P-wave interval velocity 纵波层速度
The purpose of migration is to inversely solve for the singularity (interrupted surface of interval velocity) of wave equation coefficient.
偏移的目的是要反演波动方程系数的奇性(层速度的间断面)。
Trace integration value represents relative wave impedance. it reflects the variation of relative interval velocity in a seismic section.
道积分值代表相对波阻抗值，它反映了地震剖面上相对层速度的变化。
The distribution of interval velocity is rich in the information of the formations through which the seismic wave transmits, and can reflect the mechanic property of the formations.
特定的层速度分布规律包含着丰富的地层信息，能不同程度地反映地层力学特性。
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