Geophysical methods as a tool for improving our knowledge of ornamental rock deposits and their exploitation
DOI:
https://doi.org/10.21701/bolgeomin.128.2.006Keywords:
borehole, deposit, geophysics, ornamental stone, resistivityAbstract
The ornamental rock sector, particularly the investigation of deposits, is not readily given to the incorporation of new technologies. The Marble Technology Center (CTM) has made advances in this sector with the implementation of geophysical techniques able to obtain subsurface information. There are still a few outcrops and active quarries where joint geophysical techniques have been applied sufficiently to obtain a three-dimensional model of the study area.
The application of geophysics and more specifically, ground penetrating radar, electrical tomography and seismic refraction, when conducting research of a reservoir or outcrop, is only slightly aggressive to the environment, allowing a real knowledge of the characteristics before beginning the more aggressive work, as is the case when conducting surveys and test pits which can subsequently complement the data obtained. This makes it possible to gain a good idea of the quality of the reservoir thus allowing optimization of resources, both financial and environmental beforehand.
Several studies conducted by the CTM illustrate the benefits brought by the application of these geophysical techniques as well as the weaknesses within the characteristics of the extraction sites and ornamental rock outcrops.
Downloads
References
Abbiss, C.P. (1981). Shear wave measurements of the elasticity of the ground. Geotechnique, Vol 31, no.1, p.91-104. https://doi.org/10.1680/geot.1981.31.1.91
Beres, M., Luetsher, M. and Olivier, R. (2001). Integration of ground penetrating radar and microgravimetric methods to map shallow caves. Journal of Applied Geophysics 46, 249-262. https://doi.org/10.1016/S0926-9851(01)00042-8
Collins, M. E., Cumb, M. and Hanninenc, P. (1994). Geoderma. Volume 61, Issues 1-2, Pages 1-15.
Conyers, L. B. (2004). Ground-penetrating Radar for Archaeology. Walnut Creek, CA, United States: AltaMira Press Ltd.
Daniels, D. J. (ed.) (2004). Ground Penetrating Radar (2nd Ed.). Knoval (Institution of Engineering and Technology). https://doi.org/10.1049/PBRA015E
Espín de Gea, A. (2009). Analysis of karsts cave structure for the location of a new entrance using 3D images obtained by ground penetrating radar. IWAGPR 2009.
Espín de Gea, A., Reyes, M., Gil, A. y Arévalo, L. (2014). Modelización geológica tridimensional del yacimiento de roca ornamental ubicado en Monte Coto parcelas K, C y D. (Inédito).
Federación Española de la Piedra. (2013). Fondos propios.
Granda, A. y Cambero, J.C. (2012). Introducción al método de la Tomografía Eléctrica. International Geophysical Technology, S.L. (lgt).
Gómez López, R. (2008). Aplicación del radar de penetración en tierra (georadar) a la exploración no destructiva de yacimientos arqueológicos. http://maxwell.ugr.es/ProyectoRaf/final2-babel-spanish.pdf.
IGME (2011). Panorama minero. Piedra natural. Disponible en: www.igme.es/internet/PanoramaMinero/PMLin.htm
Menke, W. (1984). Geophysical Data Analysis: Discrete Inverse Theory. Academic Press, Orlando. USA.
Parasnis. D.S. (1997). Principles of Applied Geophysic. Chapman & Hall.
Sharma, P.V. (2004). Enviromental and engineering geophysics. Cambridge University Press.
Telford,W.M., Geldart,L.P., Sheriff, R.E. (1990). Apllied geophysics. Second Edition. Cambridge University Press. https://doi.org/10.1017/CBO9781139167932
Trabajos Investigación Geológico Minera. Centro Tecnológico del Mármol. Proyectos propios.
Williams, P. W. (2008). The role of the epikarts in karst and cave hydrogeology: a review. International journal of Speleology 37, 1-10. Bologna (Italy). ISSN 0392-6672. https://doi.org/10.5038/1827-806X.37.1.1
Downloads
Published
How to Cite
Issue
Section
License
Copyright (c) 2024 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.