阜新盆地东梁区地热地质特征探讨

阜新盆地东梁区九佛堂组底邗裂隙及雾迷山组顶部碳酸盐岩风化壳裂隙带为两套含水系统。区内构造断层，裂隙发育，有利于地下热水的运移和贮藏，成矿条件优越。地热水类型为裂隙水。水量可这1589-2400m^3／d，出口水温达69-71℃，水质极具医疗价值，具良好的开发利用远景，可为阜新市经济转型作出贡献。

Two water bearing lay existed in bottom fracture in Jiufetang formation and upper carbonate mineral crust of weathering fracture in Wumishan formation in Dongliang field of Fuxin basin respectively. There were constructional faults and fracture in this field, That is advantageous to underground hot water to transform and storage. The condition of metellogeny was superior, The underground hot water cames from fracture and is about 1389-2400m3/d from specific well. The water temperature is about 69-71℃. That have great development potential because of the the medical care value to human body. The geothermal exploitation and utilization is significant to the economic transition in Fuxin city.