重力的一维正演和最小二乘反演
测量与围岩有密度差异的地质体在其周围引起的重力异常﹐以确定这些地质体存在的空间位置﹑大小和形状﹐从而对工作地区的地质构造和矿产分布情况作出判断的一种地球物理勘探方法。 -One-dimensional forward modeling of gravity and least-squares inversion, measurement and differences in rock has density in its surrounding geological body caused by gravity anomalies in order to determine the existence of the spatial location of geological bodies or size and shape, and thus the work area geological structure and mineral distribution to judge a geophysical exploration methods.
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