Özet:

In the Hadim area within the middle Toros tribe, the Haddim plots are floating within the area of the Autokton Geyikdağı and allokton Bozkır, Bolkardağı and Aladağ units. Each of these tectonic shapes covers stratigraphic assemblies that characterize very different paleocographic environments. In Early-Middle Cambrian, the Hadim area is covered by a thick sea where dolomite-dolomite-bioclastic-carbonates collapse. The area is located in the late Cambrian-Ordovision process, in a pool in which seafood crushes, containing conodonted and graptolitic pelitic sediments, collapse. In the Hadim area Late Ordovisiyen-Early Devoniyen old rocks don't give rings. During the late Devoniyen-Carbonifer period, the thick marine environmental conditions are observed in which abundant fossil, carbonate-intermediate crashed units collapse. In the area that preserves the resifal, lagune thick carbonate shelf state in Permian, Early Trias begins with stromatolithic-olithic thick carbonates and passes in a row to the row-marn-shelf phases. In the northern part, in Early-Middle Trias, a methalistostromal community developed; in the southern part of the region, a typical flush stairs were formed in the middle Trias, where the sand, clay, carbonate lithophasies were coated with each other. After this flush period, in the region that turns up with the Early Chimerian orogenic phase, Liyas-Dogger is represented by land-half-terrestrial molasic fractures; and Malm-Early Kretase is represented by thick and stable shelf carbonates. In late Kretase, the main carbonate platform follows the development of the pelagic rhythmic series consisting of a broken sequence of square and square carbonates in Senoniyen. If a different geological community formed during the late Senonian- Early Paleosen process in the region, it is an official-political melanid that is characteristic of the immersion zones. The stratigraphic unit, which was the last to complete its evolution in the Paleotectonic period, is the Lutheran rocks. Lütesien units begin with abundant microfosil resifal carbonates. Then the Lütesiyen resignation, which passes to the flush façade made of sand-smalled crushes, ends with the wild flush façade at the top. The upper Lutheran-Oligosen units are not seen in the field of examination. This process is a period of turning-up-up-up-up in the area. In the late Eosen-Oligosen process, allocton communities (Bozkır, Bolkardağı and Aladağ unions) swallowed from north to south first to the relative autocton (Geyikdağı Union), and then alloctones swallowed on each other.

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