摘要

Near surface high resolution imaging in seismic data processing is attracting great attention. Reverse time migration (RTM) from two way wave equation is considered a good way to image the steep structure. However low frequency noise generated during the RTM imaging process is relatively high, which affects high resolution imaging of near surface. To challenge this problem, we propose in this paper a least square reverse time migration (LSRTM) method. Test results on a complex near surface velocity model indicate that LSRTM is much better than RTM for structure high resolution imaging and energy preservation.