ON THE STABILITY OF FINITE-DIFFERENCE SCHEMES OF HIGHER–ORDER APPROXIMATE ONE–WAY WAVE EQUATIONS
The finite difference migration, proposed and developed by J. F. Claerbout[1], is now widely used in seismic data processing. The method has a limitation that the events are not dipping too much.
Finite-Difference Time-Domain (FDTD) methods have become a cornerstone in the simulation of electromagnetic phenomena, enabling researchers to solve Maxwell’s equations through discretisation in both ...
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