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.
地热异常分布主要受区域构造因素控制，断裂导热是本区地热异常的主要特点。
The anomalies are controlled by tectonic factors; fault heat conduction is the major feature of the geothermal anomaly in the area.
腾冲不但是现代火山活动区，也是地热异常区，这里温泉、热泉及喷气孔到处可见。
Tengchong is a famous active area of the modern volcano, where the hydrothermal activity is very violent.
西南次海盆也是一个高地热异常区，虽然该次海盆形成较早，但与年轻的构造拉张有关。
The southwest subbasin is another thermal anomalous unit, which might be also related to the young tectonic extension.
火山区的突发性地热异常特征与火山区的地质构造、火山成因、规模、类型等多种因素有关。
The characters of the abrupt geothermal anomaly concern many factors such as geological structure, cause of volcanic formation, volcanic scope and type.
地热异常、地壳内存在低速层和高导层、强烈地震频繁发生等现象说明，这一地区是现代构造运动的活动区。
The geothermal anomaly, low velocity zone and high conductivity layer in crust, and frequent occurrence of strong earthquakes show that the study area is an active area of modern tectonization.
地热异常、地壳内存在低速层和高导层、强烈地震频繁发生等现象说明，这一地区是现代构造运动的活动区。
The depth of upper mantle high-conductive layer in Chinese mainland is presented and a cause of its formation is given.
地热异常、地壳内存在低速层和高导层、强烈地震频繁发生等现象说明，这一地区是现代构造运动的活动区。
The depth of upper mantle high-conductive layer in Chinese mainland is presented and a cause of its formation is given.
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