Variaciones de la anisotropia de la susceptibilidad magnética en turbiditas albienses de la Cuenca Vasco-Cantábrica
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Abstract
The first results extracted from the study of the Anisotropy of magnetic susceptibility (ASM) from 33 turbidites allocated in Basque-Cantabrian basin show the validity of the ASM as a rock fabric analysis tool to determine deposit mechanism and paleocurrents in turbidites
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