Static computation is a key step to deal with coalfield seismic data of complex surface conditions. 复杂地表条件煤田地震数据处理的静校正计算是解决地质问题的关键性步骤。
The tomographic inversion of the surface layer velocity model with the first break is the important base of the tomographic static correction. 初至波表层速度模型层析反演是层析静校正的重要基础。