Standard stacking procedures are based on the combination of many scalar traces, and can exploit the coherency of arrivals between traces using non-linear methods. Such stacks can be used with some success for three-component data but do not exploit the vector character of the seismic wavefield. A set of stacking methods are introduced to work directly with three-component data and include intercomponent coherency through 3 x 3 matrix measures. These techniques include extensions of both...[Show more]
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