Caracterización sedimentológica de un nivel guía y su posible origen sísmico, Corredor del Almanzora (Almería).

• Autores: Fernando Sola
• Localización: Geogaceta, ISSN 0213-683X, Nº. 49, 2010, págs. 31-34
• Idioma: español
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• Resumen

  • A conglomeratic level intercalated in a turbiditic sequence in the Almanzora corridor (Betic Cordillera) has been mapped. This level is 3 to 15 m thick, with clasts bigger than 3 m diameter. It can be continued along 6 km, which makes it being a good key bed in the study area. The level origin has been interpreted as a collapse deposit from the southern margin of the basin, probably due to a seismic event.