闫浩飞 (2008) 重磁三维可视化建模. 硕士论文, 中国地质大学, 北京.
典型地质模型2D与3D重力正演模拟对比研究Comparative Study on 2D and 3D Gravity Forward Modeling of Typical Geological Model
地质模型, 重力异常正演, 重力异常各阶导数, 二维, 三维Geological Model, Gravity Anomaly Forward, The Derivative of Gravity Anomaly, 2D, 3D
《Advances in Geosciences》, Vol.5 No.4, 2015-08-18
The study of three-dimensional gravity forward of typical geological model was based on the two- dimensional gravity forward method. The sphere is presented as the main geological model, which derives two-dimensional and three-dimensional gravitational Bouguer anomaly, the gravitational anomaly formula of every derivative respectively. The two-dimensional and three-dimensional gravity anomaly curve was achieved in the MATLAB environment. Combining with the analytical method of two-dimensional gravity forward modeling, this paper conducted a three-dimensional gravity forward modeling analysis, as well as compared and discussed the advantages and disad-vantages of two-dimensional gravity forward and three-dimensional gravity forward, and then got the results that two-dimensional gravity forward can only reflect gravity information of geological vertical slice, while three-dimensional gravity forward can reflect gravity information of the whole geological body. Small local geological body can obtain its size and shape through analyzing high- order derivative.