In the next stage, we will make an inference using active fault and geological information. In this blog post, it was thought that proximity to the fault would increase the thermal source potential and a scenario was studi in which proximity to the strike-slip faults in our study area would be suitable for high potential as a fault type.
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In our geology map where we made age and lithology grouping, we saw the places with high potential in blue and the places with low potential in r, we cannot yet make an inference to evaluate the proximity to the active fault in this symbology display. Therefore, a numerical classification is requir in the group data. In the classification, the number of classes in the geology group layer was us and a rating was made between 1-10. You can see that the dark green and green color areas are the places where Tertiary, Quaternary and lithological information volcanic rocks are locat as desir.
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Tertiary – Volcanic and simentary rocks: Most suitable.
Quaternary – Alluvial and young volcanic areas: Very suitable.
Mesozoic – Carbonate rocks: Moderately suitable.
Paleozoic – Metamorphic rocks: Low suitability.
Precambrian – Massive crystalline rocks: Least suitable.
Following these assessments, potential geothermal areas were mapp. Thus, according to the first stage, geological data, we can see the areas with high potential in blue and the areas with low potential in r.
