Information message about the devastating earthquake in Central Italy, October 30, 2016

     The devastating earthquake M=6.7 has occurred on October 30, 2016 at 06:40 GMT (09:40 Moscow time) in Central Italy.
     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 34 stations, accurate processing - with data 80 stations.
     Fig. 1 presents fragments of records obtained from digital stations Apeiranthos of Naxos (∆ 11.1º), Malin Array (∆ 13.6º), Isparta (∆ 14.2º), Keshkin SH Array (∆ 15.7º), Kongsberg (∆ 17º). Fig. 2 presents fragments of records obtained from digital stations Vasula (∆ 17.8º), Sochi (∆ 19.4º), Obninsk (∆ 19.6º), Kislovodsk (∆ 21.5º), Khabaz (∆ 21.7º).

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 06-40-17.2 42.8 13.12  10  80  6.7/436.6/369.5 76 IPC GS RAS (Accurate)
2 06-40-24.4 42.89 13.41  33  34   6.3/106.5 -7 IPC GS RAS (Preliminary)
3 06-40-18.3 42.84 13.11  10  168  Mw 6.5   27 CSEM
4 06-40-19.2 42.86 13.09  10  124  Mw 6.6   28 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 presents with red star the epicenter of this earthquake, its origin was located in the central part of Italy at the depth of 10 km, 54 km N-N-W of L'Aquila, 70 km E-S-E of Perugia and 113 km N-E of Rome.

    Figure 3
    Aftershock
         GS RAS registered 9 aftershocks М>=4.4 within one day 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
    201638522016-10-30 07:13:05.042.7113.291021-4.6/ 124.5 Central Italy
    201638532016-10-30 07:34:47.042.9212.971010-4.4/ 74 Central Italy
    201638542016-10-30 08:35:59.042.8213.141022-4.8/ 124.5-5 Central Italy
    201638582016-10-30 12:07:01.042.8513.11027-5.0/ 165-5.5 Central Italy
    201638592016-10-30 13:34:54.042.9312.91023-4.7/ 124.5-5 Central Italy
    201638602016-10-30 14:03:19.043.0713.381016-4.5/ 104-4.5 Central Italy
    201638632016-10-30 18:21:10.042.9313.071022-4.5/ 114-4.5 Central Italy
    201638672016-10-31 03:27:39.042.8512.891023-4.6/ 134.5 Central Italy
    201638702016-10-31 07:05:43.042.7513.21022-4.6/ 124.5 Central Italy
    Macroseismic manifestations
         According to ITAR-TASS, several dozen people were injured in the earthquake. The number of homeless may reach 100 thousand. More than 40 settlements partially or completely were destroyed in the province of Macerata after the earthquake. Among the largest cities affected by the earthquake, Norcia (reg. Umbria), it hit a few, including ancient churches, among them the church of St. Benedict with a nunnery (Fig. 4). Undeground shocks were felt across the Italy. Fig. 5 was obtained from USGS NEIC , it presents USGS Community Internet Intensity Map based on 1062 responses in 351 cities.

    Figure 4

    Figure 5
    Historical records
         The epicenter was located 14 km S-S-W of the devastating earthquake's epicenter of October 26, 2016 М=6.2 and 13 km W-N-W of devastating earthquake's epicenter of August 24, 2016 М=6.2, which killed 297 persons.
    Focal mechanism and seismic moment of the earthquake
         Focal mechanism solution of the origin was obtained in IPC GS RAS with signs of initial arrivals of P waves at 71 stations, including 17 stations which registered compression waves (plus signs) and 54 stations which registered tensile waves (minus signs). These stations are located in the interval of epicentral distances of 2.4–99.6º and azimuthal sector Az=3-352º. Focal mechanism solution in stereographical projection at the lower hemisphere is shown at fig. 6, it's elements are given in table 2. Fig. 7, 8 present focal mechanism solutions obtained in USGS NEIC with W-phase Moment Tensor (Mww) technique and in Lamont-Doherty Earth Observatory Global CMT Columbia University, USA (LDEO GCMT) with СМТ (Centroid moment tensor) technique. All solutions are close. The earthquake has occurred under the action of tensile stresses oriented to the north–east. NP1 plane according to GS RAS has a circum-meridian direction of propagation, according to NEIC and GCMT - it strikes south-east, NP2 plane in all solutions strikes north-west. NP1 plane is more flat, the angle of dipping to the horizon DP=27-39º, NP2 palne is dipping to the horizon under the angle DP=53-63º. The type of motion along both planes – fault (according to GS RAS - with insignificant latteral component). Seismic moment of this earthquake was obtained in IPC GS RAS with spectra of P waves registered at "Arti" station (∆ 31.81º), it makes Mo=1.2*10**19 N*m, Mw=6.7. According to USGS NEIC – Mo=1.071*10**19 N*m, Mw=6.6; according to LDEO GCMT – Mo=1.03*10**19 N*m, Mw=6.6
    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
    127463187 2433819139-50324 61-118IPC GS RAS
    186772238 333616227-84335 63-93NEIC
    86879293 815914938-102345 53-81GCMT
  • IPC GS RAS - Informational Processing Center, Geophysical Survey, Russian Academy of Sciences
  • NEIC - National Earthquakes Information Center of US Geological Service
  • GCMT - Lamont-Doherty Earth Observatory Global CMT Columbia University, USA

  • Figure 6

    Figure 7

    Figure 8


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