Abstract
A program of geophysical research was carried out as a preliminary stage of study of the Santorini volcanic group. This area is of remarkable geothermal and volcanological interest, and the definition of a volcanological structural model is the starting point for an understanding of the local geodynamic processes.
Gravity, magnetic and geoelectrical data proved that:
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(i)
the core of the volcanic edifice consists of a sedimentary-metamorphic basement;
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(ii)
the basement is tectonically disturbed and a linear tectonic system produces a graben-type structure in the middle part of the area.
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Budetta, G., Condarelli, D., Fytikas, M. et al. Geophysical prospecting on the Santorini Islands. Bull Volcanol 47, 447–466 (1984). https://doi.org/10.1007/BF01961218
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DOI: https://doi.org/10.1007/BF01961218