progressive sand wave [地质] 前进沙波
sand wave bed 沙波河床
sand wave area 沙波区
wind sand wave 风成沙浪
sand wave motion 沙波运动
sand wave height 沙波高度
seabed sand wave 海底沙波
sand-wave movement 沙波运动
sand wave velocity 沙波速度
The formation of sand wave is a typical self organization phenomenon of simple giant systems.
沙波的形成是典型的简单巨系统自组织现象。
The seabed terrain, sand wave migration and the growth of regional erosion ditch create subsea pipeline suspended span.
沙波沙脊区海底管线悬跨的产生,主要是海底地形、沙波的移动和区域性冲沟的发育所造成的。
Based on the relationship between sand porosity and wave impedance, we can use the sand wave impedance to estimate the sand porosity.
根据砂岩孔隙度与波阻抗之间的函数关系,可以利用砂岩波阻抗估算砂岩孔隙度。
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