Department of Earth Science, Geodynamics Group www.geo.uib.no Svalbard earthquake of 21 Feb. 2008 (M=6.0) K. Atakan, L. Ottemöller, M. Raeesi and J. Havskov.

Slides:



Advertisements
Similar presentations
Time Domain Moment Tensor & Finite Fault Solution for the Aquila Earthquake (2009/04/06 01:32) Laura Scognamiglio and Elisa Tinti Preliminary results.
Advertisements

Fast determination of earthquake source parameters from strong motion records: Mw, focal mechanism, slip distribution B. Delouis, J. Charlety, and M. Vallée.
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.
Cascadia Ken Creager, Steve Malone, Geoff Abers, Stephane Rondenay, Brad Hacker and Tim Melbourne Earth and Space Sciences University of Washington.
Helge Drange Geophysical Institute University of Bergen Helge Drange Observed and projected climate change.
HD 44283: Delta Scuti star with regular frequency distribution? Zsófia Bognár Konkoly Observatory COROT Day, 2007 March 12.
 Depth Into the earth Surface of the earth Distance along the fault plane 100 km (60 miles) Slip on an earthquake fault START.
Sendai Earthquake NE Japan March 11, 2011 Some explanatory slides Bob Stern, Dave Scholl, others updated March
DISCRIMINATING SMALL EARTHQUAKES FROM QUARRY BLASTS USING PEAK AMPLITUDE RATIO - Vmax/Hmax MA, S., EATON, D., & DINEVA, S. Department of Earth Sciences.
Magnitude 8.9 (9.0) earthquake near Sendai, east coast of Honshu, Japan Friday, March 11, 2011 at 05:46:23 UTC Japan was struck by a magnitude 8.9 (9.0)
Stress, Strain, Elasticity and Faulting Lecture 11/23/2009 GE694 Earth Systems Seminar.
EARTHQUAKES AND TSUNAMI IN HAWAI‘I (GG103) ~50 years of Hawai‘i seismicity.
Lecture #13- Focal Mechanisms
Stress III The domino effect Stress transfer and the Coulomb Failure Function Aftershocks Dynamic triggering Volcano-seismic coupling.
Application to Wells Nevada Earthquake
Tsunami Great Sumatra Earthquake Tsunami Death Toll ~ 250,000 Tsunami Death Toll ~ 250,000.
Václav Vavryčuk Institute of Geophysics, Prague Origin of earthquake swarms in West Bohemia inferred from observations of non-doble-couple components in.
Earthquake potential of the San Andreas and North Anatolian Fault Zones: A comparative look M. B. Sørensen Department of Earth Science, University of Bergen,
Earthquake Focal Mechanisms
Earthquakes Susan Bilek Associate Professor of Geophysics New Mexico Tech How to figure out the who, what, where, why… (or the location, size, type)
8.2 Measuring Earthquakes
Seismic Reflection Image along I-64 Pratt et al., 1988 Coruh et al., 1988.
M. Herak, S. Markušić, D. Herak Department of Geophysics, Faculty of Science University of Zagreb, Zagreb.
LECTURE 4: EARTHQUAKE FOCAL MECHANISMS
Exploring Planet Earth Blind Thrust Fault Earthquake Rupture Animation (Northridge, 1994) Brad Aagaard, USGS
Mercalli Scale Crust Mantle Plate Tectonics P-wave S-wave focus epicenter seismograph Richter Scale Tsunami fault.
03/000 Phil R. Cummins March 2005 The Indian Ocean Tsunamis – Science and Seismics Australian Government Geoscience Australia.
1 Cythera M6.7 earthquake (January 8, 2006) in southern Aegean: uneasy retrieval of the upward rupture propagation J. Zahradnik, J. Jansky, V. Plicka,
DISCRIMINATING SMALL EARTHQUAKES FROM QUARRY BLASTS USING PEAK AMPLITUDE RATIO Vmax/Hmax MA, S., EATON, D., & DINEVA, S. Department of Earth Sciences The.
Zadonina E.O. (1), Caldeira B. (1,2), Bezzeghoud M. (1,2), Borges J.F. (1,2) (1) Centro de Geofísica de Évora (2) Departamento de Física, Universidade.
Present-day tectonic stress determined from focal mechanisms in the seismoactive area Dobrá Voda V. Vavryčuk, L. Fojtíková.
Disputable non-DC components of several strong earthquakes Petra Adamová Jan Šílený.
The January 2010 Efpalio earthquake sequence in Western Corinth Gulf: epicenter relocations, focal mechanisms, slip models The January 2010 Efpalio earthquake.
DISCRIMINATING SMALL EARTHQUAKES FROM QUARRY BLASTS USING PEAK AMPLITUDE RATIO Vmax/Hmax MA, S., EATON, D., & DINEVA, S. Department of Earth Sciences The.
Geology 15 Mid Term II Review. Focal mechanisms are diagrams made from first motion seismologic records that show the possible motion on a fault, and.
1 Cythera M6.7 earthquake (January 8, 2006) in southern Aegean: uneasy retrieval of the upward rupture propagation J. Zahradnik, J. Jansky, V. Plicka,
NORWAY Coordinating Institute (partner signing the CA): University of Bergen (UiB), Bergen, Norway National team: Following are the 4 core members of the.
1994 Bolivian Earthquake Eric Kiser Bolivian Earthquake Moment Magnitude (Mw): 8.3 Epicenter: 13.84°S and °W Depth: 631km.
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.
GROUND MOTION SIMULATIONS AT RAPID RESPONSE SITES IN ISTANBUL, TURKEY Mathilde Bøttger Sørensen 1, Nelson Pulido 2, Anibal Ojeda 3, Kuvvet Atakan 1, Mustafa.
Near Fault Ground Motions and Fault Rupture Directivity Pulse Norm Abrahamson Pacific Gas & Electric Company.
Aftershock statistics 266 aftershocks of M>2.5 were recorded during the first two months after the main shock Daily distribution does not decay exponentially.
California Earthquake Rupture Model Satisfying Accepted Scaling Laws (SCEC 2010, 1-129) David Jackson, Yan Kagan and Qi Wang Department of Earth and Space.
EART 118 Seismotectonics MWF D250 9:30-10:40 am; Th D250 2:00-4:00 pm Prof.: Thorne Lay, C382 E&MS, Office Hours 11:00-12:00 MWF TA: Lingling Ye, Office.
By NTU Palert, CWB & NCDR teams. Wu and Chiao (2006)
Brittle failure occurs within “seismogenic zone” defined by fault properties Typically 15 km for vertical strike slip faults ~30-50 km for subduction zone.
Shaking and Flooding by the Tohoku-Oki earthquake Shengji Wei*, Rob Graves**, Don Helmberger*, Jean-Philippe Avouac* and Junle Jiang* * Seismological Lab,
Seismograph Mercally Scale Richter ScaleSan Andres Fault Focus Epicenter Aftershock Pictures of disasters(earthquakes) credits.
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.
Future Directions and Capabilities of Simulators Jim Dieterich
GEOL 308 Quiz: Focal Mechanisms
The Charlevoix Seismic Zone
10th Inkaba yeAfrica/!Khure Africa (AEON) Conference/Workshop
Understanding Earth Chapter 13: EARTHQUAKES Grotzinger • Jordan
12. Faulting and Earthquake Focal Mechanisms William Wilcock
دانشگاه شهیدرجایی تهران
تعهدات مشتری در کنوانسیون بیع بین المللی
SICHUAN EARTHQUAKE May 12, 2008
Earthquakes.
University of California, Davis
Slip pulse and resonance of Kathmandu basin during the 2015 Mw 7
by J. Galetzka, D. Melgar, J. F. Genrich, J. Geng, S. Owen, E. O
by Satoshi Ide, Annemarie Baltay, and Gregory C. Beroza
by Wenyuan Fan, and Peter M. Shearer
Susan Bilek University of Michigan
Fig. 1 Map of the trifurcation area of the SJFZ.
Mediterranean a Year in Review.
Earthquakes Forces Inside Earth
Presentation transcript:

Department of Earth Science, Geodynamics Group Svalbard earthquake of 21 Feb (M=6.0) K. Atakan, L. Ottemöller, M. Raeesi and J. Havskov

Department of Earth Science, Geodynamics Group Jordskjelvet på Svalbard 21 februar 2008 (M=6.0)

Department of Earth Science, Geodynamics Group Svalbard earthquake (21.feb.2008) recorded at Tromsø station

Department of Earth Science, Geodynamics Group Svalbard earthquake (21.feb. 2008) record at Kings Bay (Spitsbergen).

Department of Earth Science, Geodynamics Group Svalbard earthquake (21.feb. 2008) record at Bjørnøya station.

Department of Earth Science, Geodynamics Group Svalbard earthquake (21.feb. 2008) record at Kongsberg station.

Department of Earth Science, Geodynamics Group

Department of Earth Science, Geodynamics Group The earthquake occurred likely between the Billedfjord and Lomfjorden faults. More than 2000 aftershocks are recorded.

Department of Earth Science, Geodynamics Group More than 200 aftershocks are located.

Department of Earth Science, Geodynamics Group MT-inversion on regional stations (depth fixed to 15 km)

Department of Earth Science, Geodynamics Group MT-inversion on local stations

Department of Earth Science, Geodynamics Group Focal mechanism based on the first motion polarities (left) and based on the slip inversion (right)

Department of Earth Science, Geodynamics Group

Department of Earth Science, Geodynamics Group (Ingolfsson, 2007)

Department of Earth Science, Geodynamics Group (Ingolfsson, 2007) The focal mechanism is compatible with E-W oriented maximum horizontal compression. Fault rupture area is roughly 9 x 11 km.

Department of Earth Science, Geodynamics Group (Breivik et al., 2005)

Department of Earth Science, Geodynamics Group (Breivik et al., 2005)

Department of Earth Science, Geodynamics Group (Breivik et al., 2005)

Department of Earth Science, Geodynamics Group Norsk Nasjonalt Seismisk Nettverk (NNSN) Institutt for geovitenskap, Universitetet i Bergen

Department of Earth Science, Geodynamics Group Thank you for your attention!