gelıbolu Regıon By Usıng Wavelet Method
In this study, wavelet transform is used to identify tectonic structure of Gelibolu Region by using magnetic and gravity anomalies maps optained by TPAO. The success of wavelet method for determining the limit border edge and distinction between regional and residual maps are discussed. First of all, the wavelet method is applied to synthetic samples, after having good results, the method is applied to field data. In addition to the geological structures creating anomaly are modelled with the cross – sections captured on magnetic and gravity anomalies maps. The results are compared with the deep seismic cross sections taken on Gelibolu by TPAO (DG-158; DG-159) and tectonic structure of Gelibolu Peninsula is determined in detail. This study also show that determination a revese fault in this region. In addition to development a new tectonic map of Gelibolu Peninsula. We also say that the succes of wavelet transform for determining the limit border analyse.
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