Miocene tectonic history of the Central Tauride intramontane basins, and the paleogeographic evolution of the Central Anatolian Plateau

Date

2017-11-01

Author

Koç, Ayten
Kaymakcı, Nuretdin
Van Hinsbergen, Douwe J. J.
Kuiper, Klaudia F.

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Marine Lower-Upper Miocene deposits uplifted to > 2 km elevation in the Tauride mountains of southern Turkey are taken as evidence for the rise of a nascent plateau. The dynamic causes of this uplift are debated, but generally thought to be a regional dynamic topographic effect of slab motions or slab break-off. Immediately adjacent to the high Tauride mountains lie the Central Tauride Intramontane Basins, which consist of Miocene and younger fluvio-lacustrine basins, at much lower elevations than the highly uplifted marine Miocene rocks. These basins include the previously analyzed Altinapa and Yalvac basins, as well as the until now undescribed rigin Basin.

Subject Keywords

Ilgm Basin, Paleostress inversion, Central Taurides, Anatolia, Paleogeograph

URI

https://hdl.handle.net/11511/46485

Journal

GLOBAL AND PLANETARY CHANGE

DOI

https://doi.org/10.1016/j.gloplacha.2017.09.001

Collections

Department of Geological Engineering, Article

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Citation Formats

A. Koç, N. Kaymakcı, D. J. J. Van Hinsbergen, and K. F. Kuiper, “Miocene tectonic history of the Central Tauride intramontane basins, and the paleogeographic evolution of the Central Anatolian Plateau,” GLOBAL AND PLANETARY CHANGE, pp. 83–102, 2017, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/46485.