最后，我纠正了颜色，为了展示出地形，又叠加了阴影。
Finally, I did some color correcting and added shadows to play up the topography.
综合体b是叠加式的别墅，它使用叠加的方法，体现了倾斜的地形特征。
Complex B as a stacking Villa format, it USES stacking method that reflects the characteristics of sloped topography.
如果地形剖面图与地质图、水文图、构造图等进行叠加，可以形成综合剖面图。
Integrated profiles can also be developed by overlaying geological maps, hydrological maps and tectonic maps on the terrain profiles.
在地形起伏剧烈和表层低速带速度横向变化较大的地区，做好野外静校正是取得高质量叠加剖面的重要一步，而确定表层低速带速度是做好静校正的关键。
Field statics is one of vital processing for achieving high quality stacked sections in areas with drastic topographic relief and sharp lateral variations of LVZ velocity.
在此浮动基准面上求取的叠加速度仅取决于低速带底板下伏介质的速度，而与地形、低速带无关。
The stack velocity calculated on the floating datum depends on the velocity of medium underlying the low velocity layer and is independent of topography and low velocity layer.
他们列队与地形，所以你可以看到真正的处理叠加在我们的三维图像。
They line up with the terrain, so you can see the real deal superimposed on our 3d imagery.
本文提出的基于起伏地表的叠加速度分析方法，应用双平方根方程计算反射波的旅行时间，可适用于地形起伏剧烈地区。
The method of stack velocity analysis based on relief surface presented in the paper uses double-square-root equation to compute the travel time of reflections, which is suitable to use in the area w.
测试得知，叠加了建筑物、道路、植被的复杂地形的平均生成时间为15.96秒，实现了复杂三维场景的流畅漫游。
The test showed that the average production time overlapped by the complex terrain of buildings, roads and vegetation is 15.96 seconds, thus realized the roam in the complex 3-d scene fluently.
GIS学者在研究三维地形可视化和数字城市可视化时，普遍在地形、城市建筑物的几何模型上叠加了纹理。
The scholars in the GIS domain always add adding texture on geometry model of the 3D things in the study on the 3D terrain and the digital city.
国内外地应力实测资料证实，地表附近构造应力受多种影响因素的干扰，经常叠加着非构造应力（如地形等引起的应力）。
The concept of tectonic stress plane (TSP) is defined as an ideal curved plane drawn by the locations with different depths where the influence of non-tectonic stress disappears.
国内外地应力实测资料证实，地表附近构造应力受多种影响因素的干扰，经常叠加着非构造应力（如地形等引起的应力）。
The concept of tectonic stress plane (TSP) is defined as an ideal curved plane drawn by the locations with different depths where the influence of non-tectonic stress disappears.
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