GNGTS 2024 - Atti del 42° Convegno Nazionale

Session 1.2 GNGTS 2024 from multple explosions scatered within the lake perimeter, with non-coincident points of origin (Sotli et al., 2012). Figure 3: Bathymetry map of Martgnano Lake displayed using a nonlinear color scale and contour lines. AB represents an echo-sounder profle line intersectng two craters. References Blaikie T.N. , L. Ailleres, P.G. Bets, R.A.F. Cas, (2014) A geophysical comparison of the diatremes of simple and complex maar volcanoes, Newer Volcanics Province, south-eastern Australia, Journal of Volcanology and Geothermal Research, Volume276, Pages 64-81, ISSN 0377-0273, htps:// doi.org/10.1016/j.jvolgeores.2014.03.001. Caudron, C., A. Mazot, and A. Bernard (2012), Carbon dioxide dynamics in Kelud volcanic lake, J. Geophys. Res., 117, B05102, doi :10.1029/2011JB008806. Cioni, R., Laurenzi, M.A., Sbrana, A., Villa, I.M., 1993. 40Ar/39Ar chronostratgraphy of the inital actvity in the Sabatni volcanic complex (Italy), Boll. Soc. Geol. Ital.,112,251-263.