GNGTS 2014 - Atti del 33° Convegno Nazionale

GNGTS 2014 S essione 1.1 25 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 Azzaro R.; 1999: Earthquake surface faulting at Mount Etna volcano (Sicily) and implications for active tectonics. Journal of Geodynamics, 28 , 193-213. Azzaro R.; 2004: Seismicity and active tectonics in the Etna region: constraints for a seismotectonic model. ���In: BonaccorsoA., Calvari S., Coltelli M., Del Negro C., Falsaperla S., (Eds.), Mt. Etna: volcano laboratory. �������� American Geophysical Union, Geophysical monograph, 143 , pp. 205-220, doi: 10.1029/1436M13. Azzaro R., Barbano M.S., D’Amico S., Tuvè T., Albarello D. and V. D’Amico; 2008: First studies of probabilistic seismic hazard assessment in the volcanic region of Mt. Etna (Southern Italy) by means of macroseismic intensities. Bollettino di Geofisica Teorica e Applicata, 49 (1) , 77-91. Azzaro R., D’Amico S. and T. Tuvè; 2011: Estimating the magnitude of historical earthquakes from macroseismic intensity data: new relationships for the volcanic region of Mount Etna (Italy). Seismological Research Letters, 82 , 4, 533-544. Azzaro R., Branca S., Gwinner K. and M. Coltelli; 2012a: The volcano-tectonic map of Etna volcano, 1:100.000 scale: an integrated approach based on a morphotectonic analysis from high-resolution DEM constrained by geologic, active faulting and seismotectonic data. Italian Journal of Geosciences, 131 (1) , 153-170. Azzaro R., D’Amico S., Peruzza L. and T. Tuvè; 2012b: Earthquakes and faults at Mt. Etna (Southern Italy): problems and perspectives for a time-dependent probabilistic seismic hazard assessment in a volcanic region. Bollettino Geofisica Teorica e Applicata, 53 (1) , 75-88. Azzaro R., BonforteA., Branca S. and F. Guglielmino; 2013a: Geometry and kinematics of the fault systems controlling the unstable flank of Etna volcano (Sicily). Journal of Volcanology and Geothermal Researches, 251 , 5-15. Azzaro R., D’Amico S., Peruzza L. and T. Tuvè; 2013b: Probabilistic seismic hazard at Mt. Etna (Italy): the contribution of local fault activity in mid-term assessment. Journal of Volcanology and Geothermal Research, 251 , 158-169. CMTE Working Group; 2014: Catalogo Macrosismico dei Terremoti Etnei dal 1832 al 2013. ����� �������� INGV, Catania, http:// www.ct.ingv.it/macro/etna/html_index.php. Cinti F. R., D. Pantosti, P.M. De Martini, S Pucci, R. Civico, S. Pierdominici, L. Cucci, C.A. Brunori, S. Pinzi and A. Patera.; 2011: Evidence for surface faulting events along the Paganica fault prior to the 6 April 2009 L’Aquila earthquake (central Italy). J. Geoph. Res., 116 , B07308, doi:10.1029/2010JB007988. Field E.H., D.D. Johnson and J.F. Dolan; 1999: A mutually consistent seismic-hazard source model for Southern California. Bulletin of the Seismological Society of America, 89 , 559-578. Galli P., B. Giaccio and P. Messina; 2010: The 2009 central Italy earthquake seen through 0.5 Myr- long tectonic history of the L’Aquila faults system. Quaternary Science Reviews, 29 , 3768–3789. Moro M., S. Gori, E. Falcucci, M. Saroli, F. Galadini and S. Salvi; 2013: Historical earthquakes and variable kinematic behaviour of the 2009 L’Aquila seismic event (central Italy), causative fault, revealed by paleoseismological investigations. Tectonophysics, 583 , 131-144. Pace B., F. Visini and L. Peruzza; 2013: D5.1 Numerical simulation of earthquake recurrence time for selected fault. DPC-INGV Project S2-2102 “Constraining Observations into Seismic Hazard”, https://sites.google.com/site/ ingvdpc2012progettos2/deliverables/d5_1, v. 0.15 released online on 30 Aug 2013. Peruzza L. and B. Pace; 2002: Sensitivity analysis for seismic source characteristics to probabilistic seismica hazard assessment in Central Apennines (Abruzzo area). Bollettino di Geofisica Teorica ed Applicata, 43 , 79-100. Peruzza L., B. Pace, and F. Cavallini; 2010: Error propagation in time-dependent probability of occurrence for characteristic earthquakes in Italy. Journal of Seismology, 14 ,119-141, DOI 10.1007/s10950-008-9131-1, online eds 1573-157X, 2008 Peruzza L., B. Pace, and F. Visini; 2011: Fault-based earthquake rupture forecast in Central Italy: remarks after the L’Aquila M w 6.3 event . �������� �� ��� ������������� ������� �� �������� Bulletin of the Seismological Society of America, 101 , 404-412. Stirling M., T. Godet, K. Berryman and N. Litchfield; 2013: Selection of earthquake scaling relationships for seismic- hazard analysis. Bulletin of the Seismological Society of America, 103 (6) , 2993-3011. Villamor P., Berryman R.K.R., Webb T., Stirling M., McGinty P., Downes G., Harris J. and N. Litchfield; 2001: Waikato Seismic Loads: revision of Seismic Source Characterisation. GNS Client Report 2001/59. Wells D.L. and K.J. Coppersmith; 1994: New empirical relationships among magnitude, rupture lenght, rupture area, and surface displacement. Bulletin of the Seismological Society of America, 84 (4) , 974-1002. Wesnousky S.G.; 2008: Displacement and geometrical characteristics of earthquake surface ruptures: issues and implications for seismic-hazard analysis and the process of earthquake rupture. Bulletin of the Seismological Society of America, 98 (4) , 1609-1632�.

RkJQdWJsaXNoZXIy MjQ4NzI=