Determination of crustal structure beneath the Çameli Basin (SW Turkey) using an aeromagnetic data

Year 2022, Volume: 18 Issue: 2, 31 - 40, 31.12.2022

Fahriye Akar , Funda Bilim

Abstract

The Çameli basin is situated at the southwestern Anatolia (Turkey), where is tectonically a very active region. The reduction to the pole (RTP), the upward continuation and the analytic signal (AS) methods were used in this study to determine the tectonic lineaments/bodies caused magnetic anomaly beneath the Çameli basin. The results show that the deep-seated magnetic bodies (at least 5 km deep) are possibly emplaced in the upper crust along the NE-SW trending faults. The AS map indicates that many of the causative sources appear elliptical shaped in the study.

Keywords

The Çameli Basin, Magnetic Anomaly, the Reduction to Pole (RTP), the Upward Continuation, the Analytic Signal (AS).

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