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一、概述遥感地质方法是利用飞机或卫星装载一些仪器,对地球表面进行各种地质探测的方法。其中又分主动遥感和被动遥感。主动遥感系利用测况雷达主动对地面发射微波、激光等能量进行探测,被动遥感则利用地质体自身辐射的能量进行探测。遥感地质调查方法广泛应用于地质测量、矿产普查、水文地质、工程地质以及地震、地热、环境地质、地貌、第四纪地质和海洋地质等多方面的研究。遥感地质是建立在地质体及地质现象的电磁波辐射(反射、吸收、发射)理论基础上的。是在“光场”这个领域内进行研究的。
I. Overview Remote sensing geology method is the use of aircraft or satellite loading some instruments on the surface of the earth for a variety of geological exploration methods. Which is divided into active remote sensing and passive remote sensing. Active remote sensing uses the condition radar to actively launch microwave and laser energy on the ground, while passive remote sensing uses the energy of the geologic body to detect itself. Remote sensing geological survey methods are widely used in geological survey, mineral survey, hydrogeology, engineering geology and earthquake, geothermal, environmental geology, geomorphology, Quaternary geology and marine geology and other aspects of research. Remote sensing geology is based on the theory of electromagnetic radiation (reflection, absorption, emission) of geological bodies and geological phenomena. In the “light field” in the field of research.