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首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Matrix-fluid decoupling-based joint PP-PS-wave seismic inversion for fluid identification
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Matrix-fluid decoupling-based joint PP-PS-wave seismic inversion for fluid identification

机译:基于基于基于基于基于的pp-ps-wave抗震反演,用于流体识别

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摘要

Seismic fluid identification is the main goal of current prestack seismic inversion. Various kinds of fluid indicators are used for fluid detection in industry today. However, the existing methods cannot always provide reliable fluid prediction owing to the insensitivity to fluid response and the lack of converted wave constraints. The equivalent fluid bulk modulus is an effective fluid factor based on matrix-fluid decoupling, which can provide persuasive evidence for fluid detection. Combining poroelasticity theory and matrix-fluid decoupling theory, we have deduced a new PS-wave linear amplitude versus offset approximation equation that provides estimations of equivalent fluid bulk modulus, rigidity, porosity, and density. Then, the joint inversion of PP-and PS-waves based on matrix-fluid decoupling was executed in a Bayesian framework with constraints from rock physics and well-log data obtaining elastic parameter estimation of high precision directly. We tested the new method on a synthetic example and field multicomponent data, and the results indicated that the estimated fluid factor matched with well-data interpretation and geology information because of adding converted wave information and avoiding indirect inversion error. This demonstrated that the new method can enhance the quality of fluid detection and provide reliable geophysical evidence for reservoir characterization.
机译:地震液体识别是当前普雷斯特克地震反演的主要目标。各种流体指示器用于当今工业中的流体检测。然而,由于对流体反应的不敏感和缺乏转换的波约,现有方法不能总是提供可靠的流体预测。等效流体体积模量是基于基质流体去耦的有效流体因子,其可以为流体检测提供有说服力的证据。组合Poro弹性理论和矩阵流体去耦理论,我们推导了一种新的PS波线性振幅与偏移近似方程,提供了等效流体体积模量,刚性,孔隙率和密度的估计。然后,基于基于矩阵流体去耦的PP-和PS波的联合反演在贝叶斯框架中执行,其具有从岩石物理学和井 - 日志数据直接获得高精度的弹性参数估计的限制。我们在合成示例和字段多组分数据上测试了新方法,结果表明,由于添加转换的波信息并避免间接反转误差,估计流体因子与良好的数据解释和地质信息匹配。这证明了新方法可以提高流体检测的质量,并为储层特征提供可靠的地球物理证据。

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