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ROBUST FULL WAVEFORM INVERSION OF SEISMIC DATA METHOD AND DEVICE

机译:地震数据的鲁棒全波形反演方法及装置

摘要

A method for calculating a velocity model for a subsurface of the earth. The method includes receiving (200) measured seismic data d; calculating (204) predicted seismic data p; selecting (206) a matching filter w that when applied to one of the measured seismic data d or the predicted seismic data p reproduces the other one of the measured seismic data d or the predicted seismic data p; selecting (208) a misfit function J that calculates (1) a distance between the matching filter w and a Dirac Delta function or (2) a travel time shift associated with the measured seismic data; and calculating (218) a new velocity model using the misfit function J, the measured seismic data d, and the predicted seismic data p. The measured seismic data d includes wavefields generated by a seismic source and the wavefields propagate through the subsurface where they are attenuated and reflected, and the attenuated and reflected wavefields are recorded by plural seismic receivers.
机译:一种用于计算地球地下速度模型的方法。该方法包括接收(200)测量的地震数据d;以及计算(204)预测地震数据p;选择(206)匹配滤波器w,该匹配滤波器w当应用于测量的地震数据d或预测的地震数据p之一时,再现另一个测量的地震数据d或预测的地震数据p;选择(208)失配函数J,该失配函数J计算(1)匹配滤波器w和狄拉克增量函数之间的距离,或者(2)与所测量的地震数据相关联的行进时间偏移;并使用失配函数J,测得的地震数据d和预测的地震数据p计算(218)新的速度模型。测得的地震数据d包括由地震源产生的波场,并且该波场传播通过地下并在其中被衰减和反射,并且由多个地震接收器记录衰减和反射的波场。

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