Method for processing seismic exploration data in process of controlling full acoustic wave equation inversion
A technology of inversion process and seismic exploration, applied in the field of seismic exploration data processing, which can solve the problems of increasing computing cost and the number of iterations cannot be allowed.
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[0069] The theoretical model is a three-layer medium model, figure 2 The black curve in the middle is the variation curve of the parameters of the three-layer medium model with depth. image 3 Synthesize seismic data for the theoretical model and invert the data. The specific implementation steps are as follows:
[0070] 1. Collect theoretical model seismic data, extract common center point gather data, perform velocity analysis, time-domain layer velocity calculation and time-depth conversion, and obtain the initial model of bulk modulus and density in the depth domain;
[0071] 2. Based on the initial model, use the pseudospectral method to simulate the seismic wave field in the acoustic medium;
[0072] 3. Calculate the difference between the theoretical model and the initial model simulation data according to formula (5);
[0073] 4. Given δ=1.0e-6, calculate the error energy E according to formula (6), when E≤δ, stop the inversion and output the inversion result, if E>...
example 2
[0081] Example 2 is a gas field located in the west of my country. The gas field is a continental lacustrine deposit with well-developed underwater distributary channels. The target layer has a large burial depth, a long burial time, a high degree of diagenetic evolution, and poor physical properties. It is a typical gas field with low porosity and low permeability. The reservoir is thick vertically and distributed over a large area on the plane, but the single layer of effective sandstone is thin, with large lateral variation and strong heterogeneity. Sedimentary microfacies, physical property analysis and gas test results confirm that effective reservoirs are mainly developed in high-energy distributary channels in the delta plain and delta front subfacies.
[0082] Due to the small difference in P-wave velocity and impedance between the effective reservoir and surrounding rock, conventional seismic inversion results cannot meet the requirements of exploration. In 2006, we...
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