地下热水的评价因子为地热异常程度及热流体质量。
Geothermal water resource can be assessed by the abnormity degree of geothermal and thermal flow quality.
榆中盆地地热异常区，处于区域性地热背景之上，具有深源热机制。
The geothermal anomalous area of Yuzhong Basin is on the regional geothermal background and related to deep source geothermal mechanism.
利用二氧化硅水文地球化学地热温标和井中测温预测地热异常分布范围；
Predicted the abnormal geothermal distribution area using hydrogeochemical geothermal thermometric scale of SiO_2 and predirect temperature test in wells.
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