Helium and CO2 soil gas emission from Santorini (Greece) |
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Authors: | Franco Barberi Maria Luisa Carapezza |
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Institution: | (1) Dipartimento di Scienze della Terra, University of Pisa, via S. Maria 53, 56100 Pisa, Italy;(2) Istituto di Mineralogia, Petrografia e Geochimica, University of Palermo, via Torino 27D, 90100 Palermo, Italy;(3) Istituto per la Geochimica dei Fluidi, CNR, via Torino 27D, 90100 Palermo, Italy |
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Abstract: | Soil gas investigation is a useful tool to detect active faults. The sudden appearance of soil gas anomalies in zones of deep-reaching faults represents a promising potential precursor of earthquakes and volcanic eruptions. In volcanic areas the development of soil gas monitoring techniques is particularly important, as they can represent, together with remote sensing techniques, the only geochemical methods that can be safely applied during volcanic unrest, when it becomes impossible or too dangerous to sample crater fumaroles. A soil gas survey was carried out in June 1993 at the main island of Thera, in the Santorini volcanic complex. CO2 flux and CO2 and helium concentrations were measured at 50 cm depth for 76 points covering the entire island, with a spacing of 500 m or less. Several anomalous soil degassing sites have been detected. The main anomalies correspond to the Kolumbos line and to the Kameni line, two volcano-tectonic fault systems that controlled all the historic volcanic activity of Santorini. A third anomaly is related to a gas-leaking fault cutting the geothermal field of southern Thera. Soil gas data, together with geovolcanological and seismological evidence, indicate that the Kolumbos and Kameni lines are the most probable sites for future volcanic or seismic reactivation, and provide the basis for the establishment of a new geochemical monitoring technique at Thera. |
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Keywords: | Santorini volcano Greece soil gas helium and carbon dioxide geochemical monitoring active faults |
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