Two dimensional finite difference simulation of magnetotelluric and magnetic variation soundings when the source field is considered
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Se describe un algoritmo de diferencias finitas en dos dimensiones para simular sondeos magnetotelúricos (MT) y de variaciones magnéticas (VM). Este algoritmo fue desarrollado con el objeto de comparar estudios de resistividad aparente realizados con uno y otro método. Se considera una fuente de campo con geometría finita. Se presentan resultados de una simulación de este tipo de sondeos en Islandia para ilustrar las aplicaciones de este algoritmo.
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