Estructura y estratigrafía de la sierra de los Guajares y sectores próximos (Conjunto Alpujarride, Cordilleras Béticas)
DOI:
https://doi.org/10.3989/egeol.90461-2444Keywords:
Thrusts, Alpujarride Complex, Betic CordillerasAbstract
The Guajares and Chaparral-Guindalera Sierras are mainly formed by carbonatic materials, of Middle and Upper Triassic (and perhaps of the Lower Liassic) age, belonging to the Almijara Unit (Alpujarride Complex). Their structure is mainly formed by thrust-slides (and younger faults affecting them). The Almijara Unit is overthrusted by the Guajares Unit (including in this Unit the Salobreña Sub-unit). In its thrusting, the Guajares Unit, is progressively situated over more modern materials of the Almijara Unit, inducing in it other lesser trust-slides. Boths units, Almijara and Guajares, overthrusted the Escalate Unit (with an approximate NNW to NW direction and sense) causing important tectonic thinning.
Downloads
Downloads
Published
How to Cite
Issue
Section
License
Copyright (c) 1990 Consejo Superior de Investigaciones Científicas (CSIC)
This work is licensed under a Creative Commons Attribution 4.0 International License.
© CSIC. Manuscripts published in both the print and online versions of this journal are the property of the Consejo Superior de Investigaciones Científicas, and quoting this source is a requirement for any partial or full reproduction.
All contents of this electronic edition, except where otherwise noted, are distributed under a Creative Commons Attribution 4.0 International (CC BY 4.0) licence. You may read the basic information and the legal text of the licence. The indication of the CC BY 4.0 licence must be expressly stated in this way when necessary.
Self-archiving in repositories, personal webpages or similar, of any version other than the final version of the work produced by the publisher, is not allowed.
