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A Geophysical Study of the Carcavai Fault Zone, Portugal

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Abstract

The Algarve province is located a few hundred kilometres north of the crossing of the E–W Eurasia–Africa plate boundary in an area of diffuse seismicity and broad deformation. It is characterised by a moderate seismicity, with some important historical and instrumental earthquakes causing loss of lives and significant material damages. The area is affected not only by plate boundary earthquakes but also by moderate to large events generated by local sources. The assessment of onshore local sources is, therefore, of vital importance for an evaluation of the regional seismic hazard. This paper discusses the application of geophysical data to the study of the Carcavai fault zone, an outcropping structure more than 20 km long which is seen to deform sediments of the Plio-Quaternary age. The location of some sectors of the fault zone, as well as the vertical offsets of the structure, are still to be confirmed. In order to estimate these and to study the geometry of the fault zone at depth, geophysical data were acquired together with new geological data. Where the location of the fault was less certain, EM and seismic reflection profiles with coarse spatial sampling were carried out. After the detailed location of the fault zone, seismic reflection profiles with a more dense spatial resolution were acquired. The integrated interpretation of the geological and geophysical data confirmed the presence of a large fault zone. The total fault length is still unknown as its extension offshore is still being studied. Together with estimated values of the throw obtained, this data set has improved understanding the seismic hazard in the area by providing more refined estimates of co-seismic rupture, maximum expected earthquake and return periods.

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Acknowledgments

The authors are particularly grateful to the ANPC (National Authority for Civil Protection Agency) for financing the ERSTA (Study of the Tsunami and Seismic Risk of the Algarve) project. Fernando Santos, from the University of Lisbon is also acknowledged for providing the software for the inversion of the EM data and helpful comments on its application. Our thanks to F. Carrilho and the Instituto de Meteorologia for allowing publication of epicentre location data. The authors would also like to thank G. Manuppella, J. Cabral and P. Terrinha for discussions on the location of the seismic reflection profiles and to L. Martins, the former head of the INETI Geophysics Division for support to this project. We are also indebted to the field crew: J. Leote, F. Caneiras, J. Marquilhas and J. Gomes. The contributions of two anonymous reviewers are also acknowledged.

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Carvalho, J., Ramalho, E., Dias, R. et al. A Geophysical Study of the Carcavai Fault Zone, Portugal. Pure Appl. Geophys. 169, 183–200 (2012). https://doi.org/10.1007/s00024-011-0318-y

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