针对地质特征,综合运用大地电磁测深法、直流电阻率测深和瞬变电磁法查清研究区内热储地层分布、大地构造部位和区内深部断裂构造情况,从而为研究区内地热资源的预测和开发提供依据。工作原理大地电磁测深是研究地壳和上地幔构造的一种地球物理探测方法。它以天然交变电磁场为场源,当交变电磁场以波的形式在地下介质中传播时,由于电 According to the geologic features, the geothermal field distribution, the tectonic parts of the tectonic area and the deep faults in the study area are comprehensively explored using the methods of the magnetotelluric sounding method, the DC resistivity sounding method and the transient electromagnetic method. Forecast and development to provide the basis. Working principle Earth’s electromagnetic sounding is a geophysical exploration method to study the crust and upper mantle structure. It is the natural alternating electromagnetic field as the source, when the alternating electromagnetic field in the form of waves propagating in the underground medium, due to electricity