反射界面及层速度是地震勘探中相当重要的地层参数。
Reflection interface and interval velocity are quite important stratigraphic parameters in seismic exploration.
线性化反演是通过从反射界面深度由分离速度参数迭代进行的。
The linearized inversion was undertaken by DE coupling velocity parameters from reflector depths.
当反射界面上下两侧的声波组抗降低时，反射系数就会出现负值。
Negative coefficients occur where there is a decrease in acoustic impedance across the reflecting interface.
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