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The geology map of study area (modified after Ulutürk, 2009).

The geology map of study area (modified after Ulutürk, 2009).

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Figure 1. Geothermal fields in Afyonkarahisar.
Figure 2. The geology map of study area (modified after Ulutürk, 2009).
Figure 3: Oyuklu Tepe marbles; (a): General view of the abandoned...
Figure 4. Different alteration zones observed in Oyuklu Tepe marbles....
+5 Figure 5. Primary calcite crystals (Ka), secondary muscovite (Mu) and...
The Mineropetrographic and Geochemical Properties of Reservoir Rocks (Ömer-Gecek/ Afyonkarahisar Geothermal Field)
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Full-text available
  • Jun 2020
The most important elements of the geothermal system are fluid, reservoir-cover rock, heat source, and fault lines. In geothermal basins, it is necessary to have a reservoir rock of sufficient thickness with high porosity and permeability. This study aims to determine the mineralogic-petrographic and geochemical features of the marbles, which are t...
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Context 1
... Upper Miocene Erkmen volcanics are the last products of volcanism in the region. Quaternary travertine and alluvium are the youngest units in the study area (Figure 2). ...
Context 2
... the study area, the effectiveness of hydrothermal alteration, which is related to geothermal waters, is monitored intensively in two regions. The first is between Ömer-Gecek and Köprülü Village, and the other is between Erkmen own and Çakırköy (Figure 2). The distribution of the alteration zones is fracture controlled and is in line with the direction of major faults in the region. ...
Context 3
... Upper Miocene Erkmen volcanics are the last products of volcanism in the region. Quaternary travertine and alluvium are the youngest units in the study area (Figure 2). ...
Context 4
... the study area, the effectiveness of hydrothermal alteration, which is related to geothermal waters, is monitored intensively in two regions. The first is between Ömer-Gecek and Köprülü Village, and the other is between Erkmen own and Çakırköy (Figure 2). The distribution of the alteration zones is fracture controlled and is in line with the direction of major faults in the region. ...

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Crystallinity index of quartz for the peak 778 cm -1
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In the present work, rock samples have been collected from Paleolithic archaeological site Attirampakkam, Tamil Nadu, India to assess the presence of mineralogical composition of samples using Fourier Transform infrared-spectroscopic (FT-IR) technique and these identified minerals are confirmed by using X-Ray Diffraction (XRD) technique. From FT-IR...
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