Estudio geológico revela que la península ibérica gira lentamente en sentido horario debido a tensiones tectónicas
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Summary
Un estudio científico basado en el análisis de terremotos revela que la península ibérica está experimentando un lento giro en sentido horario. Este movimiento se atribuye a las tensiones tectónicas generadas por la convergencia entre las placas de África y Eurasia. La investigación también examina la evolución tectónica de la región desde la fragmentación de Pangea, ofreciendo nuevas perspectivas sobre la dinámica geológica de la península.
Key quotes
· 2 pulledEste desplazamiento se debería a las tensiones tectónicas generadas por la convergencia entre África y Eurasia.
También se estudia la evolución tectónica de la región desde la fragmentación de Pangea
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