Abstract
The induction seismomagnetic effects arising in the seismic wave motion in the constant Earth's magnetic field are numerically studied in this article. The phenomenon is described as a simultaneous solution of the system of elastic equations and quasi-stationary Maxwell's equations with displacement velocity components. For solving the problem, we use numerical-analytical algorithm based on the finite Fourie transform. The obtained system of ordinary differential equations is solved by the factorization method.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have