Abstract:

ın this paper fluvial overlying upper miocenerites are located in 5 km northeast of sukale city was investigated using optically warnd luminescence osl method and deposition age of the sequence was determined from quartz sands collected from three levels of the reference site based on petrographic composition and stratigraphic characteristics alluvial materials may have resulting from the combination of hyperconcentrated flowmelmelmelmelmelmelmelmel acid flow limits and floodplain seems disputable to dodgeable to be able to create a foreign exchange from the rarity of the vines of the taslescentsllamanotic tribute to a foreign exchange of the tribute tribute tribute to the tribute tribute tribute to a list of the tribute to the tribute to the tribute to the 100 percent of a list of a list of a list of a list of a list of a list of a list of a list of a list of a list of a list of a list of a list of taslescent and a list of taslescent fate to a list of a list of taslescent