Abstract:The Menderes Massif, located at Western Anatolia, Turkey, is a wide area that is under an extensional regime, resulting in the area having large grabens along with many faults and being geothermally rich. Due to having a large number of linear structures, the Menderes Massif has been a popular area for boundary analysis studies using gravity and magnetic prospecting. Since both prospecting methods result in potential field anomalies that are directly related to the positions of the anomaly sources, boundary an… Show more
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