Morphology and flow characteristics of the lamas river mouth.

Ebren, Gurhan


Morphology and genetic variability among four populations of brown trout (Salmo trutta L.) in Turkey.
Yalın, Ali Erdinç; Togan, İnci; Department of Biology (1996)
Structure and recent evolution of the Hazar Basin: a strike-slip basin on the East Anatolian Fault, Eastern Turkey
Moreno, D. Garcia; Hubert-Ferrari, Aurelia; Moernaut, Jasper; Fraser, J. G.; Boes, Xavier; Van Daele, Maarten; Avşar, Ulaş; Cagatay, N.; De Batıst, Marc (Wiley, 2011-04-01)
The Hazar Basin is a 25 km-long, 7 km-wide and 216 m-deep depression located on the central section of the East Anatolian Fault zone (eastern Turkey) and predominantly overlain by Lake Hazar. This basin has been described previously as a pull-apart basin because of its rhombic shape and an apparent fault step-over between the main fault traces situated at the southwestern and northeastern ends of the lake. However, detailed structural investigation beneath Lake Hazar has not been undertaken previously to ve...
Morphology and optical properties of thin silica films containing bimetallic Ag/Au nanoparticles
Yashan, G. R.; Eremenko, A. M.; Smirnova, N. P.; Suzer, S.; Ertaş, Gülay; Tabor, Ch. (Springer Science and Business Media LLC, 2008-11-01)
We have studied the optical spectra in the UV and visible regions, the morphology by scanning electron microscopy (SEM), and the X-ray photoelectron spectra (XPS) of bimetallic Ag/Au nanoparticles incorporated into transparent silicate films in the sol-gel transition stage. The bimetallic nanoparticles, obtained by a combination of photoreduction and thermal reduction, form structures of the alloy or core-shell type.
Morphology of Solidification Microstructures in Fe-Al Based Intermetallic Compounds
Akdeniz, Mahmut Vedat; Mehrabov, Amdulla (1995-09-01)
OGUZ, T; ROZMAN, L (1991-01-01)
Hydrographic observations obtained during the period 6-13 August 1989 are used to illustrate characteristics of the dense water of the Mediterranean underflow in the southwestern Black Sea shelf/slope region. The inflowing warmer and saltier Mediterranean water is observed to spread north-northwestward of the channel-canyon axis along the bottom of the shelf. As the inflowing water crosses the shelf it becomes gradually cooler, fresher and thus less dense by mixing continually with the waters of the Cold In...
Citation Formats
G. Ebren, “Morphology and flow characteristics of the lamas river mouth.,” Middle East Technical University, 1982.