1) erosion depth relationship
冲深关系式
2) shock wave relation
冲花关系式
3) shock-wave relations
冲击波关系式
4) Time-depth relationship
时深关系
1.
In correlating sequence by synthetic seismogram,wavelet,polarity and time-depth relationship are very important,but they are usually simplified by interpreter.
在合成地震记录层位标定过程中,子波、极性、时深关系是三个十分重要同时又常被解释人员简单化的问题。
2.
Finally when synthetic seismograms are successfully built, the time-depth relationships obtained can help us to check whether the adverse influences of the various factors have been completely eliminated, so as to ensures precise reservoir inversion and target prediction.
通过制作合成地震记录来标定准确的时深关系是层序地层对比和储层反演的基础。
6) Hugoniot shock velocity relation
冲击波速度关系式
补充资料：冲深
1.幽深;深奥。
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