多波多分量地震地质层位对比是多波地震资料解释和应用中最关键、最基础的工作。
The geologic correlation of multiwave and multicomponent seismic data is the most important and fundamental work.
通过合成地震记录将地质层位标定到地震剖面上，在井资料与地震资料之间建立准确的对应关系。
Through synthetic seismogram we can use geological horizon calibrate the seismic profile, and establish the corresponding relationship between seismic data and geological data.
由于榴辉岩与其他岩石类型之间存在较大的波阻抗差异，因此用零偏VSP资料标定该区地震波的地质层位是有效的。
Since large impedance contrasts exist between eclogite and other rocks, it is effective that the VSP profiles are used to calibrate geological horizons of seismic reflections.
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