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温度是能量一种度量参数,温度的高低在一定程度上反映了地质活动的程度。温度随时间变化,在瞬时的地表温度场能够为遥感所检测。遥感所检测的地表瞬时温度场能够获得与地温有关的活动构造、地热资源、冻土等有关信息,在工作中,我们可以利用地温异常活动一些信息,从而指导我们寻找活动构造、地热资源和冻土带分布等。本摘要简单阐述利用瞬时温度场遥感效应进行地质工作:
Temperature is a measure of energy. The level of temperature reflects to some extent the extent of geological activity. The temperature changes with time and can be detected by remote sensing at the instantaneous surface temperature field. The instantaneous temperature field measured by remote sensing can obtain information related to geothermal activity structure, geothermal resources and permafrost. In the course of work, we can use some information about geothermal anomalies to guide us in finding tectonics, geothermal resources and frozen Soil distribution. This summary briefly describes the use of instantaneous temperature field remote sensing effect of geological work: