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Assessment of Vertical Magnetic Gradient Data of Tuzla Fault Using Boundary Analysis and 3 D Inversion Techniques

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Figure

Figure 1. Location of the study area, indicated with black rectangle (not to scale).
Figure 2. Locations of active faults in Izmir. Study area is indicated with red rectangle (not to scale)
Figure 3. Geologic map of the Seferihisar geothermal region (after [31] and [34]).
Figure 4. Location of grid intersections used to test for a maximum near G i j(,  )and 8 neighbour points (modified
+4

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