Information message about destructive earthquake in Pakistan on September 24, 2013

     The destructive earthquake with M=7.7 has occurred on September 24, 2013 at 11:29 GMT (15:29 Moscow time) in Pakistan, it caused victims and damage.
     Parameters of the earthquake have been determined in the Alert Service (AS) of Information Processing Center (IPC) of Geophysical Survey of RAS in Obninsk with station data obtained from digital and analog seismic stations of Russia, countries of CIS and from abroad. Alert message on this earthquake has been delivered in 11 min after registration to the Ministry of Emergency of the Russian Federation (EMERCOM).
     Preliminary processing has been done with data from 38 stations, accurate processing - with data 80 stations.
     Fig. 1 presents fragments of records obtained from digital stations Ala-Archa (∆ 17.2º), Garni (∆ 21.6º), Nalchik (∆ 24.2º), Kislovodsk (∆ 25º), Kurchatov (∆ 25.7º). Fig. 2 presents fragments of records obtained from digital stations Borovoe (∆ 26.2º), Arti (∆ 29.8º), Obninsk (∆ 35.1º), Talaya (∆ 37.8º), Lovozero (∆ 44.9º).

Figure 1
 

Figure 2
 
     IPC GS RAS also has obtained information with parameters of this event from some seismological centers, these data are given in table 1:
Table 1
NN Time in origin h-min-s (GMT) Lat degr. Lon degr. Depth km N s/st Ms/ N mb/ N I0 calc GAP Center
1 11-29-47.9 27.03 65.52  20  80  7.7/456.9/399.5-10 82 IPC GS RAS (Accurate)
2 11-29-50.3 27.41 65.57  10  38   6.7/289.5-10 82 IPC GS RAS (Preliminary)
3 11-29-49.4 27.07 65.561  20  467  Mw 7.7   23 CSEM
4 11-29-48.9 27 65.514  20  216  Mw 7.7   22 NEIC
  • IPC GS RAS - Informational Processing Center, Geophysical Survey, Russian Academy of Sciences
  • CSEM - European - Mediterranean seismological center
  • NEIC - National Earthquakes Information Center of US Geological Service
  • Epicenter
         Fig. 3 presnts epicenter of this earthquake with red star, it's origin was located on the territory of Pakistan, at the depth of 20 km, 278 km N-N-E of Karachi, Pakistan, 340 km N-E of Hyderabad, Pakistan and 533 km S-E of Zahedan, Iran.

    Figure 3
    Aftershock
         GS RAS registered 11 aftershocks with М>=4.7 within 11 hours after the main shock.
    N Date   &   Time (GMT)
    yy-mm-dd hh:mm:sec
    Lat
    degr.
    Lon
    degr.
    Depth
    km
    N
    station
    Ms/ N mb/ N Io
    calc.
    Region
    201333632013-09-24 11:36:29.027.365.662039-6.0/ 246.5-7 Pakistan
    201333642013-09-24 12:07:04.027.2365.651021-4.9/ 145-5.5 Pakistan
    201333652013-09-24 12:42:11.027.3265.62039-5.2/ 284.5-5 Pakistan
    201333662013-09-24 13:01:39.027.4465.722055-5.8/ 426-6.5 Pakistan
    201333672013-09-24 14:08:33.027.6565.762050-5.4/ 285-5.5 Pakistan
    201333682013-09-24 15:12:22.027.1365.72031-5.0/ 174-4.5 Pakistan
    201333702013-09-24 17:20:13.027.265.582046-5.6/ 325.5-6 Pakistan
    201333712013-09-24 19:54:06.027.565.712027-4.7/ 163.5-4 Pakistan
    201333722013-09-24 21:59:02.027.5765.832036-5.0/ 254-4.5 Pakistan
    201333732013-09-24 22:38:16.027.2665.492023-4.8/ 173.5-4 Pakistan
    Macroseismic manifestations
         According to RIA-Novosti as a result of this earthquake 348 persons were killed. Nearly 20 thousand houses were destroyed or seriously damaged. Almost 90% of buildings were damaged in Avaran town. Chief minister of Balochistan Province Mr. Abdul Ballodge announced emergency situation in the region. Military personnel and border guards were sent to support the rescue teams. The shocks were felt in Hyderabad, Larkana and other settlements. Indian media reported about weak shocks which were felt in New-Delhi and other parts of northern India. Fig. 4 obtained from USGS NEIC presents the USGS Community Internet Intensity Map made by 50 responses in 20 cities.

    Figure 4
    Historical records
         This earthquake has occurred 361 km E-S-E of strong earthquake on April 16, 2013 with mb=7.8 (yellow star on fig. 5).

    Figure 5
    Focal mechanism and seismic moment of the earthquake
         Focal mechanism of this earthquake was calculated in IPC GS RAS on the P-wave first-motions at 125 stations, 79 stations registered compression waves (plus signs) and 46 stations registered expansion waves (minus signs) at distances 8–95º and dispersed rather evenly along the azimuths. The fig.6 shows a focal mechanism solution in stereographic projection at the lower hemisphere, elements of focal mechanism are presented in table.2. Fig. 7, 8 show focal mechanism derived with W-phase from the estimated moment tensor in USGS NEIC and focal mechanism derived from the estimated CMT in Quick CMT Catalog, USA. Both solutions are close. This earthquake has occurred under the action of close in value compression stresses oriented to the south and expansion stresses oriented to the east. One nodal planeь NP2 in all solutions is almost vertical (DP=86-89º) and it is oriented north-west (STK=309-322º) – south-east (STK=134º), another nodal plane NP1 is more flat (DP=46-47º) and oriented south-west. The type of motion along NP2 is right hand slips with fault components (IPC GS RAS and СМТ solutions) and reverse fault (USGS NEIC solution). For NP1 – left hand slips (with fault components for IPC GS RAS, reverse fault components for USGS NEIC) and «pure» slip for CMT. Averaged value of seismic moment was obtained in IPC GS RAS with Р wave spectra registered at two stations: «Obninsk» (∆35.07º) and «Talaya» (∆37.77º) Мо=1.0*10**20 N*m, Mw=7.3. According to USGS NEIC – Мо=1.42*10**20 N*m, Mw=7.7; according to Quick CMT – Мо=4.81*10**20 N*m, Mw=7.7.
    Table 2
    Axes of main strengths Nodal planes Center
    T P N NP1 NP2
    Pl Azm Pl Azm Pl Azm Stk Dp Slip Stk Dp Slip
    268732194 4732622848-5322 86-137IPC GS RAS
    338145309 45309228466134 86136NEIC
    277530183 4731221847-2310 86-137Quick CMT
  • IPC GS RAS - Informational Processing Center, Geophysical Survey, Russian Academy of Sciences
  • NEIC - National Earthquakes Information Center of US Geological Service
  • Quick CMT - Quick CMT catalog

  • Figure 6

    Figure 7

    Figure 8


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