GNGTS 2016 - Atti del 35° Convegno Nazionale

580 GNGTS 2016 S essione 3.2 surrounding Somma-Vesuvius: application of geophysical surveys for soil thickness mapping. Journal of Applied Geophysics, vol. 59/2 pp. 126-139 - DOI: 10.1016/j.jappgeo.2005.09.001 De Vita P., Napolitano E., Godt J.W., Baum R.L. (2013) - Deterministic estimation of hydrological thresholds for shallow landslide initiation and slope stability models: case study from the Somma-Vesuvius area of southern Italy. Landslides, p. 1-16, ISSN: 1612-5118, online first, DOI: 10.1007/s10346-012-0348-2. Guadagno F.M., Forte R., Revellino P., Fiorillo F., Focareta M. (2005) - Some aspects of the initiation of debris avalanches in the Campania region: the role of morphological slope discontinuities and the development of failure. Geomorphology, 66 (2005), 237-254 Haghshenas, E., Bard, P.Y., Theodoulidis, N., SESAME WP04 Team (2008) - Empirical evaluation of microtremor H/V spectral ratio. Bull. Earthq. ���� �� ������� Eng. 6, 75–108. Ippolito, F., Ortolani, F. andRusso,M. (1973) - Strutturamarginale tirrenica dell’AppenninoCampano: reinterpretazione di dati di antiche ricerche di idrocarburi. ���� ���� ����� ������ ������������ Mem. Sot. Geol. Ital., XII:227-250. Rolandi G., et al. (1993) - “The Avellino plinian eruption of Somma-Vesuvius (3760 yBP): the progressive evolution from magmatic to hydromagmatic style.”Journal of Volcanology and Geothermal Research 58.1: 67-88.