Characterization method of fractured-vuggy reservoirs in carbonate rock surface
A technology for carbonate rock and fracture-cavity reservoirs, applied in complex mathematical operations, seismology for logging records, seismic signal processing, etc., can solve problems that cannot accurately reflect the spatial distribution of surface fracture-cave bodies and surface reservoirs Collectively characterize leakage and other problems to achieve the effect of improving the coincidence rate and improving the recovery rate
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Embodiment 1
[0053] In order to solve the above-mentioned technical problems existing in the prior art, an embodiment of the present invention provides a method for characterizing fracture-vug reservoirs on the surface of carbonate rocks.
[0054] figure 1 A flow chart of the method for characterizing fractured-vuggy reservoirs on the surface of carbonate rocks according to Embodiment 1 of the present invention is shown.
[0055] refer to figure 1 In this embodiment, the fracture-vuggy reservoir description method on the surface of carbonate rocks includes:
[0056] Step S1: Calculate the root mean square amplitude attribute in the first depth range of the carbonate rock surface.
[0057] Step S2: Calculate the relative wave impedance property in the second depth range of the carbonate rock surface.
[0058] Step S3: Establish a regression function between the root mean square amplitude attribute and the relative wave impedance attribute.
[0059] Specifically, through the RMS amplitud...
Embodiment 2
[0068] In this embodiment, on the basis of the first embodiment, steps S1-S3, S5 are further limited, and step S4 is further defined differently from the first embodiment.
[0069] In this embodiment, the method for describing fractured-vuggy reservoirs on the surface of carbonate rocks includes:
[0070] Step S1 : Calculating the root mean square amplitude attribute in the first depth range of the carbonate rock surface.
[0071] Specifically, according to the original seismic data volume in the first depth range of the carbonate rock surface layer, the root mean square amplitude value in the first depth range of the carbonate rock surface layer is obtained; the obtained root mean square amplitude value is reciprocated , and the reciprocal of the root mean square amplitude value is homogenized to obtain the root mean square amplitude attribute in the first depth range of the carbonate rock surface. Among them, the calculation of the root mean square amplitude value is: squar...
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