Kızıldere geothermal field is located in the Aegean graben systems. The study area comprises Kızılkaya, İğdecik, Sazak, Kolonkaya, and Tosunlar formations consisting of marbles, limestones, conglomerates, sandstones, travertines, and alluviums. The wells were drilled to develop the Kızıldere geothermal field, and the reservoir temperatures in the wells were various between 170 and 212 °C. There are three reservoir rocks in the Kızıldere geothermal area. The top reservoir rock is limestone with limited lateral continuity in the Pliocene-aged Sazak formation. The limestones have low porosity, low permeability, and low temperature at about 180 °C compared to other reservoir rocks. The middle reservoir rock, which has a slightly higher porosity and permeability, is represented by İğdecik formation consisting of the alternation of marble-quartz-schist. It has known that there is a hydrostatic pressure relation between these two aquifers. The quartzites are the deepest reservoir in the Kızıldere region. According to the data in R-1 well, quartzites have high permeability and high temperature, which is about 242 °C. The water analysis in the Schoeller diagram demonstrated that the origins of water were the same; however, the amount of ion in water was different. According to the Piper diagram, water samples were classified as a water class with carbonate alkalinity. Finally, the Giggenbach diagram analysis confirmed that the water class of almost all of the water samples were determined as partially in equilibrium condition.

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Kızıldere（Aydın）地区的地热田间研究

Kızıldere地热田位于爱琴海抓斗系统中。研究区域包括Kızılkaya，İğdecik，Sazak，Kolonkaya和Tosunlar地层，包括大理石，石灰石，砾岩，砂岩，钙华和冲积层。钻了这些井以开发Kızıldere地热田，井中的储层温度在170至212°C之间变化。Kızıldere地热区有3个储层岩石。在上新世时代的萨扎克组中，顶部储层岩石是横向连续性有限的石灰岩。与其他储层岩石相比，石灰石的孔隙率低，渗透率低且温度低至约180°C。中层储层岩石具有较高的孔隙度和渗透率，其特征是由由大理石-石英片岩交替组成的İğdecik地层所代表。已知在这两个含水层之间存在静水压力关系。石英岩是基兹尔德雷地区最深的储层。根据R-1井的数据，石英岩具有高渗透率和高温，约为242°C。Schoeller图中的水分析表明水的来源是相同的。但是，水中的离子量不同。根据Piper图，将水样品归为具有碳酸盐碱度的水类。最后，Giggenbach图分析证实，几乎所有水样品的水类别均被确定为部分处于平衡状态。根据R-1井的数据，石英岩具有高渗透率和高温，约为242°C。Schoeller图中的水分析表明水的来源是相同的。但是，水中的离子量不同。根据Piper图，将水样品归为具有碳酸盐碱度的水类。最后，Giggenbach图分析证实，几乎所有水样品的水类别均被确定为部分处于平衡状态。根据R-1井的数据，石英岩具有高渗透率和高温，约为242°C。Schoeller图中的水分析表明水的来源是相同的。但是，水中的离子量不同。根据Piper图，将水样品归为具有碳酸盐碱度的水类。最后，Giggenbach图分析证实，几乎所有水样品的水类别均被确定为部分处于平衡状态。水样品被分类为具有碳酸盐碱度的水类。最后，Giggenbach图分析证实几乎所有水样品的水类别都部分处于平衡状态。水样品被分类为具有碳酸盐碱度的水类。最后，Giggenbach图分析证实几乎所有水样品的水类别都部分处于平衡状态。