Sedimentological and cyclostratigraphic analysis of upper part of the kartal formation (sw of Ankara)

Download
2008
Aghayev, Rufat
The Montian Kartal Formation lies in the south-west of Ankara region and overlies the Upper Cretaceous Beyobasi Formation and is overlain by Thanetian Kırkkavak Formation conformably in the studied region (Kayabası village, NW of town of Haymana). A 283 m stratigraphic section, which is mainly composed of an alternation siliciclastic and carbonate rocks has been measured in the Kartal Formation within the Haymana-Polatlı basin. The aim of this study is to carry out the sedimentological and cyclostratigraphical analyses of the upper part of the Kartal Formation within Haymana-Polatlı basin which represents a well developed cyclic pattern. In this study, detailed lithofacies analyses were performed and four different facies were recognized along the measured section: sandstones, limestones, mudrocks and conglomerates. Sedimentological analyses, such as modal, provenance, palaeocurrent, grain-size and grain parameters were also performed and their relation with the depositional environment and change in depositional conditions were discussed. Interpretations of the depositional environment revealed that the deposition occurred by low sinuosity rivers and waves. Additional environmental interpretations suggested that the sediments were deposited in shallow marine and/or coastal (beach) environments. High resolution cyclostratigraphy studies based on meter scale cyclic and rhytmic occurrences of lithofacies along the measured section were performed. The whole section, which is 283 m thick, was divided into large-scale hierarchy-cycles which comprise smaller-scale fining upward and deepening upward cyclic and rhythmic beds.

Suggestions

Post-paleocene deformation in Kalecik region, East of Ankara, Turkey
Kasımoğlu, Pınar; Rojay, Fuat Bora; Department of Geological Engineering (2010)
In order to understand the tectonic evolution of the Kalecik region (Ankara, Turkey), a structural field study was performed in a selected area located in the east of Kalecik, where mostly imbricated thrust sheets of the Cretaceous Ophiolitic melange crop out. In the study area, the Cretaceous Ophiolitic melange, Cretaceous radiolaria-bearing sequences and the Paleocene units are all intruded by sub-vertical dykes. The attitudes of planar structures (dykes, beds and faults) and the kinematic data measured o...
Evolution of the Çiçekdağı Basin, Central Anatolia, Turkey
Gülyüz, Erhan; Kaymakcı, Nuretdin; Department of Geological Engineering (2010)
Çiçekdağı basin developed on the Central Anatolian Crystalline Complex (CACC) is a foreland basin developed as the southern integral part of the Çankırı Basin during the Late Paleocene to middle Oligocene. The basin has two compartments separated by the Çiçekdağı High comprises two sedimentary cycles. The oldest cycle comprises Baraklı, Kocaçay and Boğazköy formationsa and is exposed both in the northern and the southern sectors. They were deposited in marine conditions. The second cycle comprises İncik and...
Cretaceous/paleogene boundary in the Haymana basin, Central Anatolia, Turkey: micropaleontological, mineralogical and sequence stratigraphic approach
Esmeray, Selen; Altıner, Demir; Department of Geological Engineering (2008)
An integrated micropaleontological, mineralogical and sequence stratigraphical investigation was carried out across the Cretaceous/Paleogene (K/P) boundary in the Haymana basin, Turkey. A 29.41 m thick boundary section consisting of limestones and marls was measured and 90 samples were analyzed. Biostratigraphic and chronostratigraphic works are based on the planktonic foraminifera. 64 planktonic species were identified and 5 biozones were established. The biozones are, in ascending order, Planoglobulina ac...
Developing a geotechnical microzonation model for Yenişehir (Bursa) settlement area
Kolat, Çağıl; Süzen, Mehmet Lütfi; Department of Geological Engineering (2010)
The purpose of this study is to develop a geotechnical microzonation model regarding the suitability of the residential areas in Yenişehir (Bursa, Turkey), which is a currently developing settlement area in a seismically active region. For this purpose, soil properties and dynamic soil behaviors of the study area were assessed. Soil classification, soil amplification, natural soil predominant period, resonance phenomena and liquefaction potential of the study area were evaluated using borehole data and micr...
Geochemistry of the post-collisional Miocene mafic Tunceli Volcanics, Eastern Turkey: Implications for the nature of the mantle source and melting systematics
Aktağ, Alican; Sayıt, Kaan (2019-01-01)
The East Anatolian Accretionary Complex (EAAC) comprises an ideal example of post-collisional volcanism within the Africa-Eurasia collision zone. The Miocene mafic Tuncell Volcanics, as a part of this post-collisional volcanic system, are located in the western termination of EAAC. The mafic Tunceli Volcanics are characterized by mildly alkaline and tholeiitic basalts, in which olivine, clinopyroxene and plagioclase characterize the main mineralogy. The role of fractional crystallization (FC) and assimilati...
Citation Formats
R. Aghayev, “Sedimentological and cyclostratigraphic analysis of upper part of the kartal formation (sw of Ankara),” M.S. - Master of Science, Middle East Technical University, 2008.