论文部分内容阅读
本文详细地讨论了磁化强度填图的方法原理,并且通过理论模型和实测异常计算了引起磁异常激发体的磁化强度分布,还讨论了该方法的效果。一、方法原理根据观测到的重磁异常,确定引起这一异常的激发体的各种参数,构成了重磁反问题。对反问题而言,一般说来唯一解是不可能的。这是因为,无限数目的不同密度或磁性分布,都可以引起一个给定的重力或磁力异常。因此,为了使反问题得到唯一解,必须事先附加某种假设。按照给定的附加条件,实际问题可分为两种类型。第一种类型是假设源的几何形状和空间位置已知,根据观测到的异常求解密度或磁化强度的分布;第二种类型则是假设密度或
In this paper, the principle of magnetization mapping is discussed in detail, and the distribution of magnetization caused by the magnetic anomalous exciton is calculated by theoretical model and measured anomaly. The effect of this method is also discussed. First, the principle of method According to the observed gravity and magnetic anomalies, to determine the cause of this abnormal excitation of the various parameters, constitute a heavy magnetic inverse problem. In general, the only solution to the inverse problem is impossible. This is because an infinite number of different densities or magnetic distributions can cause a given gravity or magnetic anomaly. Therefore, in order to get the only solution to the inverse problem, some assumptions must be attached in advance. According to the given additional conditions, the actual problems can be divided into two types. The first type assumes that the source geometry and spatial location are known, and solves the distribution of density or magnetization based on observed anomalies. The second type is the assumption of density or