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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 geologic
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一个很好的模拟退火反演算法程序,例子是地球物理重力反演-A good simulated annealing inversion procedure, example is the geophysical inversion of gravity
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地球物理学重力勘探中,用最小二乘法对重力异常进行正反演的程序-Gravity exploration geophysics, the least square method on the gravity anomaly inversion procedure
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球体重力异常曲线正演,加噪音后异常曲线,最小二乘反演-Gravity anomaly curve ball forward, plus the noise of abnormal curve, least-squares inversion
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采用U函数余项式反演三维密度界面,其布格重力异常采用Parker法计算-U-function density of more than three-dimensional inversion-type interface, the Bouguer gravity anomaly calculated using Parker
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Matlab code for gravity anomaly inversion
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重力异常反演,《MATLAB程序设计及在地球物理中的应用》一书中的代码,手动敲的。-Gravity anomaly inversion, MATLAB programming and application in geophysics, a book of code, manual knock.
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inversion non-linear
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method of gravity inversion
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