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espanolEn la parte occidental de la Sierra de los Filabres (perteneciente al Complejo Nevado-Filabride, en la Zona Interna Betica) se han descrito diversas unidades tectonicas, en muchos casos diferentes de un autor a otro. Sin embargo, una nueva cartografia permite concluir que todos los limites de estas unidades pasan a traves de las formaciones litologicas que alli existen sin desplazarlas. Ademas, rocas atribuidas a algunas unidades que se consideran en una posicion tectonica inferior realmente pertenecen a formaciones altas. Estas formaciones son, de abajo arriba: 1) esquistos oscuros y cuarcitas, 2) cuarcitas, areniscas, arenas, lutitas, esquistos y micacitas, 3) esquistos y 4) marmoles, esquistos y micacitas. Fallas inversas de alto angulo se asocian con el gran anticlinal E-O de la Sierra de los Filabres. La presencia de arenas y de las aparentes lutitas intercaladas entre rocas tales como esquistos y micacitas con granates plantea un problema metamorfico no abordado hasta el momento. EnglishIn the western part of Sierra de los Filabres (in the Nevado-Filabride Complex, within the Betic Internal Zone) several tectonic units have been described, in varying numbers depending on the author describing them. However, new cartographical data show that the limits of these units pass through the lithological formations without displacing them. Moreover, the rocks belonging to some units that are supposedly situated in a lower tectonic position really belong to higher formations. From bottom to top, these lithological formations are the following: (1) dark schists and quartzites; (2) quartzites, sandstones, sands, lutites, schists, and mica schists; (3) schists; (4) marbles, schists, and mica schists. High-angle reverse faults are associated with the great E-W anticline of Sierra de los Filabres. The existence of sands and apparent lutites visibly interlayered between rocks, such as schists and mica schists with garnets, poses a metamorphic problem that has not as yet been addressed.

The nevado-filábride complex in the western part of Sierra de los Filabres (Betic Internal Zone), structure and lithologic succession