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1D viscoelastic waveform inversion for Q structures from the surface seismic and zero-offset VSP data

机译:利用表面地震和零偏移VSP数据对Q结构进行一维粘弹性波形反演

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摘要

Wave attenuation is an important physical property of hydrocarbon- bearing sediments that is rarely taken into account in site characterization with seismic data. We present a 1D viscoelastic waveform inversion scheme for determining the quality factor Q from the normal-incidence surface seismic and zero-offset vertical seismic profile VSP data simultaneously. The joint inversion problem is solved by the damped least-squares method, and the inversion result is successful using synthetic data. The effects of initial model thickness,Q value, and the existence of noise were studied through a synthetic example. By extracting all of the information contained in the waveforms, the waveform inversion of the seismic reflection and transmission data becomes a powerful tool for estimating Q. For a more comprehensive image of Q, the tomographic inversion of Q is applied to the walkaway VSP and prestack surface seismic data, using the waveform inversion result as the initial model. Results from applying the method to a real seismic line and zero-offset VSP data from the Nanyang oilfield, central China, indicate that Q from the tomographic inversion of reflection and transmission data contains useful information on medium properties, which can aid in reservoir appraisal.
机译:波衰减是含烃沉积物的重要物理性质,在地震数据的现场表征中很少考虑。我们提出了一种一维粘弹性波形反演方案,用于同时从法向入射地表地震和零偏移垂直地震剖面VSP数据确定品质因数Q。用阻尼最小二乘法解决了联合反演问题,利用合成数据成功反演了结果。通过一个综合实例研究了初始模型厚度,Q值和噪声存在的影响。通过提取波形中包含的所有信息,地震反射和传输数据的波形反演成为估算Q的有力工具。对于更全面的Q图像,将Q的断层摄影反演应用于步入式VSP和叠前地面地震数据,使用波形反演结果作为初始模型。通过将该方法应用于真实地震线和来自中国中部南洋油田的零偏移VSP数据的结果表明,来自反射和透射数据的层析X射线反演的Q包含有关介质性质的有用信息,可以帮助进行储层评估。

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