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ELASTIC FULL WAVEFIELD INVERSION WITH REFINED ANISOTROPY AND VP/VS MODELS

机译:具有精细各向异性和VP / VS模型的弹性全波场反演

摘要

Methods for inversion of seismic data to infer subsurface physical property parameters, comprising constructing an inhomogeneous anisotropy model and/or inhomogeneous VS/VP or VP/VS model; and inverting the seismic data in a sequential or simultaneous approach to obtain at least one subsurface physical property parameter using an elastic inversion algorithm and the inhomogeneous anisotropy model and/or inhomogeneous VS/VP or VP/VS model. Constructing an inhomogeneous anisotropy model may comprise deriving geobodies from at least one of seismic facies analysis, regional geologic information, or seismically derived earth models; and adjusting at least one of ε, δ, γ, or parameters of the elastic stiffness tensor matrix in a homogeneous anisotropy model in areas corresponding to the geobodies. Constructing an inhomogeneous VS/VP or VP/VS model may comprise deriving geobodies and adjusting values in a homogeneous VS/VP or VP/VS model in areas corresponding to the geobodies.
机译:地震数据反演以推断地下物理性质参数的方法,包括构造不均匀的各向异性模型和/或不均匀的V S / V P 或V P / V S 模型;使用弹性反演算法和非均质各向异性模型和/或非均质V S / V P <,以顺序或同时方式对地震数据进行反演,以获得至少一个地下物理属性参数。 / Sub>或V P / V S 模型。构造非均质各向异性模型可以包括从地震相分析,区域地质信息或地震推导的地球模型中的至少一种推导地质体。在均质各向异性模型中,在对应于地质体的区域中,调整ε,δ,γ或弹性刚度张量矩阵的参数中的至少一个。构造不均匀的V S / V P 或V P / V S 模型可能包括推导地体和调整值在对应于地理主体的区域中的均质V S / V P 或V P / V S 模型中。

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