CAJ | 학술논문

断裂构造是控制辽宁省岫岩县暖泉地热田地热异常的主导构造，地热系统属于“断控对流型”地热系统，属低温地热区，热储呈带状。地热异常区中心位于F1、F2断裂交汇部位。地下热水是在构造裂隙中储存的原生地下热水，为裂隙热储。热储受构造和岩性共同控制，热储岩性为印支期二长花岗岩，上覆盖层为砂及砂砾卵石，地热水可命名为氟、偏硅酸复合型医疗矿水。
단렬구조시공제요녕성수암현난천지열전지열이상적주도구조，지열계통속우“단공대류형”지열계통，속저온지열구，열저정대상。지열이상구중심위우F1、F2단렬교회부위。지하열수시재구조렬극중저존적원생지하열수，위렬극열저。열저수구조화암성공동공제，열저암성위인지기이장화강암，상복개층위사급사력란석，지열수가명명위불、편규산복합형의료광수。
The dominant structure that lead to the abnormal geothermal phenomenon of Nuanquan geothermal field in Liaoning Xiuyan is fracture.The geothermal system belongs to “break controlling convection”,“hypothermia”and“ribbon”type.The geothermal anomaly area center located in the intersection of F1 and F2.Underground hot water is stored in the native structural fracture, belongs to fracture geothermal reservoir.Thermal reservoir is controlled by structure and lithology,Thermal reservoir lithology is indo-chinese epoch monzonitic granite that covered with sand and gravel.Geothermal water can be named as complex medical mineral water contained fluorine, metasilicic acid.