2147-9364_2008_23_4

Author: M.Hakkı ARSLAN, Arife AKIN, İ.Hakkı ERKAN, F.Gülten GÜLAY Publishing Date: 2008 ISSN: 2147-9364 Volume 23 Issue 4 ABSTRACT: In order to check the seismic performance of typical two- bay Lambda frames, very commonly used for industrial plants in Turkey, a detailed study on a sample prefabricated structure is performed using the criteria given by the recent Turkish Seismic Code(TEC) issued […]

Author: Alican ÖZTÜRK, M.Muzaffer KARADAĞ, Arif DELİ Publishing Date: 2008 ISSN: 2147-9364 Volume 23 Issue 4 ABSTRACT: İnceleme alanında en altta otokton olarak yerleşmiş Üst Kambriyen-Alt Ordovisiyen yaşlı Seydişehir Formasyonu, Üst Jura yaşlı Hacıalabaz formasyonu, Üst Kretase yaşlı Çökelen diyabazı ve yine Üst Kretase yaşlı Saytepe formasyonlarında oluşan Geyikdağı birliği yer almaktadır. Bu birlik üzerine allokton olarak Devoniyen-Alt-Orta Karbonifer yaşlı Hocalar

Author: Ali Rıza SÖĞÜT, Ahmet GÜZEL Publishing Date: 2008 ISSN: 2147-9364 Volume 23 Issue 4 ABSTRACT: The basement of the study area formed by Crateceous aged gabbros. Over the basement, the rock units span to Cenozoic to Quaternary. The volcanic activity in the region started at Miocene and ended at the end of Quaternary. In this process, the Melendizdağı at first

Author: Ali SARI, Derya KOCA, Şükrü KOÇ, Berna YAVUZ, D.Banu KORALAY Publishing Date: 2008 ISSN: 2147-9364 Volume 23 Issue 4 ABSTRACT: In Late Jurassic which is a period that the global sea rising occurred in the world, important source rocks for oil beds had been occurred as a result of anoxic events. In Middle Taurus region Akkuyu formation which also is

Author: Kerim KOÇAK Publishing Date: 2008 ISSN: 2147-9364 Volume 23 Issue 4 ABSTRACT: Phyllite of Bagrıkurt Formations contains dark color fragments, which have variable size (long axis: 1-18 cm) but usually elliptical shape. The fragments are quartzite, quartz-phyllite, chloritoid-quartz-phyllite, phyllite and metasandstone in composition. They are composed mainly of quartz (0.3-1 mm; 35-95%), colorless chlorite (0-50%), calcite (0-20%), chloritoid (0.1-0.4 mm;%