1) Direction Fractal
方位-分维法
2) direction-fractal estimating method
方位-分维估值法
1.
Using the combined method of fractional Brownian motion and geostatistics extracting the concealed fractal information from the geochemical data, an accurate model to predict the regional background and local background with the improved direction-fractal estimating method is established, and finally the geochemical anomalies are delineated.
阐述了分数布朗运动与地质统计学的关系及用变差函数求分数布朗运动分维数的方法，提出用改进的方位－分维估值法预测化探数据的区域背景和局部背景，从而圈定出地球化学异常。
3) 1-D integral equation method
一维积分方程法
4) 3D integral equation method
三维积分方程法
1.
Using the 3D integral equation method,the mathematical modeling of the hollow ferromagnetic cylinder s magnetic states in the geomagnetic field is established,and the calculations are performed on the different partition meshes.
采用三维积分方程法,建立了地磁场中空心铁磁圆柱体纵向磁化状态的数学模型,并按照不同的剖分格式进行了计算分析。
5) 3D layering method
三维分层式方法
1.
Directed against the 3D data "points cloud" acquired form CMM,the 3D layering method used to realize the automatic feature line picking up based on scanning line was proposed.
针对由CMM获取的三维数据“点云”,提出了基于扫描线的三维分层式方法实现特征线的自动提取,提出了基于局部增量网格扩张的三维散乱数据三角剖分算法,实现任意曲面尖锐棱线的自动提取。
6) 3-D analysis method
三维分析方法
补充资料：比色分析法(见紫外—可见分光光度法)
比色分析法(见紫外—可见分光光度法)
比色分析法见萦外一可见分光光度法。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条