摘要
梵净山穹窿区地热水呈带状分布,属中低温热矿水,其形成受区域性深大断裂控制。通过对梵净山穹窿区区域水文地质、地热地质条件研究,以及地热水成因分析,总结出梵净山穹窿区地热资源具有以下赋存特征:区域性断裂构造有带状热储形成条件;区域性断裂与背斜复合构造区具有地热田形成条件。梵净山属于世界自然遗产,旅游资源丰富,地热资源赋存条件较好,具有较高的开发利用价值。
The geothermal water in the Fanjing mountain dome region distributes in zones and belongs to medium-low temperature hot mineral water.Its formation is controlled by regional deep and large faults.Based on the study of regional hydrogeology and geothermal geological conditions in Fanjing mountain dome area and the analysis of geothermal water genesis,it is concluded that the geothermal resources in Fanjing mountain area have the following characteristics:the formation conditions of zonal thermal reservoirs are in regional fault structures and the formation conditions of geothermal fields are in the composite structural areas of regional faults and anticlines.Fanjing mountain is a world natural heritage,rich in tourism resources,good conditions for geothermal resources,and has high value for development and utilization.
引文
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