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• W2765966430 abstract "There is significant uncertainty in measuring the Thomsen’s parameter δ in laboratory even though the dimensions and orientations of the rock samples are known. It is expected that more challenges will be encountered in the estimating of the seismic anisotropy parameters from field seismic data. Based on Monte Carlo simulation of vertical transversely isotropic layer cake model using the database of laboratory anisotropy measurement from the literature, we apply the commonly used quartic non-hyperbolic reflection moveout equation to estimate the seismic anisotropy parameters and test its accuracy and sensitivities to the source-receive offset, vertical interval velocity error and time picking error. The testing results show that the methodology works perfectly for noise-free synthetic data with short spread length. However, this method is extremely sensitive to the time picking error caused by mild random noises, and it requires the spread length to be greater than the depth of the reflection event. The uncertainties increase rapidly for the deeper layers and the estimated anisotropy parameters can be very unreliable for a layer with more than five overlain layers. It is possible that an isotropic formation can be misinterpreted as a strong anisotropic formation. The sensitivity analysis should provide useful guidance on how to group the reflection events and build a suitable geological model for anisotropy parameter inversion." @default.
• W2765966430 created "2017-11-10" @default.
• W2765966430 creator A5007524574 @default.
• W2765966430 creator A5028752346 @default.
• W2765966430 date "2018-02-13" @default.
• W2765966430 modified "2023-09-27" @default.
• W2765966430 title "Accuracy and sensitivity analysis on seismic anisotropy parameter estimation" @default.
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• W2765966430 doi "https://doi.org/10.1088/1742-2140/aa93b1" @default.
• W2765966430 hasPublicationYear "2018" @default.
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