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USGS NEIC Event Executive Summary
Mw 7.2 Eastern Turkey
October 23, 2011 10:41:21
Version 1
38.63N 43.49E Depth 20km
Location Last Updated at 10/23/2011 07:09:33 (Mountain Time)
Event Coordinator: Benz, Harley M.(benz@usgs.gov)
Nearest Cities
19 km (12 miles) NE (43°) from Van, Turkey 116 km (72 miles) N (351°) from Hakkari, Turkey 130 km (81 miles) SSE (161°) from Karakose (Agri), Turkey 192 km (119 miles) SSW (206°) from YEREVAN, Armenia
Tectonic Summary
Turkey is a tectonically active country that experiences frequent destructive earthquakes. On a broad scale, the seismtectonics of the region near the October 23, 2011 earthquake is controlled by the collision of the Arabian Plate and the Eurasian Plate with northerly convergence of the Arabian plate at a rate of approximately 24 mm/y. West of the October 23, 2011 earthquake the tectonics is dominated by strike-slip faulting on the East and North Anatolian fault zones. These large fault systems extend across much of central and western Turkey accommodating the western motion of the Anatolian block as it is being squeezed by the converging Arabian and Eurasian Plates. In the area of Lake Van and further east, tectonics are dominated by the Bitlis Suture Zone in eastern Turkey and Zagros fold and thrust belt of Iran. The October 23, 2011 earthquake occurred in a broad region of convergence beyond the eastern extent of Anatolian strike-slip tectonics. The focal mechanism of today’s earthquake is consistent with oblique-thrust faulting on a south-southwest trending fault, similar to the trend of mapped faults in the region. This earthquake is a reminder of the many deadly seismic events that Turkey has suffered in the recent past. The devastating Izmit earthquake of 1999 (M = 7.6) broke a section of the North Anatolian Fault 1000 km to the west of the October 23 event and killed 17,000 people, injured 50,000, and left 500,000 homeless. Approximately 70 km from the October 23, 2011 earthquake a M7 earthquake occurred on November 11, 1976 destroying several villages near the Turkey and Iran border and killing several thousand people. A M8.0 earthquake struck Erzincan in 1939, killing an estimated 33,000 people.
Talking Points
• Complex region of faulting dominated by compressional tectonics associated with the Bitlis Suture Zone and Zagros Fold and Thrust belt
• Generally east-west trending thrust fault with waveform controlled depth of 20 km
• Within about 70 km of the November 11, 1976 M7 earthquake that killed 3,900 people
Historical Seismicity
Within approximately 400 km of the epicenter there have been 3 destructive earthquakes since the mid-1970s. These were 1975/09/08 M6.7 MMI(max)VIII Deaths: 2,370 Dist from epi: 241 km 1976/11/24 M7.0 MMI(max)IX Deaths: 3,900 Dist from epi: 66 km 1992/03/13 M6.6 MMI(max)IX Deaths: 498 Dist from epi: 358 km
Style of Faulting: Thrust
Centroid Moment Tensor
11/10/23 10:41:21.73 Epicenter: 38.710 43.446 MW 7.3 USGS CENTROID MOMENT TENSOR 11/10/23 10:41:44.50 Centroid: 39.451 43.354 Depth 16 No. of sta: 159 Moment Tensor; Scale 10**19 Nm Mrr= 5.89 Mtt=-6.13 Mpp= 0.24 Mrt= 7.73 Mrp= 1.60 Mtp=-0.51 Principal axes: T Val= 9.83 Plg=63 Azm=344 N 0.22 4 81 P -10.05 26 173 Best Double Couple:Mo=9.9*10**19 NP1:Strike= 80 Dip=71 Slip= 86 NP2: 272 19 101
W Phase Moment tensor 11/10/23 10:41:21 Epicenter: 38.627 43.534 MW 7.2 USGS/WPHASE CENTROID MOMENT TENSOR 11/10/23 10:41:21.00 Centroid: 38.527 43.790 Depth 11 No. of sta: 89 Moment Tensor; Scale 10**19 Nm Mrr= 5.09 Mtt=-5.75 Mpp= 0.66 Mrt=-4.00 Mrp=-3.80 Mtp=-0.45 Principal axes: T Val= 8.07 Plg=60 Azm=118 N = -0.65 19 248 P = -7.43 20 346 Best Double Couple:Mo=7.8*10**19 NP1:Strike=108 Dip=30 Slip= 133 NP2: 240 69 68
PAGER Population Exposure MMI VI 482K MMI VII 265K MMI VIII 67K MMI IX 377K MMI X 29K
Reported Damage Preliminary reports of collapsed structures in Van, Turkey and widespread outage of power and communication
Links to News Articles http://www.msnbc.msn.com/id/45005013/ns/world_news-europe/ http://www.bbc.co.uk/news/world-europe-15421633 http://www.hurriyetdailynews.com/n.php?n=quake-hits-se-turkey-2011-10-23
USGS Event Link http://earthquake.usgs.gov/earthquakes/eqinthenews/2011/usb0006bqc/
Prompt Assessment of Earthquakes for Response http://earthquake.usgs.gov/earthquakes/pager/events/us/b0006bqc/index.html
If there are any changes, suggestions, questions, or comments about this particular email, please contact benz@usgs.gov
This information is provided by David Phillips at UNAVCO (sent by e-mail):
UNAVCO would be able to provide at least 2 terrestrial LIDAR (TLS) systems with trained operators. Additional UNAVCO or shared (via CWU, UTD, KU, etc.) TLS systems would also be available though trained operators would need to be identified from within UNAVCO or the community. Besides traditional scanning methods, we could explore deployment of 1 or more scanners in a semi-permanent mode to help detect post-seismic displacements through time.
David A. Phillips, Ph.D.
Geodetic Imaging Project Manager
UNAVCO
6350 Nautilus Drive, Boulder, CO 80301
Tel: 303-381-7471, Fax: 303-381-7451
phillips@unavco.org
www.unavco.org <http://www.unavco.org/>
Hi All, I created a ShakeMap for a similar rupture in the CyberShake 1.0 database. CyberShake results are interpolated on top of a Campbell & Bozorgnia 2008 (CB 2008) base map. Log base 10 of 3 second Spectral Acceleration is given. The rupture is from UCER2, a mag 7.45 on the San Cayetano.
CB 2008 base map only: http://opensha.usc.edu/ftp/kmilner/cybershake/2011shakeout/basemap.150.png
CB 2008 + CyberShake: http://opensha.usc.edu/ftp/kmilner/cybershake/2011shakeout/interpolated....
Kevin Milner
TerraSAR-X (TSX) has been acquiring data over the Los Angeles Supersite on two tracks, one ascending and one descending. I attach the map of the available coverage of archive data. Most recent scene was 16 Oct. 2011 on descending track 167, so next pass will be 27 Oct. On ascending track 144 over LA, the most recent scene was 19 March 2011. Obviously, this won't help too much for the Ventura scenario earthquake for InSAR or SAR pixel offset tracking analysis.
From OpenTopography data discovery interface from USGS Click and EarthScope coverage: http://opentopo.sdsc.edu/gridsphere/gridsphere?cid=datasets
Here is a map of the available archived COSMO-SkyMed SAR images. We are fortunate that they have been regularly acquiring data on one track over the area north of Ventura. The most recent acquisition was 16 October 2011 using CSK2 satellite in right-looking mode at about 23-degree incidence angle. ++Eric
Damage proxy map of Los Angeles derived from InSAR coherence of ALOS PALSAR data. The red pixels represent significant surface change during the time period of 2007.02.15 - 2008.02.18. Most of them are due to building demolition or construction projects, which can be confirmed by comparing with Google Earth's historical imagery of similar dates, using the time slider. For example, try to locate Pasadena City College and see how the red pixels correlate with the campus remodeling projcet over the time period.
After the major earthquake hits Los Angeles area at 2011.10.21 06:00:00 PM GMT, this type of damage proxy map that would show major building damage can be made available to responding agencies at the following times, derived from the indicated platforms, considering their orbit plans, data transfer latencies, and processing time.
SAR data are acquired at:
2011.10.22 01:42 AM GMT - TerraSAR-X
2011.10.22 01:58 AM GMT - COSMO-SkyMed (CSM3)
2011.10.22 06:00 PM GMT - UAVSAR
2011.10.24 01:48 AM GMT - Radarsat-2
2011.10.27 06:00 PM GMT - Envisat
Damage proxy map becomes available at:
2011.10.22 05:58 AM GMT - COSMO-SkyMed (data transfer latency: 3 hrs)
2011.10.24 03:48 AM GMT - Radarsat-2 (Data transfer latency: 1 hr)
2011.10.24 06:00 PM GMT - UAVSAR (Overall latency: 3 days)
2011.10.27 02:42 AM GMT - TerraSAR-X (Data transfer latency: 5 days)
2011.10.29 07:00 PM GMT - Envisat (Orbit data latency: 2 days)
Two pre-quake scenes are assumed to be available.
Provided by ARIA project at JPL/Caltech
Contact aria@jpl.nasa.gov or aria@caltech.edu for more information.
maybe it is just my ears, but it is a little hard to hear, maybe just people in the room there?
Here is a broader extent
Image of the topography (lidar hillshade) and USGS fault traces; of course assuming that it occurs along this system (where we think it should?)