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Tectono-stratigraphical Evolution of the Çankiri Basin (Central Anatolia, Turkey)
Date
2000-01-01
Author
Kaymakcı, Nuretdin
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The Menderes Massif forms a large metamorphic culmination in western Turkey ا an extensional province where continental lithosphere has been stretching following Palaeogene crustal thickening. Northern sector of the Massif on the horst between Gördes and Demirci Basins was chosen for structural analysis aimed to study the tectono-metamorphic evolution of the northern Menderes Massif. Within the study area, four groups of rocks are recognized: (1) the metamorphic rocks ا orthogneisses and metasediments; (2) ...
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In Central and Western Anatolia two continent-derived massifs simultaneously underthrusted an oceanic lithosphere in the Cretaceous and ended up with very contrasting metamorphic grades: high pressure, low temperature in the Tavsanli zone and the low pressure, high temperature in the Kirsehir Block. To assess why, we reconstruct the Cretaceous paleogeography and plate configuration of Central Anatolia using structural, metamorphic, and geochronological constraints and Africa-Europe plate reconstructions. We...
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In the Foothills belt of the Taurus overthrust belt in southeast Turkey, a number of Late Cretaceous to late Miocene southward-migrating flexural foredeeps were generated in response to contractional and crustal loading events occurring along their internal margins. From a study of the disposition and deformation of the foreland basin sediments, the relative importance of the following events can be demonstrated: (1) A thin-skinned shortening of the northward-facing Arabian passive margin, which occurred du...
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N. Kaymakcı,
Tectono-stratigraphical Evolution of the Çankiri Basin (Central Anatolia, Turkey)
. 2000.