Caracterización de la roca soporte de los petroglifos de Campo Lameiro (Pontevedra)

  1. Benita Silva 1
  2. Patricia Sanmartín 1
  3. Beatriz Prieto 1
  1. 1 Departamento de Edafoloxía e Química Agrícola. Universidade de Santiago de Compostela (España)
Revista:
Cadernos do Laboratorio Xeolóxico de Laxe: Revista de xeoloxía galega e do hercínico peninsular

ISSN: 0213-4497

Ano de publicación: 2019

Número: 41

Páxinas: 141-152

Tipo: Artigo

DOI: 10.17979/CADLAXE.2019.41.0.5821 DIALNET GOOGLE SCHOLAR lock_openAcceso aberto editor

Outras publicacións en: Cadernos do Laboratorio Xeolóxico de Laxe: Revista de xeoloxía galega e do hercínico peninsular

Resumo

Between 2005 and 2008 a research project about the deterioration causes of the petroglyphs of Campo Lameiro (Pontevedra) was developed. The substrate of the carvings was characterised as a two mica-granite, fine to medium grained, with granular allotriomorphic texture. Intense cracking is present in the rock at all levels, which is responsible of its high porosity and therefore its high capacity to absorb water. A dense network of diaclases was observed on site, however a specific study revealed that this does not involve a risk of massive loss of rock, which might affect the carved surfaces. The mineralogical and geochemical analysis showed that the granite was subjected to processes of hydrolysis and solubilisationprecipitation of iron, showing that water is the main deterioration agent in the lithic material.

Referencias bibliográficas

  • Bellido Mulas, F., González Lodeiro, F., Klein, E., Martínez Catalán, J.R., Pablo Macía, J.G. (1987). Las rocas graníticas hercínicas del Norte de Galicia y occidente de Asturias. Colección Memorias. Tomo 101. IGME.
  • Benavente, D., García Del Cura, M. A., Fort, R., Ordóñez, S. (2004). Durability estimation of porous building stones from pore structure and strength. Engineering Geology 74 (1), 113-127.
  • Capdevila, R., Floor, P. (1970). Les different types de granites hercyniens et leur distribution dans le nor-ouest de Espagne [The different types of Hercynian granites and their distribution in the north-west of Spain]. Boletín Geológico y Minero, 81, 215-225.
  • Costa-Casais, M., Martínez-Cortizas, A., Pontevedra-Pombal, X., Criado-Boado, F. (2009). Analysis of landforms in geoarchaeology: Campo Lameiro, NW Iberian Peninsula. Memorie Descrittive della Carta Geologica d'Italia LXXXVII: 39-52.
  • Grant, W.H. (1969). Abrasion pH, an index of chemical weathering. Clays and Clay Minerals, 17, 151-155.
  • R.I.L.E.M. (1980). Essais recommandés pour mesurer l'altération des pierres et évaluer l'eficacité des méthodes de traitements. Matériaux et Constructions, Bull. RILEM, 13 (75), pp. 216-220.
  • Romero, R., Taboada, T., García, C., Macías, F. (1987). Utilización del pH de abrasión como un índice del grado de evolución de la alteración y edafogénesis en suelos graníticos de la provincial de La Coruña. Cadernos do Laboratorio Xeolóxico de Laxe, 11, 171-182.
  • UNE-EN 1936:1999. Natural stone test methods, Determination of real density and apparent density, and of total and open porosity, AENOR (Spanish Association for Standardisation and Certication).
  • Wilson, M. J. (2004). Weathering of primary rock forming minerals: processes, products, and rates. Clay Minerals, 39, 233-266.