搜索资源列表
gravity
- 关于地球物理重力和磁法勘探的仿真程序及说明-About geophysical gravity and magnetic exploration and descr iption of the simulation program
zrh
- 根据位场数据的有效性，采用地球物理重力勘探方法对地下异常体进行边界检测,-According to the effectiveness of potential field data, the use of geophysical gravity anomalies of the underground exploration methods for boundary detection,
WeiChang
- 有限单元法用于解地球物理位场延拓问题,第一类边值问题-Finite element method for the solution of geophysical field continuation problem
inverse_questions-codes
- 主要是关于地球物理反演问题的几种方法，对其进行了编程实现-Mainly on geophysical inversion problem several methods to achieve its programming
erweitaijie
- 断层正演程序，很实用，地球物理的同学用的上-Fault forward procedure, very practical, the students used the geophysical
MyPoint
- 物探野外测点生成程序，可实现单线，多线，需要输入起始和终点坐标。-Geophysical Field measurement points generator, enabling single-line, multi-line, you need to enter the start and end coordinates.
Correl080
- 本软件适合工程技术人员及学生进行数据分析。适用范围广、输入界面简单方便、功能模块实用强大、操作简便易懂。 本软件可进行二元线性与非线性相关分析；多元线性与非线性相关分析；多元线性的相关矩阵分析；数理统计与误差分析；计算行列式的值、求解多元方程组；学习与研究函数的图形及特性；计算常用函数等等。例如：可对化验分析成果进行回归及误差分析、对地质物化探数据进行相关性分析、对测量数据进行误差分析、对社会调查数据进行统计分析等等。 -The software for engineering an
FD-
- 地球物理交错网格有限差分波场数值模拟及边界处理PML-Geophysical finite difference wave field numerical simulation with PML boundary
1D-inverse-
- 几个地球物理一维反演程序 可做简单的一维反演 类似于一个软件的东西 从老师那要的，大家内部交流 不要用作商业用途 -geophysical inverse
bp-matlab
- 物探中基于BP神经网络模型煤层含气量预测-In the geophysical prospecting based on BP neural network model to predict coal bed gas content
Data-smooth
- 本程序是基于地球物理理论中，测量得到的磁法数据需要圆滑，故而有此程序。程序使用的圆滑方式是5个点的圆滑。-This procedure is based on geophysical theory, measurement of the magnetic method of data need to be smooth, and therefore have this program. Uses smooth sleek five points.
FD-
- 地球物理交错网格有限差分波场数值模拟及边界处理PML-Geophysical finite difference wave field numerical simulation with PML boundary
three_D
- 物探三维电法勘探方法试验性设计，演示三维电法勘探的方法和结果-Geophysical 3D electrical prospecting method of experimental design, demonstrates 3D electrical prospecting methods and results
zaituiguang
- 属于地球物理反演。不适定问题求解方法三，再推广。（有图像）-Belong to the geophysical inversion. Ill-posed problem solving methods, and promotion. (image)
BG
- 属于地球物理反演。不适定问题求解方法四，平均核方法。（有图像）-Belong to the geophysical inversion. Four ill-posed problem solving method, the average nuclear methods. (image)
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
3DDC
- 此代码属于地球物理领域，是用有限差分开发的直流电法三维正演，基于FORTRAN平台，此代码具有很高的运算效率，对于从事地球物理领域的人来说是不可多得的-This code belongs to the field of geophysics, is developed using finite difference method of three-dimensional forward modeling of DC, FORTRAN-based platform, this code has h
MATLAB-GPS-data-processing
- 利用MATLAB实时处理GPS数据,：利用MATLAB软件环境，现场接收并实时处理海上地球物理调查过程中的GPS定位数据，剔除原始数据中的跳点，处理定位误差.-Real-time GPS data processing, using MATLAB: using the MATLAB software environment, the site receives and real-time processing GPS positioning in the process of Marine ge
Kriging
- 协同克里金插值算法，可用于各种地球物理手段的成图，地形图，高程图，电阻率分布等-Collaborative Kriging interpolation algorithm can be used for a variety of geophysical instruments to map, topographic maps, elevation maps, resistivity distribution.