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在分析三李矿区和龙门矿区的地热异常带形成特点的基础上 ,结合嵩山区域水文地质条件 ,说明了区域水文地质条件对正确认识和解释正常地温背景条件下的局部地热异常有明显效果。
Based on the analysis of formation characteristics of geothermal anomaly zones in Sanli mining area and Longmen mining area, the hydrogeological conditions of Songshan area are combined to show that regional hydrogeological conditions have a significant effect on the correct understanding and interpretation of local geothermal anomalies under normal geothermal background conditions.