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一、地球物理异常地质解释的新途径 地球物理调查结果的地质解释,决定了地球物理调查结果被利用的程度,直接影响地球物理调查的地质效果。过去,人们对地球物理调查结果的数学物理解释方法研究得较多,对它的地质解释方法则研究较少。因此,现在对大面积的地球物理调查结果作地质解释,还停留在目视的水平上。传统的作法是:根据解释者直接观察到的异常特征,对异常进行分类,然后根据异常分布地区的地质情况,赋予每类异常一定的地质意义。这种解释方法所能达到的
I. New Approaches to Geophysical Abnormal Geological Interpretation Geological interpretation of geophysical survey results determines the degree to which geophysical survey results are utilized and directly affects the geological effects of geophysical investigations. In the past, there have been more studies on the methods of mathematical and physical interpretation of geophysical survey results and less on its geological interpretation methods. Therefore, geological interpretation of large-scale geophysical survey results is still at the visual level. The traditional method is to classify the anomalies according to the anomalous features directly observed by the interpreter, and then give each type of anomalies some geological significance according to the geological conditions in the areas where the anomalies are distributed. This method of interpretation can be achieved