Sedimentology and Miocene-Pliocene depositional evolution of the stream-dominated alluvial fan deposits at circum-Sultandağları region
Yıl 2022,
Cilt: 168 Sayı: 168, 43 - 66, 18.08.2022
Ayhan Ilgar
,
Ali Ergen
Alper Bozkurt
Ercan Tuncay
Öz
Yalvaç and Ilgın basins surrounding Sultandağları were opened due to the orogenic collapse in the early Miocene. The NW-SE trending Çakırçal and Akşehir fault zones, forming boundaries with these basins, caused both the opening of the basins and uplifting of Sultandağları. During the Miocene-Pliocene period, the alluvial fans fed from Sultandağları developed on the basin margins, while the lacustrine carbonate and clastic depositions formed in the basin’s interior. The alluvial fan deposits are laterally and vertically transitional with lacustrine sediments and alternate several times in the sequence. The alluvial fans, widespread in the region, consist of debris flow, hyperconsantrated stream flood, braided river and meandering river deposits. Fan deposits that pass from high-energy fluvial facies at the basin margin to the low-energy fluvial facies towards the basin interior have been interpreted as stream-dominated alluvial fan deposits. The age data obtained from the fan deposits of the Yalvaç and the Ilgın basins show that Sultandağları concurrently feeds the alluvial fans on both flanks. Alluvial fan deposition around Sultandağları formed under the control of tectonic and climatic processes. The tectonism led to the formation of basins and source areas. Simultaneously, the climate maintained the streams to be perennial by precipitation, thus proving a continuous sediment supply to the basins. Tectonism and climate-controlled base-level changes determined the quantity of sediments carried to the basin from the source area, causing regressive or transgressive developments.
Teşekkür
This study was carried out within the scope of Sultandağları’nın Jeolojisi ve Jeodinamik Evrimi (Geology and Geodynamic Evolution of Sultandağları) project conducted between 2015- 2016 by the Department of Geological Researches of the General Directorate of Mineral Research and Exploration (MTA), Türkiye. The determination of ostracod fossils was made by Dr. Gönül ÇULHA. We would like to acknowledge Dr. Oktay PARLAK and Tolga ESİRTGEN who reviewed the earlier version of the manuscript and provided valuable contributions. We are also thankful to Prof. Dr. Attila ÇİNER and the other anonymous referee.
Kaynakça
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Yıl 2022,
Cilt: 168 Sayı: 168, 43 - 66, 18.08.2022
Ayhan Ilgar
,
Ali Ergen
Alper Bozkurt
Ercan Tuncay
Kaynakça
- Akgün, F., Akyol, E. 1992. Yukarıkaşıkara ve Yarıkkaya (Isparta) kömürlerinin karşılaştırmalı palinostratigrafisi ve paleoekolojisi. Türkiye Petrol Jeologları Derneği Bülteni 4(1), 129–139.
- Akıska, E., Varol, B. E. 2020. Alluvial-lacustrine sedimentation and volcaniclastic deposition in an intracontinental tectonic graben: paleoenvironmental evolution of the Neogene Sinanpaşa Basin, West-central Turkey. Turkish Journal of Earth Sciences 29, 295–324.
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- Boothroyd, J. C., Ashley, G. M. 1975. Process, bar morphology and sedimentary structures on braided outwash fans, Northeastern Gulf of Alaska. Glaciofluvial and Glaciolacustrine Sedimentation.
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- Brierley, G. J. 1991. Bar sedimentology of the Squamish River, British Columbia: definition and application of morphostratigraphic units. Journal of Sedimentary Petrology 61, 211–225.
- Brunn, J. H., Dumont, J. F., Graciansky, P. C., Gutnic, M., Juteau, T., Marcoux, J., Monod, O., Poisson, A. 1971. Outline of the geology of the Western Taurides. Geology and History of the Turkey. Guidebook for the 13th field session os PESL, Tripoli, 225–255.
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- Carroll, A. R., Bohacs, K. M. 1999. Stratigraphic classification of ancient lakes: balancing tectonic and climatic control. Geology 27, 99–102.
- Catuneanu, O. 2006. Principles of Sequence Stratigraphy. Elsevier, Amsterdam, 375.
- Changsong, L., Eriksson, K., Sitian, L., Yongxian, W., Jianye, R., Yanmei, Z. 2001. Sequence architecture, depositional systems, and controls on development of lacustrine basin fills in part of the Erlian Basin, northeast China. American Association of Petroleum Geologists Bulletin 85, 2017–2043.
- Colella, A., Prior, D. B. 1990. Coarse-grained deltas. International Association of Sedimentologists Special Publications 10.
- Collinson, J. D. 1996. Alluvial sediments. Sedimentary Environments: Processes, Facies and Stratigraphy. Blackwell Science, Oxford, 37–82.
- Demirkol, C. 1982. Yalvaç-Akşehir dolayının stratigrafisi ve Batı Toroslarla deneştirimi. Türk Mühendis ve Mimar Odaları Birliği Jeoloji Mühendisliği Dergisi 14, 3-14.
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- Demirkol, C., Sipahi, H., Barka, A., Sönmez, Ş., Çiçek, S. 1977. Sultandağı’nın stratigrafisi ve jeolojik evrimi. Maden Tetkik ve Arama Genel Müdürlüğü, Report No: 6305, 86, Ankara (unpublished).
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- Eren, Y. 1987. Sultandağları Masifi’nin stratigrafisi ve mesoskopik tektoniği. Yüksek Lisans Tezi, Selçuk Üniversitesi, 80 (unpublished).
- Eren, Y. 1990. Engilli (Akşehir) ve Bağkonak (Yalvaç) köyleri arasında Sultandağları Masifi’nin tektonik özellikleri. Türkiye Jeoloji Bülteni 33, 39–50.
- Ergen, A., Bozkurt, A., Tuncay, E., Doğan, A., Ilgar, A. 2016. Çay-Akşehir arası Sultan Dağları’nın tektono-stratigrafisi: yeni bulgular. 69. Türkiye Jeoloji Kurultayı Bildiri Özleri, 11-15 Nisan 2016, Ankara.
- Ergen, A., Tuncay, E., Bozkurt, A., Doğan, A., Ilgar, A. 2017. Sultan Dağları güneydoğusunun tektonostratigrafisi: Paleozoyik volkanik aktivitelerinin bölgesel jeolojik olaylarla ilişkisi. 70. Türkiye Jeoloji Kurultayı Bildiri Özleri, 10-14 Nisan 2017, Ankara.
- Ergen, A., Bozkurt, A., Ilgar, A., Tuncay, E., Doğan, A. 2021. Sultandağları’nın jeolojisi ve jeodinamik evrimi. Maden Tetkik ve Arama Genel Müdürlüğü, Report No: 13958, 241, Ankara (unpublished).
- Gawthorpe, R. L., Colella, A. 1990. Tectonic controls on coarse-grained delta depositional systems in rift basins. Coarse-Grained Deltas. International Association of Sedimentologists Special Publications 10, 113-128.
- Gawthorpe, R. L., Leeder, M. R. 2000. Tectono-sedimentary evolution of active extensional basins. Basin Research 12, 195-218.
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