Nuevas observaciones en el Alpujárride del sector centro-occidental de la sierra de Carrascoy (Murcia). Consecuencias paleogeográficas

C. Sanz de Galdeano; A. C. López-Garrido; F. J. García-Tortosa; F. Delgado

doi:10.3989/egeol.97535-6229

Nuevas observaciones en el Alpujárride del sector centro-occidental de la sierra de Carrascoy (Murcia). Consecuencias paleogeográficas

Authors

C. Sanz de Galdeano Instituto Andaluz de Ciencias de la Tierra. CSIC-U.G.R. Facultad de Ciencias. Universidad de Granada.
A. C. López-Garrido Instituto Andaluz de Ciencias de la Tierra. CSIC-U.G.R. Facultad de Ciencias. Universidad de Granada.
F. J. García-Tortosa Instituto Andaluz de Ciencias de la Tierra. CSIC-U.G.R. Facultad de Ciencias. Universidad de Granada.
F. Delgado Departamento de Estratigrafía y Paleontología. Facultad de Ciencias. Universidad de Granada

DOI:

https://doi.org/10.3989/egeol.97535-6229

Keywords:

Alpujarride, Betic Internal Zone, Triassic

Abstract

The Romero and Carrascoy units defined by Kampschuur (1972) have common stratigraphic series, with several changes in its facies and thickness, although these changes are not situated in the hypothetic contact between both units. Similarly, from a tectonic point of view it is not possible to maintain the differentiation between these units, because usually they pass each other stratigraphically with no faults involved. For this reason we discard, at least in this area the differentiation between the Almagride Complex (Romero D.) and the Alpujarride (Carrascoy D.) and we thus suggest that they all belong to the Alpujarride Complex.
The structure of this area is complex, not only by the thrustings, but specially by the opposed vergences observed in the E-W folds, southwards in the northern area and progressively northwards in the southern area of the Sierra. Moreover, N-S folds verging to the W, are also observed.

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Published

1997-12-30

How to Cite

Sanz de Galdeano, C., López-Garrido, A. C., García-Tortosa, F. J., & Delgado, F. (1997). Nuevas observaciones en el Alpujárride del sector centro-occidental de la sierra de Carrascoy (Murcia). Consecuencias paleogeográficas. Estudios Geológicos, 53(5-6), 229–236. https://doi.org/10.3989/egeol.97535-6229

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Issue

Vol. 53 No. 5-6 (1997)

Section

Articles

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