Determination of the coal-bearing zones and the alteration zones containing uranium ore by using two dimensional (2D) seismic reflection method in Thrace Basin

Author:

AYKAÇ Sinem1,GÜRER Abdullah2,ÇELİK İmam3,YIKMAZ Batuğhan4,ERYILMAZ Erdoğan4,APATAY Erdi1,ÖZDEMİR Sami Aytaç5,GÜNDÜZ Sermet1,CAN Tuğce1,AK Esra1,IZLADI Erdener1,ERDEN Salih1,ÖZERK Zeynep Rezzan6,GÜNEY Recep1,KÖSE Esra Burcu1,DEMİRCİ Büşra Bihter1

Affiliation:

1. General Directorate of Mineral Exploration and Research

2. Akpınar Neighborhood 850. Street, No:10/19 Çankaya, Ankara,

3. Çiçekli Neighborhood Akten Street, No: 58/8 İncirli/Keçiören, Ankara

4. Turkish Petroleum International Company (TPIC), Ankara,

5. Turkish Petroleum International Company (TPIC),

6. General Directorate of Mineral Exploration and Research,

Abstract

It is aimed to reveal the basement topography, the coal-bearing levels, the alteration zones containing uranium ore, and the tectonic structure prevailing by using 2D seismic reflection method in the Thrace Paleogene-Neogene Basin. In this context, seismic data collected on the six profiles were interpreted by correlating with the data of 97 wells. In the seismic lines, respectively, the Metamorphic Basement-Eocene boundary, the top of the coal-bearing zone and the boundary of the Danişmen-Ergene formations were confirmed by using the borehole data. By evaluating seismic data, the coal propagation is modeled with 3D figures. Moreover, coal accumulation starts from the southwest of the field and continues towards the northeast, and it is supported by the results obtained from the borehole data. The presence of uranium ore in some of the alteration zones and borehole data indicated that all alteration zones determined should be inspected for uranium ore. In addition to normal and reverse faults, positive and negative flower structures formed in the strike-slip fault zones were determined, and lignite deposits were cut in the flank of these structures. Finally, it is recommended to carry out seismic studies before drilling, to investigate potential coal and uranium areas and to plan more seismic lines.

Publisher

Bulletin of the Mineral Research and Exploration

Subject

Geology,Geotechnical Engineering and Engineering Geology

Reference29 articles.

1. Boer, N.P. de, 1954, Report on a Geological Reconnaissance in Turkish Thrace September, December G.A. 25373.

2. Coşkun, B.1998. Triple junction zone-North Anatolian Fault relationship and implications on petroleum exploration Saros Gulf, northern Aegean Sea Turkey 3rd International Turkish Geology Symposium (Abstract)., Ankara.

3. Çağlayan, M.A., Yurtsever, A., 1998, Burgaz-A3, Edirne-B2 ve B3; Burgaz-A4 ve Kırklareli-B4; Kırklareli-B5 ve B6; Kırklareli-C6 maps, 1:100 000 scaled geological maps of Turkey, No: 20, 21, 22, 23. General Directorate of Mineral Research and Exploration, Ankara (in Turkish).

4. Erten, T., Çubukçu, A. 1998. Petrographic-sedimentological features, tectonic environmental models, nutritional sources, hydrocarbon and reservoir properties of the Eocene-Oligocene aged deposits of the Northern Thrace Basin. TPAO Research Group Report No: 1217, 66p. (unpublished) (in Turkish).

5. Günaydın, A.B., Çolak, T. 2010-2011. Industrial raw material exploration prospecting report in the Strandja Massif (E19 and E20 Sheets) and Thrace Tertiary (F19 Sheets), General Directorate of Mineral Research and Exploration, Report No:11833 (unpublished) (in Turkish).

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