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The magnetotelluric (MT) method in the period range 0.075-42 s was applied to determine the electrical structure (<8 km) of the Kos Island geothermal region and delineate the tectonic features at this part of the Hellenic Volcanic Arc (HVA). Nineteen MT soundings were conducted on the western half of the island and the collected MT data were found to be two-dimensional (2-D). The NNW-SSE (30°W)...
The magnetotelluric (MT) method in the period range 0.075-42 s was applied to determine the electrical structure (<8 km) of the Kos Island geothermal region and delineate the tectonic features at this part of the Hellenic Volcanic Arc (HVA). Nineteen MT soundings were conducted on the western half of the island and the collected MT data were found to be two-dimensional (2-D). The NNW-SSE (30 ...
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