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Doğu Toroslarda Derebaşı (Develi), Armutalan ve Gedikli (Saimbeyli) Köyleri Arasının Jeolojisi

Year 1983, Volume: 4 Issue: 1-2, 45 - 66, 16.08.2014

Abstract

THE GEOLOGY OF AN AREA AMONGST THE DEREBASI
(DEVELI), ARMUTALAN AND GEDiKLi (SAIMBEYLI)
WILLAGES IN THE· EASTERN TAURIDE MOUNTAINS


    Investigated area is located in the western part of Eastern Taurids between Saimbeyli (Adana) and Develi (Kayseri). The district is approximately 550 km2 . In this district, there is a thick stratigraphical sequence comprising almost all systems with their characteristic fossils from Paleozoic to Late Cainozoic. In Paleozoic, the detritals and carbonates, in Mesozoic the carbonates, and in Cainozoic detritals were deposited. There is no metamorphism in the sequence.
The ophiolitic melange compleix including serpantinised ultrabas ic rocks and Triassic - Cretaceous sedimentary rock fragments are found tectonically on Maestrichtien
autochthonous pelagic limestone, and in places rwith stratiphical relation. The probable provences of these allochthonous masses were in the North and Northwest,
and there trasportation occured in Upper Maestrichtien - Paleocen. Between Cambrian and Lotwer Carboniferous, the sequence is continous. There is an important stratigraphical gap between Lorwer Carboniferous and Upper Permian;
and Lower Triassic and Jurassic. However, there are the places where Upper Permian sediments were deposited on the Devonian sediments and Jurasic rocks  were deposited on Permian or older. Lutetian sediments, overly all of the older units with a basal conglomerate, and with an angular unconformity. The strikes of the beds in the autochthonous rock units are generally in NE - SW directions. They dip NW and SE. Some structures in NW - SE trends have been recognized particularly in the Jurassic - Cretaceous formations. After Eocene, the region have been affected by severe compressive forces in NW - SE direction. As a result of this compression, the region had been shortened and extensive thrust faults had formed in NE - SW direction more or less parallel to the structure. The Cambrian formations thrusted over Eocene sediments by these faults. In the areas where sediments of Oligocene and Miocene are absent it is thought that an uplift movement have been developed. Therefore from plioce;ie onrNards the sea connection ended. The evidences of this uplift is the presence of lacustrine and fluvial deposits of Pliocene which cover all the rock units.


Year 1983, Volume: 4 Issue: 1-2, 45 - 66, 16.08.2014

Abstract

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Details

Primary Language English
Journal Section Makaleler
Authors

Sait Metin This is me

Publication Date August 16, 2014
Published in Issue Year 1983 Volume: 4 Issue: 1-2

Cite

APA Metin, S. (2014). Doğu Toroslarda Derebaşı (Develi), Armutalan ve Gedikli (Saimbeyli) Köyleri Arasının Jeolojisi. İstanbul Yerbilimleri Dergisi, 4(1-2), 45-66.
AMA Metin S. Doğu Toroslarda Derebaşı (Develi), Armutalan ve Gedikli (Saimbeyli) Köyleri Arasının Jeolojisi. İstanbul Yerbilimleri Dergisi. August 2014;4(1-2):45-66.
Chicago Metin, Sait. “Doğu Toroslarda Derebaşı (Develi), Armutalan Ve Gedikli (Saimbeyli) Köyleri Arasının Jeolojisi”. İstanbul Yerbilimleri Dergisi 4, no. 1-2 (August 2014): 45-66.
EndNote Metin S (August 1, 2014) Doğu Toroslarda Derebaşı (Develi), Armutalan ve Gedikli (Saimbeyli) Köyleri Arasının Jeolojisi. İstanbul Yerbilimleri Dergisi 4 1-2 45–66.
IEEE S. Metin, “Doğu Toroslarda Derebaşı (Develi), Armutalan ve Gedikli (Saimbeyli) Köyleri Arasının Jeolojisi”, İstanbul Yerbilimleri Dergisi, vol. 4, no. 1-2, pp. 45–66, 2014.
ISNAD Metin, Sait. “Doğu Toroslarda Derebaşı (Develi), Armutalan Ve Gedikli (Saimbeyli) Köyleri Arasının Jeolojisi”. İstanbul Yerbilimleri Dergisi 4/1-2 (August 2014), 45-66.
JAMA Metin S. Doğu Toroslarda Derebaşı (Develi), Armutalan ve Gedikli (Saimbeyli) Köyleri Arasının Jeolojisi. İstanbul Yerbilimleri Dergisi. 2014;4:45–66.
MLA Metin, Sait. “Doğu Toroslarda Derebaşı (Develi), Armutalan Ve Gedikli (Saimbeyli) Köyleri Arasının Jeolojisi”. İstanbul Yerbilimleri Dergisi, vol. 4, no. 1-2, 2014, pp. 45-66.
Vancouver Metin S. Doğu Toroslarda Derebaşı (Develi), Armutalan ve Gedikli (Saimbeyli) Köyleri Arasının Jeolojisi. İstanbul Yerbilimleri Dergisi. 2014;4(1-2):45-66.