The anomalies are controlled by tectonic factors; fault heat conduction is the major feature of the geothermal anomaly in the area.
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。
Based on the measure of ground Radon at Shizipin area, this paper gives some preliminary analyses about the characteristics of ground Radon anomaly in the geothermal field.
本文通过柿子坪地区地表氡气测量，对热田地表氡气异常特征作了初步分析。
In this area, the ground Radon high value anomaly presents annular pattern, and is controlled strictly by structure of the geothermal field.
该区地表氡气高值异常呈环状产出，并严格受构造控制。
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 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。
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