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Analysis of a radial geodetic monitoring record indicated small-scale inflation of the NW part of the Thera (Santorini) caldera (up to 10cm baseline length increase) between 1994 and 2000, corresponding to up to 2*10 −5 strain, and subsequent stabilization especially after 2006, as GPS data indicate. The southern part of the caldera on the contrary remained practically stable. This partial...
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