Post-Paleogene (post-Middle Eocene-pre-Miocene) geodynamic evolution of the Upper Cretaceous-Paleogene Basins in Central Anatolia, Turkey.

2017-04-22
Central Anatolia is one of the key areas on the evolution of Cretaceous-Paleogene Tethys where stratigraphy of the region is well studied. However not well linked with tectonics. The so-called "Ankara Mélange" belt (AOM) and the basins on top are important elements in the understanding of the İzmir-Ankara-Erzincan suture belt (İAES) evolution in Anatolia (Turkey) and in the evolution of Tethys in minor Asia (Turkey). Some of the basins are directly situated on top of the tectonic slices of the accretionary prism (IAES). However, some are not tectonically well explained as in the case of Haymana basin. The southern continental fragments (eg. Kütahya-Bolkardaǧ and Kırșehir blocks from Gondwana) are approaching to northern continents (Pontides of Lauriasia) where basins like Haymana, Alçı, Kırıkkale and Orhaniye extensional basins are evolved in between the closing margins of two continents. Haymana basin is an extensional basin developed under contractional regime on top of both northward subducting oceanic fragments and an approaching fragments of southern continents. Paleogene (end of Eocene) is the time where the Seas were retreated to S-SE Anatolia leaving a continental setting in Anatolia during Oligocene-Miocene. The slip data gathered from the faults cross-cutting the Paleogene Units and the fabric from Cretaceous mélanges depicts a NNW-SSE to NNE-SSW compressional stress regime operated during post-Eocene-pre-Miocene period. Lately the slip surfaces were overprinted by post-Pliocene normal faulting. Key words: fault slip data, Paleogene, NNW-SSE compression, Anatolia.
19th EGU General Assembly, EGU2017, (22 - 27 Nisan 2017)

Suggestions

Post-Miocene Deformation in the South of the Galatean Volcanic Province, NW of Central Anatolia (Turkey)
Rojay, Fuat Bora (2008-01-01)
Central Anatolia, located on the immense Alpine-Himalayan orogenic belt, has a complicated neotectonic evolution, and NE-SW-trending Neogene horsts-graben systems that rejuvenate pre-existing palaeostructures are among the most important structures which help us understand the tectonic evolution of Central Anatolia.
Heat flow in the Sea of Marmara Central Basin: Possible implications for the tectonic evolution of the North Anatolian fault
Grall, Celine; Henry, Pierre; Tezcan, Devrim; de Lepinay, Bernard Mercier; Becel, Anne; Geli, Louis; Rudkiewicz, Jean-Luc; Zitter, Tiphaine; Harmegnies, Francois (2012-01-01)
The Central Basin in the Sea of Marmara is a syntectonic basin related to the evolution of the North Anatolian fault. A well-dated (ca. 15.5-16 ka) homogenite sediment can be used as a marker in three-dimensional depth model calculations, allowing a precise determination of the seafloor subsidence rates during the Holocene. A steady-state model based on the propagation of the rates downward through the basin fill provides a good correlation with the deeper seismic reflection imagery for the past 250 ka but ...
Contested Histories in Central Asia: Implications for Contemporary National and Religious Identities
Kuşçu Bonnenfant, Işık; Baykız, Tekin; Ünlü Bilgiç, Tuba(2015-12-31)
Central Asia has been a region of various interests for many centuries. The collapse of the Soviet Union led to the independence of five states in the region. All these states went through major socio-economic and political challenges in the post-Soviet period. While domestic in nature, these problems have started to affect the overall stability and security in the region. The 9/11 attacks and the subsequent “War on Terror” contributed to the perception that the region is vital for global security as well....
Palaeoenvironment and human interaction during the last 4k years in the dried lake sediments (amik lake, southern turkey): evidences of lake level changes
El Ouahabi, Meriam; Hubert-ferrari, Aurelia; Auwera, Vander; Avşar, Ulaş; Karabacak, Volkan (2019-02-01)
The Amik Basin in the Eastern Mediterranean region has been continuously occupied since 6000-7000 BC. The landscape has sustained with highly variable anthropic pressure culminating during the Late Roman Period when the Antioch city reached its golden age. The basin also sustained a high seismic activity (M≥7) as it is a releasing step-over along the Dead Sea Fault. The study focuses on the sedimentary record of the Amik Lake occupying the central part of the Basin. Our objective is to constrain major paleo...
Analysis of crust and mantle structure across Turkey using passive seismic data
Abgarmi, Bizhan; Özacar, Atilla Arda; Department of Geological Engineering (2019)
Anatolia is one of the most tectonically active regions in the world which is amalgamation of different terranes and structures. This region has a complextectonic evolution which includes various stages of subduction and collision. This complexity demands more detailed observations of the crust and upper mantle to generate a comprehensive geodynamic model. However, the knowledge related to crust and mantle structure beneath Anatolia is still very limited so the fates of the structures in deeper interiors ar...
Citation Formats
F. B. Rojay, “Post-Paleogene (post-Middle Eocene-pre-Miocene) geodynamic evolution of the Upper Cretaceous-Paleogene Basins in Central Anatolia, Turkey.,” presented at the 19th EGU General Assembly, EGU2017, (22 - 27 Nisan 2017), Vienna, Avusturya, 2017, Accessed: 00, 2021. [Online]. Available: https://hdl.handle.net/11511/72294.