动目标的真实方位由相位比较干涉仪测定。
True azimuth of moving target is determined using phase-comparison interferometer.
为了能够从不同方位直观真实地观看岩心图像，应用计算机处理技术对岩心外表面展开图像进行了三维模拟岩心恢复。
Three dimensional simulation core restoration is performed on the expanded images of core outside surface so as to observe the image visually and exactly from different directions.
用构造倾角分析地层产状和区域构造；利用移去构造倾角的矢量方位频率图对沉积相精细分析判断以及计算地层真实厚度。
Using the dip vector frequency plot whose structure dip is moved away, we can analyze and judge the resources orientation of the glutinite formation and sand body d.
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