Figure 4: Field photographs from the Uyuzhamamı section in the Haymana region; a. Panoramic view showing all the lithostratigraphic units along the section, view from southwest to northeast. b. The basal part of the Uyuzhamamı section, composed of gray- to beige-colored, medium- to thick-bedded platform carbonates of the Bilecik Limestone Group at the center of the Haymana anticline, c. View from the lowermost part of the Seyran Formation within the Soğukçam Limestone Group, including collapse breccia with the platform carbonate pebbles and blocks in a white-colored pelagic matrix of the middle Berriasian age, d. View from the upper part of the Seyran Formation within the Soğukçam Limestone Group consisting of gray- to yellow-colored, thin- to medium-bedded micritic, clayey radiolarian-rich pelagic limestones from which sample Uy-5 of early Barremian age was collected, e. View from the Seyran Formation within the Soğukçam Limestone Group, made up of radiolarian-rich clayey limestones of early Aptian age, and the overlying Akkaya Formation within the Soğukçam Limestone Group composed of gray- to beige-colored, medium- to thick-bedded, closely-packed debris flow deposits of the ? middle to late Aptian-Albian age, f. Photograph showing the boundary between underlying debris flow deposits of early to middle Albian age belonging to Akkaya Formation within the Soğukçam Limestone Group and overlying clayey pelagic limestone part belonging to Akkaya Formation within the Soğukçam Limestone Group of the ? late (latest) Albian age and overlying units, g. Detailed view from the upper part of the Akkaya Formation within the Soğukçam Limestone Group consisting of gray- to beige-, slightly reddish-colored, thin- to medium-bedded, clayey pelagic limestone with abundant glauconite and planktonic foraminiferal assemblages of the latest Albian age, h. Close-up view from the Elmadağ Olistostrome, showing the block of carbonate breccia within a loosely packed, calcareous mudstone matrix of Coniacian age, i. Detailed view from a pelagic block within a loosely packed, calcareous mudstone matrix of the Coniacian Elmadağ Olistostrome.