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Full-Wavefield Inversion Using Mirror Source-Receiver Geometry

机译:使用镜像源-接收器几何的全波场反演

摘要

Method for performing a full wavefield inversion (FWI) without simulating free-surface multiple reflections. The free-surface multiples are removed from the field gathers of seismic data, which are then used to generate a subsurface velocity model by FWI. In the FWI, the field monopole sources and receivers are replaced with dipole (actual and mirror image) sources and receivers (21) when model-simulating (23) synthetic survey data. Also, direct arrivals at the mirror receiver locations are preferably simulated (25) with the dipole sources for each shot location and added (26) to the synthetic survey data (24) for that shot location, resulting in corrected synthetic survey data (27), which is used in the FWI to generate residuals. A model update may be computed by back-propagating the residuals by injecting them at both mirror and actual receiver locations.
机译:在不模拟自由表面多次反射的情况下执行全波场反演(FWI)的方法。从地震数据的现场采集中删除自由表面的倍数,然后通过FWI将其用于生成地下速度模型。在FWI中,当模型模拟( 23 )综合测量数据时,场单极源和接收器被偶极(实际和镜像)源和接收器( 21 )取代。另外,最好使用每个发射位置的偶极子源模拟直接到达镜接收器位置( 25 ),并将其添加( 26 )到综合测量数据( 24 ),得到正确的综合测量数据( 27 ),该数据将在FWI中用于生成残差。可以通过在镜像位置和实际接收器位置注入残差进行反向传播来计算模型更新。

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