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Abstract

Las caraoteristicas geotectónioas de una cuenca sedimentaria están dadas por su evoluoión de subsidencia y efectos de acumulacion de tensiones en la parte superior de la corteza. Los relevamientos geomagneticos locales en los bordes de dicha cuenca permiten observar estos efectos con el fin de conocer particularidades de la evoluoión de las anomalias.

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/content/papers/10.3997/2214-4609-pdb.317.sbgf095
1989-11-20
2024-04-20

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