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Real data waveform inversion in crossholeseismic tomography

机译:跨孔层析成像中的真实数据波形反演

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摘要

Conventional crosshole tomography uses travel times and ray tracing to produce quantitative but low-resolutionrnvelocity images of the subsurface. In contrast, full-wavefield tomographic techniques seekrnto determine a highly-resolved, quantitative model of the subsurface that is able to explain the entirernseismic wavefield including those phases that conventional processing and migration seek to remove.rnSuch methods have the potential to image the subsurface with significantly improved spatialrnresolution, to provide fully quantitative images of physical properties in the subsurface, especiallyrntime-lapse, high-resolution imaging of the reservoir. We seek to provide a computationally tractablernsolution to this problem, using existing computer hardware, that will allow practical full-wavefieldrnimaging of a crosshole seismic dataset which has typically thousands shots and each has hundredsrnreceivers.
机译:传统的井孔层析成像使用传播时间和射线追踪来生成地下的定量但低分辨率的速度图像。相比之下,全波场层析成像技术试图确定一种高度分辨的地下定量模型,该模型能够解释整个地震波场,包括常规处理和运移力图去除的那些相位。显着提高了空间分辨率,以提供地下物理特性的完全定量图像,尤其是储层的延时高分辨率图像。我们试图使用现有的计算机硬件为该问题提供一个计算上可解决的解决方案,该解决方案将允许对跨孔地震数据集进行实际的全波场成像,该数据集通常具有数千张炮弹,每个接收器具有数百个接收器。

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