Abstract: A method and system for simulating and optimizing land seismic survey operations. The method and system utilizes spatially referenced data and nonspatial data relevant to land seismic survey operations such as high resolution satellite and airborne imagery and uses discrete event information about land seismic survey operation to simulate a land seismic survey. The output of the simulation is a detailed list of survey events. Mathematical optimization techniques are used to enhance the efficiency of the survey execution via optimal route planning and optimal allocation of survey logistical components. The invention uses a discrete event simulator which is an object-oriented software program with survey geometry objects that represent the survey design, resources objects that represent resources needed to conduct survey operations and manager objects to coordinate the resource objects within the specified survey geometry.

Abstract: A method for 3 dimensional, one pass migration of post stack seismic data is implemented on a massively parallel computer. The quality of the migration and speed of execution makes possible iterative 3D post stack depth migrations. The depth migration method computes in the frequency domain and downward continues one or more frequency planes through all depth levels of interest. For a single frequency, at each depth level, the method extrapolates a shifted position for each x,y position by applying a filter for 2D convolution. A processing component is assigned to each subgrid of x,y spatial positions and the processing components operate concurrently in parallel to determine filter coefficients independently for each x,y spatial position and to extrapolate the x,y shifted positions. The filter coefficients are derived independently at each x,y position by storing a limited table of filter coefficients in local memory of each processing component.

Abstract: A method for 3 dimensional, one pass migration of post stack seismic data is implemented on a massively parallel computer. The quality of the migration and speed of execution makes possible iterative 3D post stack depth migrations. The depth migration method computes in the frequency domain and downward continues one or more frequency planes through all depth levels of interest. For a single frequency, at each depth level, the method extrapolates a shifted position for each x,y position by applying a filter for 2D convolution. A processing component is assigned to each subgrid of x,y spatial positions and the processing components operate concurrently in parallel to determine filter coefficients independently for each x,y spatial position and to extrapolate the x,y shifted positions. The filter coefficients are derived independently at each x,y position by storing a limited table of filter coefficients in local memory of each processing component.