VTI介质微震资料三维波形反演

O. Michel, I. Tsvankin
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引用次数: 1

摘要

三维各向异性波形反演(WI)可以为微地震调查提供高分辨率的速度模型和改进的事件定位。在这里,我们将之前开发的用于微地震井眼数据的二维WI方法扩展到三维各向异性模型。这种扩展使我们能够反演在多个井眼中记录的多分量数据,并适当地解释垂直和横向的非均质性。综合算例说明了该三维算法对层饼和“水力压裂”VTI(横各向同性,垂直对称轴)模型的性能。在这两种情况下,WI都能够重建模型的部分,这些部分对于所采用的源接收器几何结构来说是充分照明的。我们还介绍了页岩区数据集的初步结果,并描述了使地震图适合波形反演所需的一系列处理步骤。经过预处理后,观测到的和模拟的直接到达具有相似的振幅和相位特征,可以用于速度分析。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
3D waveform inversion of microseismic data for VTI media
3D anisotropic waveform inversion (WI) could provide high-resolution velocity models and improved event locations for microseismic surveys. Here we extend our previously developed 2D WI methodology for microseismic borehole data to 3D anisotropic models. This extension allows us to invert multicomponent data recorded in multiple boreholes and properly account for vertical and lateral heterogeneity. Synthetic examples illustrate the performance of the 3D algorithm for layer-cake and “hydraulically fractured” VTI (transversely isotropic with a vertical symmetry axis) models. In both cases, WI is able to reconstruct parts of the model which are sufficiently illuminated for the employed source-receiver geometry. We also present preliminary results for a data set from a shale play and describe a sequence of processing steps needed to make the seismograms suitable for waveform inversion. After the preprocessing, the observed and modeled direct arrivals exhibit comparable amplitude and phase characteristics and can be used for velocity analysis.
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