Today such gravitational compensation probably would not occur: the outer layerof the Moon is too cold and stiff.
今天这种引力补偿很有可能不会发生：月球的外层过于寒冷和坚硬。
2
In order to preserve the relative intensity in - formation in raw seismic data, we can consider the sea-bottom reflection as reference layer to estimate the compensation value of target stratum.
为了保持原始地震记录的相对强度，可以稳定的海底反射波作参考层，估算目的层的补偿值。
3
Weathered layer absorbs seismic waves greatly. Compensation for the absorption due to weathered layer can improve resolution of seismic data.