| abstract |
A method for modeling geological structures includes obtaining seismic data, (12), and using this data to derive an initial density model, (14). Potential field data is used to update the initial geophysical model by an inversion process using vector or tensor components of gravity or magnetic data, (46). Potential field data is used to derive the lower boundary of the anomalous density zones by using an inversion process derived from the initial model of the top topographic or bathymetric surface with the 2D or 3D density model including any zones of anomalous density, (44). The final density model from the inversion may be further refined using the seismic data in conjunction with the model obtained by inversion of the potential fields data. The model data are integrated two or three dimensions to determine an overburden stress for the subsurface that includes a proper treatment of the anomalous density zone. The seismic data can be processed in depth or time using the density model from the inversion to improve the quality of the velocity information adjacent to the anomalous bodies. The velocity measurements are used to determine the effective stress and the fluid pressure is obtained as the difference between the overburden stress and the effective stress. |