Dergiler / Maden Tetkik ve Arama Dergisi / 2026 / Cilt: 170 Sayı: 170

Evaporate salt exploration by two dimensional (2D) seismic reflection method: Ankara- Polatlı region, Türkiye

Recep Güney(General Directorate of Mineral Research and Exploration, Department of Geophysical Studies, Ankara)0000-0002-0732-4759
Zeynep Rezzan Özerk(General Directorate of Mineral Research and Exploration, Department of Geophysical Studies, Ankara)0000-0003-4360-0375
Erdener Izladı(General Directorate of Mineral Research and Exploration, Department of Geophysical Studies, Ankara)0000-0002-9164-0294
Salih Erden(General Directorate of Mineral Research and Exploration, Western Black Sea Regional Directorate, Zonguldak)0000-0001-6941-2562
Esra Ak(General Directorate of Mineral Research and Exploration, Department of Geophysical Studies, Ankara)0000-0003-4530-7850
Erdi Apatay(General Directorate of Mineral Research and Exploration, Department of Geophysical Studies, Ankara)
Erdoğan Yılmaz(Turkish Petroleum International Company (TPIC), Department of Mining and Drilling, Ankara)0000-0003-4054-4988
Batuğhan Yıkmaz(Turkish Petroleum International Company (TPIC), Department of Mining and Drilling, Ankara)0000-0002-8533-4127
Sami Aytaç Özdemir(Turkish Petroleum International Company (TPIC), Department of Mining and Drilling, Ankara)0000-0003-4693-5891
Sermet Gündüz(General Directorate of Mineral Research and Exploration, Department of Geophysical Studies, Ankara)0000-0002-5652-5469
Tuğçe Can(General Directorate of Mineral Research and Exploration, Department of Geophysical Studies, Ankara)0000-0003-1942-4797
İmam Çelik(Çiçekli Mahallesi Akten Caddesi, No: 58/8 İncirli/Keçiören, Ankara)0000-0002-4327-8163
Abdullah Gürer(Akpınar Mahallesi 850. Cadde, No:10/19 Çankaya, Ankara)0000-0003-4629-2945
Sinem Aykaç(General Directorate of Mineral Research and Exploration, Department of Geophysical Studies, Ankara)0000-0002-0050-9662
Muzaffer Özgü Arısyo(General Directorate of Mineral Research and Exploration, Department of Geophysical Studies, Ankara)0000-0001-7021-3739
Esra Burcu Köse(General Directorate of Mineral Research and Exploration, Department of Geophysical Studies, Ankara)0000-0001-8091-8679
Büşra Bihter Demirci(General Directorate of Mineral Research and Exploration, Department of Geophysical Studies, Ankara)0000-0003-2541-0463
Sayfa
161–174
Yayın Tarihi
2023-04-17
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Yapay Zeka Hızlı Bakış & Çıkarımlar

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⚡ TL;DR(1 Cümlede Hızlı Çıkarım)

The closest point of the evaporate zone to the surface is approximately 150 m, the deepest point is approximately 310 m, the average thickness is approximately 100 m and the maximum thickness is 185 m.

📌 3 Maddede Bu Makale

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Amaç & Hipotez:The presence of the evaporate salt zone in Ankara-Polatlı region has been determined by the drillings.
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Temel Bulgular & Veri:It is thought to be the largest reserve in Türkiye.
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Sonuç & Katkı:The closest point of the evaporate zone to the surface is approximately 150 m, the deepest point is approximately 310 m, the average thickness is approximately 100 m and the maximum thickness is 185 m.
🔬Tür:Araştırma Makalesi
📍Kapsam:Genişletilmiş Akademik Örneklem
⚙️Değişkenler:Salt · Evaporate · Seismic Reflection

Abstract

The presence of the evaporate salt zone in Ankara-Polatlı region has been determined by the drillings. It is thought to be the largest reserve in Türkiye. The seismic reflection method was used to determine the top-bottom levels of the region; its depth; its thickness and extent boundaries; the horst-graben structures; base depth and tectonic movements affecting the study area. Data were collected on three seismic lines. The near-surface tomographic velocity sections were compatible with the top-of-the-zone depth observed in the drillings. As a result of the study, the depth and thickness of the top-bottom of the zone were determined along the lines. Within the scope of the study, a combined interpretation was made on the lines by using gravity and seismic data. The extent of the ore zone was determined only in the E-W direction section, but not in the north-south direction lines since they are outside the license area and the seismic lines. The closest point of the evaporate zone to the surface is approximately 150 m, the deepest point is approximately 310 m, the average thickness is approximately 100 m and the maximum thickness is 185 m.

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Bu Makaleye Atıf Yap

Güney, R., Özerk, Z. R., Izladı, E., Erden, S., Ak, E., Apatay, E., Yılmaz, E., Yıkmaz, B., Özdemir, S. A., Gündüz, S., Can, T., Çelik, İ., Gürer, A., Aykaç, S., Arısyo, M. Ö., Köse, E. B., Demirci, B. B. (2023). Evaporate salt exploration by two dimensional (2D) seismic reflection method: Ankara- Polatlı region, Türkiye. Maden Tetkik ve Arama Dergisi, Cilt: 170 Sayı: 170, 161–174. https://doi.org/10.19111/bulletinofmre.1188870

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Kaynakça (18)

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