Abstract:

The basis within the examination area is the Kretase old gabrols. The units that come after this continues throughout the Senozoik until the Kuvaterner. In the region consisting of volcanic rockets, volcanism has continued its activity from Miyosen to the end of the Kuvaterner. In this process, the area was formed first and then the crop materials. The Quaterner are the youngest units consisting of old alivium and foam fillings, volcanic and magmatic foam and sand. High passivity Quaterner ruins and basalt laws form acifers. In the area of examination, Gölcük (Misli) and its surrounding areas are free-acypher characteristics consisting of pipe, square, sand and silk, while going to the northwest (Kiledere and its surrounding areas) the alivion shows a pressure-acypher characteristics because it contains curtains at different levels. With the cause of the benefit formed along the Gölcük, Kiledere and Suvermez line, the thickness of the sediment increases in the middle and north parts. According to the subterranean map of Akifer, the subterranean water flow is right from east to east to west to northwest. The fact that the waters in the area are approximately parallel to the truths that combine the anions and cations indicates that the waters have the same origin. The water is in the water class with a carbonate hardness of more than 50%, with CaCO3 and MgCO3. The hardness of the water is between 18-36 0Fs. The pH values vary between 7 and 8. The EC values are between 456-1.530 μS/cm and are in the drinking water class according to the Turkish Standards Institute (TSE 266, 1997) and the World Health Organization (WHO, 1999). The waters in the review area are in the 1st quality and 2nd quality waters class according to Schoeller's drinkability chart. According to the hydration water characteristics, it is "very good-good and well-useable" characteristics. Water is in the US Salt Laboratory Diagram C2S1 and C3S1 classes. According to the density indicators, the waters in the area can dissolve carbonate, while sulphate is soluble. According to the isotop data, the waters are connected to each other and have a meteoric origin. According to the triathlon analysis, the waters in the area are deep circulating waters that feed from high waters.

Keywords: