Seismic scatterring data migration based on scattering wave equation
HU Ziduo1, YONG Xueshan1, LIU Wei1, CHEN Shengchang2, WANG Yanxiang1
1. Northwest Branch, Research Institute of Petroleum Exploration & Development, PetroChina, Lanzhou, Gansu 730020, China; 2. School of Earth Sciences, Zhejiang University, Hangzhou, Zhejiang 310027, China
Abstract:Present reverse time migration methods don’t distinguish scattering data from reflection data,and the imaging formula is established with the concept of reflected wave propagation.In this study,starting from the perturbation form of wave equation,we defined the scatterer generating scattering wave and the reflector generating reflected wave according to the relationship between the size of a underground heterogeneous body and the wavelength of seismic wave,and formulated a linear forward equation of primary scattering data,then derived the formula of calculating seismic reverse time migration on the spatial scattering location by the linear inverse theory,and finally tested the method on Sigbee2A model data.Theory and numerical test have demonstrated that the scattering data migration method can provide migration results with more correct phase and higher resolution than those from the conventional reverse time migration method based on the concept of reflection.
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