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Revisión de las unidades alpujárrides de las Sierras de Tejeda, Almijara y Guájares (sector central de la Zona Interna Bética, provincias de Granada y Malaga)

Authors: Sanz de Galdeano, Carlos; López-Garrido, A. C.;

Revisión de las unidades alpujárrides de las Sierras de Tejeda, Almijara y Guájares (sector central de la Zona Interna Bética, provincias de Granada y Malaga)

Abstract

[ES] Se discuten el significado, las correlaciones hechas anteriormente y los límites de las diversas unidades que se han distinguido en las sierras de Tejeda, Almijara, Guájares y Albuñuelas (provincias de Granada y Málaga), en particular de las denominadas uilidades de Herradura y Salobreña del Complejo Alpujárride. Dichas unidades no se pueden separar de forma objetiva sobre el terreno, por lo que, en sustitución de ellas se propone el uso del nombre de unidad de Almijara. Tiene esta unidad una estructura muy compleja en la parte occidental, con vergencias al sur en su parte norte, especialmente en las Sierras Tejeda y Almijara, y al norte en el sur. En el sector oriental, en la Sierra de los Guájares, la estructura es mucho más simple, casi tabular. Bajo ella se sitúa la unidad de Escalate y encima la de los Guájares a la cual hay que atribuir algunos de los afloramientos que se consideraban de la unidad de Salobreña, tal como son los que se encuentran en la localidad de ese nombre. Por el contrario, el sector de las Llanadas, al sur de Pinos del Valle, antes considerado del manto de los Guájares, pertenece a la unidad de Almijara. En conjunto, se eliminan supuestos contactos de mantos dentro de los mármoles de las sierras de Almijara y de Guájares-Guindalera y se delimita la unidad de Almijara.

[EN] The meaning, the previous correlations and the limits among different units distinguished in the Tejeda, Almijara, Guájares and Albuñuelas sierras in the Granada and Málaga provinces (with an area of about 1500 km2) are discussed, particularly the so called Herradura and Salobreña Units, within de Alpujarride Complex. Some previous supossed tectonic thrust contacts within the carbonates of the Almijara and Guajares-Guindalera sierras do not exist. The comclusion is that several of these units cannot be objectively separate in the field and therefore are included together in the Almijara Unit. This unit shows a very complex structure in its western part, especially in the Tejeda and Almijara sierras, with southwards vergences in its north side and northwards in its south sector. In the eastern sector the structure is simpler, nearly tabular. In its bottom appear the Escalate unit and to the top that of the Guajares. Some of the outcrops previously considered belonging to the Salobreña unit are now included in the Guajares Nappe. The Llanadas sector, previously considered forming part of the Guajares Nappe, really belongs to the Almijara unit.

Este artículo ha sido financiado por los grupos RNM 0163 y 217 de la Junta de Andalucía.

15 páginas, 9 figuras, 1 tabla.

Peer reviewed

Keywords

Betic Cordillera, Cordillera Bética, Betic internal zone, Alpujarride, Zona interna Bética

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This is an alternative to the "Influence" indicator, which also reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
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popularity
This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network.
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influence
This indicator reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
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