2147-9364_2007_22_1and2

Author: Burhan DAVARCIOĞLU, Refik KAYALI Publishing Date: 2007 E-ISSN: 2147-9364 Volume 22 Issue 1-2 ABSTRACT:The clay specimens taken from Aksaray-Guzelyurt studied area taking place in the southeast part of Aksaray province in the Central Anatolia Region have been investigated by means of FT-IR spectroscopy. Firstly, the FT-IR spectra of the clays known as standard clays such as illite, mixed layered illite-smectite, […]

Author: Ömer AKINCI Publishing Date: 2007 E-ISSN: 2147-9364 Volume 22 Issue 1-2 ABSTRACT:Modern mining works are being conducted at different environments and positive or negative new developments are brought into attention of the earth scientİsts or mining engineers. Careless geological works made at the past play an important role on the closure of ore dressing plants and unproductive mineral exploitation.It is

Author: M.Yavuz HÜSEYİNCA, Yaşar EREN Publishing Date: 2007 E-ISSN: 2147-9364 Volume 22 Issue 1-2 ABSTRACT:In this study, it is aimed to examine the gelogy of Ilgın (NW Konya) and its northern part. In the study area the basement units are made up of Silurian-Lower Carboniferous aged Bozdağ formation that is composed of marbles and Devonian-Lower Permian aged Bağrıkurt formation that is

Author: Ahmet TURAN Publishing Date: 2007 E-ISSN: 2147-9364 Volume 22 Issue 1-2 ABSTRACT:Schisty rocks known as Alanya metamorphics and Alanya Unit, taking place in the Taurides belt, is the base in Bozyazı area. In the lower part of these schisty rocks, the Sugözü Nappe, having high-pressure metamorphism, takes place. The Sugözü Unit, which completed its formation in Late Cretaceous, includes interlayered

Author: Ahmet TURAN, Fikret KURTMAN, İhsan SEYMEN Publishing Date: 2007 E-ISSN: 2147-9364 Volume 22 Issue 1-2 ABSTRACT:In the study area located Central Taurus Belt, autochthonous Geyikdağı and lower allochthonous Bozkır, middle allochthonous Bolkardağı and upper allochthonous Aladağ tectonic units of the Taurus Orogenic Belt crop out. The each one of the tectonic slices comprises individual sequences formed in different paleogeographic environments