The red marker on the map is the epicenter of the earthquake, which occurred on the border of Balkh and Samangan provinces, Afghanistan, at a depth of 10 km, 43 km SE of Mazar-i-Sharif, 58 km W-NW of Aibak and 265 km NW of Kabul, the capital of Afghanistan.
|
Time in origin (GMT) |
Latitude, degree |
Longitude, degree |
Depth, km |
Stations number |
Ms/N |
mb/N |
I0 (calculated) |
GAP |
Center |
| 1
|
20:28:59.0
|
36.48 |
67.47 |
10.0 |
44
|
6.4/35 |
6.5/36 |
9-9.5 |
173
|
GS RAS(Verified) Federal research center, Geophysical survey of Russian Academy of Sciences
|
|
2
|
20:28:57.9
|
36.57 |
67.51 |
10.0 |
19
|
|
6.4/19 |
8.5-9 |
|
GS RAS(Preliminary) Federal research center, Geophysical survey of Russian Academy of Sciences
|
|
3
|
20:29:01.2
|
36.62 |
67.54 |
25.0 |
1195
|
Mw 6.3 |
6.3/521 |
|
26
|
CSEM European - Mediterranean seismological center
|
|
4
|
20:29:02.0
|
36.59 |
67.48 |
28.0 |
112
|
6.1/26 |
6.2/309 |
|
46
|
NEIC National Earthquakes Information Center of US Geological Service
|
Fig. 1 presents fragments of records obtained from digital stations Chuyangaron (∆ 2.6º), Jizzakh (∆ 3.6º), Ala-Archa (∆ 8.2º), Makanchi (∆ 15.1º), Garni (∆ 18.2º). Fig. 2 presents fragments of records obtained from digital stations Nalchik (∆ 19.5º), Neytrino (∆ 20.1º), Kislovodsk (∆ 20.3º), Arti (∆ 20.8º), Sverdlovsk (∆ 20.9º).
Image 1
Image 2
Focal mechanism solution of the origin was calculated by GS RAS with signs of initial arrivals of P waves at 81 stations, including 23 stations which registered compression waves (plus signs), and 58 stations which registered tensile waves (minus signs). The stations are located in the interval of epicentral distances 3.6-92.0º and in azimuth sector Az=3-354º. Focal mechanism solution in stereographic projection on the lower hemisphere and elements of the mechanism are presented in the table. The table also contains focal mechanism solutions obtained at the USGS NEIC with WW-phase Moment Tensor (Mww) technique and in Lamont-Dohert Earth Observatory of Columbia University, USA (LDEO GCMT) with СМТ (Centroid moment tensor) technique. Solutions from different centers are close. The earthquake was caused by slight prevalence of north-oriented compression stresses (AZ=357-3º). One nodal plane NP1 strikes W-SW (STK=236-243º), another plane NP2 strikes SE (STK=135-138º). NP2 plane is more horizontal (DP=41-47º) if compared with NP1 (DP=76-80º). The type of motion along NP1 – left lateral slip with reverse fault component, along NP2 – right lateral slip. The seismic moment according to USGS NEIC makes Mo= 3.339•10*18 N•m, Mww=6.28. According to LDEO GCMT it makes Mo= 3.95•10*18 N•m, Mw=6.3.
| Axes of main strengths |
Nodal planes |
Center |
|
| T |
P |
N |
NP1 |
NP2 |
PI: 43
Azm: 112
|
PI: 19
Azm: 3
|
PI: 41
Azm: 256
|
Stk: 243
Dp: 76
Slip: 48
|
Stk: 138
Dp: 44
Slip: 159
|
GS RAS Federal research center, Geophysical survey of Russian Academy of Sciences
|
|
PI: 42
Azm: 110
|
PI: 23
Azm: 357
|
PI: 39
Azm: 247
|
Stk: 238
Dp: 79
Slip: 50
|
Stk: 135
Dp: 41
Slip: 163
|
NEIC National Earthquakes Information Center of US Geological Service
|
|
PI: 37
Azm: 106
|
PI: 21
Azm: 360
|
PI: 46
Azm: 247
|
Stk: 236
Dp: 80
Slip: 43
|
Stk: 137
Dp: 47
Slip: 166
|
GCMT Lamont-Doherty Earth Observatory Global CMT Columbia University, USA
|
|