AVO AND AVA INVERSION FOR FRACTURED RESERVOIR CHARACTERIZATION

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dc.contributor.author Beretta M.M.
dc.contributor.author Bernasconi G.
dc.contributor.author Drufuca G.
dc.date.accessioned 2021-05-24T06:54:05Z
dc.date.available 2021-05-24T06:54:05Z
dc.date.issued 2002
dc.identifier https://www.elibrary.ru/item.asp?id=13980143
dc.identifier.citation Geophysics, 2002, 67, 1, 300-306
dc.identifier.issn 0016-8033
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/28675
dc.description.abstract Seismic wave reflection amplitudes are used to detect fluids and fracture properties in reservoirs. This paper studies the characterization of a vertically fractured fluid-filled reservoir by analyzing the reflection amplitudes of P-waves with varying incident and azimuthal angles. The reservoir is modeled as a horizontal transversely isotropic medium embedded in an isotropic background, and the linearized P-waves reflection coefficient are considered. The conditioning of the inverse problem is analyzed, and fracture density is found to be the best conditioned parameter. Using diffraction tomography under the Born approximation, an inversion procedure is proposed in the transformed k-ω domain to detect fracture density variations within the reservoir. Śeismic data are rearranged in pairs of incident and reflected plane waves, enlightening only one spectral component of the fracture density field at a time. Only the observable spectral components are inverted. Moreover, working in the transformed domain, picking reflection amplitudes is not required. An example of the inversion applied to a synthetic data set is presented. The limitation of source and receiver numbers and the finite bandwidth of the wavelet produce a loss of resolution, but the overall fracture density variations are recovered correctly.
dc.title AVO AND AVA INVERSION FOR FRACTURED RESERVOIR CHARACTERIZATION
dc.type Статья


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