Granites employed in Ávila-Spain. I. Chemical composition of the different types
DOI:
https://doi.org/10.3989/mc.1994.v44.i233.594Abstract
The chemical composition of the different types of granite employed in the Cathedral and buildings of historic and artistic interest in Avila (Spain) is studied. The differences among the various fades studied (grey, ochre and bloodstone granites) are explained in terms of their different mineralogical composition, a result of the profound paleoweathering that occurred in the Iberian Hercynian Basement. The chemical differences between quarry stone and the samples taken from different parts of the buildings are due to weathering processes that occurred on the buildings. Among these, the precipitation of salts in humid zones and the effect of alkaline mortar on the varieties rich in opal are striking.
Downloads
Downloads
Published
How to Cite
Issue
Section
License
Copyright (c) 1994 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.