Task 2. Test site Messina Strait WP2.5 G. Neri, Univ. Messina Meccanismi dei terremoti e regimi di stress tettonico nellarea dello Stretto di Messina.

Slides:



Advertisements
Similar presentations
SITE EFFECTS MODELING BY HYBRID TECHNIQUE: THE CASE STUDY OF SOFIA, BULGARIA 27 o CONVEGNO NAZIONALE GRUPPO NAZIONALE di GEOFISICA della TERRA SOLIDA October.
Advertisements

Istituto Nazionale di Geofisica e Vulcanologia Database of Potential Sources for Earthquakes larger than M 5.5 in Italy, and surrounding areas, version.
Time Domain Moment Tensor & Finite Fault Solution for the Aquila Earthquake (2009/04/06 01:32) Elisa Tinti and Laura Scognamiglio Preliminary results,
Earthquake rates in Italy as derived from different approaches
Time Domain Moment Tensor & Finite Fault Solution for the Aquila Earthquake (2009/04/06 01:32) Laura Scognamiglio and Elisa Tinti Preliminary results.
Technical Solutions for NEMO PROJECT R. Papaleo Villa OLMO, October 2001.
INGV-DPC S4 riunione Siena Aprile 2010 ITACA the Italian strong-motion database Task5 – site classification R. Paolucci, S. Giorgetti Politecnico.
SEISMIC SITE EFFECTS IN NORCIA BASIN (CENTRAL ITALY)
WP 4: Real -Time Shake Maps GRSmap a tool for rapid estimation of ground-shaking maps for seismic emergency management in the Campania Region of southern.
INGV ShakeMaps for the lAquila earthquake Alberto Michelini, Licia Faenza & Valentino Lauciani INGV, Centro Nazionale Terremoti.
Progetto S5 – Test sites per il monitoraggio multidisciplinare di dettaglio WP2.4 – Ground deformation pattern of the Calabro-Peloritan area and the Messina.
N THE CRUSTAL STRUCTURE OF SOUTHERN TYRRHENIAN SEA SUBDUCTION ZONE G. Gaudiosi (1),D. Lo Bascio (1),M. Maistrello (2),G.Musacchio (2) and I. Guerra (3)
+ Milena Moretti*, Aladino Govoni*, Alfonso Mandiello*, Lucia Margheriti*, Corrado Castellano*, Fabio Criscuoli*, Paola Baccheschi* and Salvatore Mazza*
+ Aladino Govoni*, Lauro Chiaraluce *, Raffaele Di Stefano*, Lucia Margheriti*, Milena Moretti*, Luisa Valoroso*, Claudio Chiarabba*, Valentino Lauciani*
Velocity and strain rate fields across the fault from integration of regional GPS networks WP 1.3 Velocity and strain rate fields across the fault from.
DPC High-resolution multi-disciplinary monitoring of active fault test-site areas in Italy S5S5S5S5 Roma 24/03/ 2010 S5 Project High-resolution.
WP 4.3 Estimates of earthquakes source parameters and structure characteristics from massive seismic waveform analysis Task 4 L’Aquila seismic sequence:
Department of Earth Science, Geodynamics Group Svalbard earthquake of 21 Feb (M=6.0) K. Atakan, L. Ottemöller, M. Raeesi and J. Havskov.
Strike Slip Right Lateral Fault Plane Auxiliary Plane How are focal mechanisms determined by seismic data? The Great California ShakeOut Focal mechanisms.
Application of SASHA for Mt. Etna case Task D: Probabilistic Hazard Assessment Salvatore D'Amico Istituto Nazionale di Geofisica e Vulcanologia Osservatorio.
EARTHQUAKE FOCAL MECHANISMS (FAULT PLANE SOLUTIONS)
A magnitude 7.1 struck early Saturday off Japan's east coast. The quake hit at 2:10 a.m. Tokyo time about 170 miles from Fukushima, and it was felt in.
用近震波形分析2013 年6 月2 日南投地震的震源過程 謝銘哲1, 趙里2, 馬國鳳1 1國立中央大學地球物理研究所
Lecture #13- Focal Mechanisms
Réunion PARIS 29/06/2006 QSHA WP2 Status report 1 WP2 - Source characterization and Determination of earthquake scenarios WP-2-1: Seismo-tectonic investigation.
Geol 600 Notable Historical Earthquakes Source mechanisms and body wave radiation patterns
UNIVERSITY OF ATHENS Faculty of Geology and Geoenvironment Department of Geophysics and Geothermics A. Agalos (1), P. Papadimitriou (1), K. Makropoulos.
Václav Vavryčuk Institute of Geophysics, Prague Origin of earthquake swarms in West Bohemia inferred from observations of non-doble-couple components in.
Focal Mechanism Solutions
AGU fall meeting, December 5-9, 2011, San Francisco INGV Spatial organization of foreshocks as a tool for forecasting large earthquakes E. Lippiello 1,
Earthquakes Susan Bilek Associate Professor of Geophysics New Mexico Tech How to figure out the who, what, where, why… (or the location, size, type)
RAPID SOURCE PARAMETER DETERMINATION AND EARTHQUAKE SOURCE PROCESS IN INDONESIA REGION Iman Suardi Seismology Course Indonesia Final Presentation of Master.
Application of SASHA for the Icelandic case Vera D’Amico 1, Dario Albarello 2, Ragnar Sigbjörnsson 3, Rajesh Rupakhety 3 1 Istituto Nazionale di Geofisica.
SHARE WP 3 Task 3.3 European crustal strain-rates INGV, NORSAR Salvatore Barba Istituto Nazionale di Geofisica e Vulcanologia, Rome.
Complex earthquake directivity during the 2009 L’ Aquila mainshock Tinti E., Scognamiglio L., Cirella A., Cocco M., and A. Piatanesi Istituto Nazionale.
Differential wave equation and seismic events Sean Ford & Holly Brown Berkeley Seismological Laboratory.
DPC High-resolution multi-disciplinary monitoring of active fault test-site areas in Italy S5S5S5S5 Roma 24/03/ 2010 S5 Project High-resolution.
Data Collection from Early Instrumental Seismological Bulletins for the ISC-GEM Global Instrumental Earthquake Catalogue D. Di Giacomo 1, J. Harris 1,
Present-day tectonic stress determined from focal mechanisms in the seismoactive area Dobrá Voda V. Vavryčuk, L. Fojtíková.
Large Earthquake Rapid Finite Rupture Model Products Thorne Lay (UCSC) USGS/IRIS/NSF International Workshop on the Utilization of Seismographic Networks.
Summary of seismology component of the course Sources Waves Location Magnitude/Intensity Focal mechanisms Other topics.
More Stuff About Earthquakes. Faults Any stress on the plates can cause an earthquake if the elastic limit is reached. Each type of stress results in.
SPICE Research and Training Workshop III, July 22-28, Kinsale, Ireland Seismic wave Propagation and Imaging in Complex media: a European.
Types of Faults and seismic waves
1 Cythera M6.7 earthquake (January 8, 2006) in southern Aegean: uneasy retrieval of the upward rupture propagation J. Zahradnik, J. Jansky, V. Plicka,
The seismogram U = Source * Propagation * Site.
A magnitude 7.6 earthquake struck near the Solomon Islands on Sunday morning local time; there were no immediate reports of damage. The earthquake was.
Chris Andronicos Institute for the Study of the Continents, Cornell University and Aaron A. Velasco, Jose M. Hurtado Department of Geological Sciences.
Surface-wave Derived Focal Mechanisms in Mid-America R. B. Herrmann 1, C. J. Ammon 2 and H. M. Benz 3 1 Saint Louis University, 2 Pennsylvania State University,
HIGH FREQUENCY GROUND MOTION SCALING IN THE YUNNAN REGION W. Winston Chan, Multimax, Inc., Largo, MD W. Winston Chan, Multimax, Inc., Largo, MD Robert.
Earthquake Focal Mechanisms from the New Madrid Seismic Zone Thesis Proposal Brown Bag Greg Johnson.
Václav Vavryčuk, Fateh Bouchaala, Tomáš Fischer Institute of Geophysics, Prague High-resolution fault tomography from accurate locations and focal mechanisms.
Earthquakes. Earthquakes Our Definition: a sudden shaking of the ground because of movement within the earth’s crust.
Brittle failure occurs within “seismogenic zone” defined by fault properties Typically 15 km for vertical strike slip faults ~30-50 km for subduction zone.
MOMENT TENSOR INVERSION OF POSSIBLY MULTIPLE EVENTS AT REGIONAL DISTANCES Petra Adamová 1, Jiří Zahradník 1, George Stavrakakis 2 1 Charles University.
Seismotectonics Mathilde B. Sørensen and J. Havskov.
Types of Faults and seismic waves
SIF 101° Meeting Session - Geophysics
GEOL 308 Quiz: Focal Mechanisms
Uplift: Faults and Earthquakes
Václav Vavryčuk Institute of Geophysics, Prague
Magnitude 7.9 SE of KODIAK, ALASKA Tuesday, January 23, 2018 at 09:31:42 UTC A magnitude 7.9 earthquake occurred at 12:31 am local time 181 miles southeast.
Principal Stress rotates to EW direction
by J. Galetzka, D. Melgar, J. F. Genrich, J. Geng, S. Owen, E. O
Extending the ISC-GEM Global Instrumental Catalogue
Seismology Introduction.
by Satoshi Ide, Annemarie Baltay, and Gregory C. Beroza
by Wenyuan Fan, and Peter M. Shearer
Seismology – Summary.
Mediterranean a Year in Review.
Presentation transcript:

Task 2. Test site Messina Strait WP2.5 G. Neri, Univ. Messina Meccanismi dei terremoti e regimi di stress tettonico nellarea dello Stretto di Messina

Focal mechanisms – CAP method We computed the moment tensor solutions using the Cut And Paste (CAP) method originally proposed by Zhao and Helmerger (1994) and later modified by Zhu and Helmerger (1996). The focal mechanisms and source depth are determined using a grid search technique. Each waveform is broken into Pnl and surface-wave segments. CAP has proven to be effective for analyzing earthquakes even with magnitudes between 2.5 and 4.0 Department of Earth & Atmospheric Sciences Università di Messina

23 eqks (M>=3; focal depths less than 25 km; period ) broadband stations of INGV & MedNet from Barberi et al., 2004

(km) travel time (sec) 1. si definisce un set di eventi e stazioni 2. si calcolano i TT teorici relativi nel modello 3D 3. si costruisce il grafico TT vs 4. dai fits con la teoria delle dromocrone si ricostruisce il modello 1D equivalente valori Vp da tomografia

RESULTS

TESTS from Barberi et al., 2004 from Barberi et al., 2004 for the present dataset from Neri et al., 2009

TESTS

RESULTS

Black and white in the polar plot correspond to P and T axes, respectively.

Black and white in the polar plots correspond to P and T axes, respectively. Normal faulting resulted to be dominant in sector A, more favourably positioned with respect to the southeast-ward retreat of subduction hinge, while strike-slip components become evident in sector B located across the transfer zone between the extensional and compressional domains.

3<=M<3.5 M>=3.5 EARTHQUAKES 97 eqks M>=3.0 Period DATA

STATIONS CAT/SCAN Project funded by National Science Fundation - Lamont Observatory NY - Dipartimento di Fisica Università della Calabria - Istituto Nazionale di Geofisica e Vulcanologia

Eventi in studio con i dati delle stazioni temporanee Messina earthquakes 01/11/ /05/2009 Ml>2.5

Next steps… FM computations with the additional contribution by the INGV experiment data Comparison and integration with other data available (RCMT, TDMT, EMMA, literature, … ) Computations of stress fields