Guía rápida para el estudio de rocas deformadas a partir del análisis de la Anisotropía de la Susceptiblidad Magnética (ASM)
DOI:
https://doi.org/10.55407/rsge.94884Palabras clave:
anisotropía de la susceptibilidad magnética, rocas deformadas, deformación, elipsoide magnético, fábrica magnéticaResumen
El análisis de la Anisotropía de la Susceptibilidad Magnética (ASM) constituye una técnica rápida y no destructiva muy valiosa en geología estructural y tectónica, ya que es capaz de proporcionar información relacionada con la orientación e intensidad del elipsoide de deformación en rocas deformadas. Parte de sus ventajas son, su capacidad para (i) caracterizar rocas muy débilmente deformadas, y (ii) integrar gran cantidad de datos provenientes de grandes áreas. Desde los trabajos pioneros de los años 1950s, gran cantidad de trabajos han utilizado esta técnica en diferentes áreas de las Ciencias de la Tierra y aplicada a, prácticamente, todos los tipos de rocas existentes tanto en edad como litología. En este trabajo exploramos y mostramos el uso actual de esta técnica en geología estructural y tectónica, así como sus beneficios y limitaciones.
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