1887

Abstract

Summary

The main purpose of this study is to evaluate the gravity data of the Bergama-Dikili geothermal field. Bergama-Dikili region is an important region with great preliminaries from the antiquity in terms of geothermal. Therefore, it is a great importance also in the future. Considering these circumstances, the importance of determination of some parameters such as geological boundaries and depths is increased. In this study, gravity data were interpreted for defining geological structures. Filtering process, upward and downward continuations, second derivation, trend analysis, boundary analysis and power spectrum methods were utilized during the evaluation of data. Besides, the calculated basement depth values with using 3D modeling were mapped.

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/content/papers/10.3997/2214-4609.201702571
2017-11-05
2024-04-25
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