首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Up/down and P/S decompositions of elastic wavefields using complex seismic traces with applications to calculating Poynting vectors and angle-domain common-image gathers from reverse time migrations
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Up/down and P/S decompositions of elastic wavefields using complex seismic traces with applications to calculating Poynting vectors and angle-domain common-image gathers from reverse time migrations

机译:利用复杂地震迹线对弹性波场进行上/下和P / S分解,并根据逆时偏移计算Poynting矢量和角域共像道集

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摘要

Separations of up-and down-going as well as of P-and S-waves are often a part of processing of multicomponent recorded data and propagating wavefields. Most previous methods for separating up/down propagating wavefields are expensive because of the requirement to save time steps to perform Fourier transforms over time. An alternate approach for separation of up-and down-going waves, based on extrapolation of complex data traces is extended from acoustic to elastic, and combined with P-and S-wave decomposition by decoupled propagation. This preserves all the information in the original data and eliminates the need for a Fourier transform over time, thereby significantly reducing the storage cost and improving computational efficiency. Wavefield decomposition is applied to synthetic elastic VSP data and propagating wavefield snapshots. Poynting vectors obtained from the particle velocity and stress fields after P/S and up/down decompositions are much more accurate than those without because interference between the corresponding wavefronts is significantly reduced. Elastic reverse time migration with the P/S and up/down decompositions indicated significant improvement compared with those without decompositions, when applied to elastic data from a portion of the Marmousi2 model.
机译:分离上下波以及P波和S波通常是处理多分量记录数据和传播波场的一部分。由于需要节省时间步长以执行随时间的傅立叶变换,因此大多数先前分离向上/向下传播波场的方法都很昂贵。一种基于复杂数据轨迹外推的分离上行波和下行波的替代方法,从声学扩展到弹性,并通过解耦传播与P波和S波分解相结合。这样可以将所有信息保留在原始数据中,并且无需随时间进行傅立叶变换,从而显着降低了存储成本并提高了计算效率。波场分解适用于合成弹性VSP数据和传播的波场快照。从P / S和上/下分解后的粒子速度和应力场获得的Poynting矢量比没有这些的Poynting矢量要精确得多,这是因为相应波阵面之间的干扰大大减少了。当将P / S和向上/向下分解的弹性逆时偏移与未分解的弹性逆时偏移相比,应用于来自Marmousi2模型一部分的弹性数据时,表明有显着改善。

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