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COMPUTEG
- computes the gravitational acceleration vector at a specified ％ ECF location using the JGM2 gravitational ellipsoid only. ％ Higher-order gravity terms (the \"gravity anomaly\") are ％ ingnored. Only the pure ellipsoid is used.
pos-study-
- ：将研究区域划分成许多具有固定长、宽、高且密度均匀的长方体，利用重力的可叠加性，计算了观测点重力异 常，在此基础上形成重力异常的目标函数。把长方体的密度作为参数，采用蚁群算法进行密度反演试验。结果表明该方法 具有一定的科学性和实用性。-: The study area is divided into a number with a fixed length, width, height and density, uniform rectangular, stackable nature
FA2Boug_CG
- 用fortran程序语言编定的进行布格重力异常改正的程序-Fortran programming language used for the scheduled procedure Bouguer gravity anomaly correction
wgh
- 重力资料处理异常分离来分离区域异常和局部异常-Gravity anomaly separation of data processing to separate regional anomalies and local anomaly
mainf
- 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
Untitled
- 计算球体重力异常G,以及2阶导数，3阶导数的matlab 程序-Sphere calculated gravity anomaly G, and 2-order derivative, 3-order derivative matlab program
gravityanomaly-of-faultmodel
- Theoretical gravity anomaly of fault model and generation of Gaussian random noise
zj
- 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
iteration
- 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
GradCalc
- 地球科学（Fortran90）: 计算空间重力异常、扰动重力、垂线偏差或重力梯度的垂向梯度。 计算方式：数值积分、二维平面FFT、二维球面FFT或一维FFT。-Earth Science (Fortran90): calculate the gravity anomaly, gravity disturbance, the deflection of the vertical or gravity gradient vertical gradient. Calculation: nume
QGRAV
- 用fortran，根据全球球鞋展开模型计算重力异常和垂线偏差-Using fortran, model calculations based on global expansion shoes gravity anomaly and vertical deviation
grav_nonlinear
- 地球物理勘探中重力资料解释的主要目的是由地表观测值推断地下可能存在的密度分布。众所周知,任何一组重力数据都可能由无数个密度分布所引起。即使假设了重力异常是由具有均匀密度差的单一地质体产生的,也得不出唯一的解-Gravity geophysical exploration data interpretation main purpose is inferred from surface observations may exist underground density distribution.
grav_plot
- 地球物理勘探中重力资料解释的主要目的是由地表观测值推断地下可能存在的密度分布。众所周知,任何一组重力数据都可能由无数个密度分布所引起。即使假设了重力异常是由具有均匀密度差的单一地质体产生的,也得不出唯一的解。画图-Gravity geophysical exploration data interpretation main purpose is inferred from surface observations may exist underground density distributi
jxzlyc
- 矩形的重力异常正演程序 输入参数可得到不同尺寸埋深的矩形的重力异常值-Rectangular gravity anomaly forward procedure input parameters available in different dimensions of the rectangle depth gravity anomaly values
gaojiedaoshu
- 重力异常数据高阶导数处理的matlab程序-the matlab programming of higher derivative gravity anomaly
Forwardmodel
- 计算规则三度体球体的重力异常，通过Visual C++语言实现。-This is a C-plus-plus code about gravity anomaly of three-dimensional body.
changfangti
- 长方体重力异常正演程序，适合物探初学者进行正演编程学习。-Cuboid gravity anomaly forward procedure for geophysical exploration forward program learning beginners.
Gravity_inversion_v0.1
- Matlab code for gravity anomaly inversion
gravity-and-magnetic-modeling
- 重磁正演模拟 地下两个相同球体不同距离时重力异常模拟，及各种数据处理；地下两个大小不一球体重力异常模拟及分离；地下球体磁倾角模拟；-Gravity and magnetic forward modeling Underground two identical spheres at different distances simulate gravity anomaly, and a variety of data processing simulation and abnormal s
interaction
- 平行四边形异常体的重力异常阻尼最小二乘反演-Parallelogram anomaly gravity anomaly damped least squares inversion