根据探测区域的磁性变化规律,确定引起各种特征磁性异常的原因,形成有规则的异常对比图及能直观反应地质特征的等值线异常剖面图,以此推断探测区域所存在的疑似断层。对比其他地球物理方法的解释,验证了磁法勘探在断层定位中方法的可行性,并且取得了较为理想的效果。
The reasons of various characteristic magnetic anomaly are determined based on mainly magnetic variation in the detection area,and the regular anomaly contrast figures and contour abnormalities profile chart are produced which can reflect intuitively the geological characteristics,to conclude suspected faults that exist in the detection area.Compared to the interpretation of other geophysical methods,the feasibility of magnetic prospecting method in fault localization is verified with much more satisfying results achieved.