JatsTech

2147-9364_2010_25_4

Selcuk University Journal of Engineering, Science & Technology

FIREPROOF APPLICATIONS IN INDUSTRIAL STEEL STRUCTURES

Author: Burhan UZBAŞ Publishing Date: 2010 E-ISSN: 2147-9364 Volume: 25 Issue: 4 ABSTRACT: It is known by everyone that concrete is commonly used as a construction material. One of the usage areas of concrete is using as protective material in fire resistance applications (fireproof) of industrial steel structures. As it is known that besides their excellent structural properties, significant losses occur […]

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CYCLIC TRANSGRESSIVE AND REGRESSIVE SEQUENCES DURING CRETACEOUS TIME, NORTHERN ZELTEN PLATFORM, SIRT BASIN, LIBYA

Author: Senusi M. HARSHA Publishing Date: 2010 E-ISSN: 2147-9364 Volume: 25 Issue: 4 ABSTRACT: Two marines transgressive and regressive cycles are recognized during the Cretaceous time; one is represented during Early Cretaceous, when the Sirt area was still an arch. In this cycle, the sedimentation had only taken place on the line base of the arch. The Jurassic sediments partially transgressed

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GEOLOGICAL SPECIAL FEATURES OF THE AKÖREN REGION (KONYA, CENTRAL TAURIDES)

Author: Ahmet TURAN Publishing Date: 2010 E-ISSN: 2147-9364 Volume: 25 Issue: 4 ABSTRACT: The Akören region is an interesting province with autochthonous Geyikdağı Unit, allochthonous Bozkır Unit and Neoautochthonous Unit. The Neoautochthonous Unitss overlie unconformable basement autochthonous and allochthonous tectonic unites. The aim of the study is to bring out stratigraphica and tectonical features of the region. In the study field

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THE STRATIGRAPHY OF THE ALLOCHTHONOUS ALADAĞ UNIT AT THE BEYRELI AREA (CENTRAL TAURIDES: HADIM)

Author: Ahmet TURAN Publishing Date: 2010 E-ISSN: 2147-9364 Volume: 25 Issue: 4 ABSTRACT: There are Middle Carboniferous‐Early Cretaceous sequences of the Aladag tectonic unit, exposed as tectonic slices of the Central Taurides around the Beyreli area. The sequences correspond to the uppermost allochtonous unit, and known as Gevne nappe. In the area, the stratigraphic sequence of the Aladağ Unit begins by

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