GNGTS 2014 - Atti del 33° Convegno Nazionale

36 GNGTS 2014 S essione 1.1 confirming field observations that creep at Etna is a common mechanism of faulting (Rasà et al. , 1996). This implies that quantifying the deficit of seismic moment-rate with respect the geodetic one in terms of spatial distribution and temporal variations is an important task to characterize t��he potential for seismic slip of contiguous fault segments. �� ����� ����� ��� �� ������ �� � ����� In fact, creep may be viewed as a proxy of loading processes on locked fault segments leading to seismic failure during subsequent earthquakes. Acknowledgments. ���� ����� ��� ��������� ���� ������� �������� �� ��� ������� ���������� ��� ��������� ��� This study has benefited from funding provided by the Italian Presidenza del Consiglio dei Ministri - Dipartimento della Protezione Civile (DPC), in the frame of the 2014-2015Agreement with Istituto Nazionale di Geofisica e Vulcanologia - INGV, project V3: “Multi-disciplinary analysis of the relationships between tectonic structures and volcanic activity ‘’. This paper does not necessarily represent DPC official opinion and policies. References Alparone S., Barberi G., Cocina O., Giampiccolo E., Musumeci C. and Patanè D.; 2012: Intrusive mechanism of the 2008–2009 Mt. Etna eruption: constraints by tomographic images and stress tensor analysis . Journal of Volcanology and Geothermal Research, 229-230 , 50-63, doi: 10.1016/j.jvolgeores.2012.04.001. 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