The red marker on the map is the epicenter of the earthquake, the origin of which was located on the southern coast of the island of Mindanao, Philippines at a depth of 65 km, 54 km S-SW of General Santos, 171 kilometers S-SW of Davao and 1082 km S-SE of Manila, the capital of the Philippines.
|
Time in origin (GMT) |
Latitude, degree |
Longitude, degree |
Depth, km |
Stations number |
Ms/N |
mb/N |
I0 (calculated) |
GAP |
Center |
| 1
|
08:14:12.0
|
5.66 |
125.01 |
65.0 |
69
|
6.4/39 |
6.7/50 |
6-6.5 |
133
|
GS RAS(Verified) Federal research center, Geophysical survey of Russian Academy of Sciences
|
|
2
|
08:14:04.1
|
5.54 |
124.91 |
10.0 |
11
|
|
6.8/10 |
9.5-10 |
|
GS RAS(Preliminary) Federal research center, Geophysical survey of Russian Academy of Sciences
|
|
3
|
08:14:13.2
|
5.64 |
125.1 |
70.0 |
539
|
Mw 6.7 |
6.4/309 |
|
18
|
CSEM European - Mediterranean seismological center
|
|
4
|
08:14:13.2
|
5.59 |
125.05 |
78.0 |
117
|
Mw 6.7/41 |
6.6/368 |
|
21
|
NEIC National Earthquakes Information Center of US Geological Service
|
Fig. 1 presents fragments of records obtained from digital stations Kappang (∆ 11.8º), Tennant Creek (∆ 27º), Taejon (∆ 30.7º), Matsushiro (∆ 33º), Vladivostok (∆ 37.8º). Fig. 2 presents fragments of records obtained from digital stations Kuldur (∆ 43.8º), Talaya (∆ 49.2º), Severo-Kurilsk (∆ 51.8º), Yakutsk (∆ 56.4º), Magadan (∆ 57.3º).
Image 1
Image 2
Focal mechanism solution of the origin was calculated by GS RAS with signs of initial arrivals of P waves at 88 stations, including 73 stations which registered compression waves (plus signs), and 15 stations which registered tensile waves (minus signs). The stations are located in the interval of epicentral distances1.5-95.7º and in azimuth sector Az=1-358º. 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 W-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 occurred under the influence of prevailing compression stresses oriented to the east (AZ=81-82º). One nodal plane NP1 strikes north (STK=4-9º), another plane NP2 – strikes S-SE (STK=153-157º), both planes are dipping to the horizon at close angles (DIP=45-50º). The type of motion along both planes – reverse fault. Seismic moment according to USGS NEIC makes Mo=1.506 *10**19 N*m, Mww=6.7. According to LDEO GCMT it makes Mo=1.8*10**19 N*m, Mw=6.8.
| Axes of main strengths |
Nodal planes |
Center |
|
| T |
P |
N |
NP1 |
NP2 |
PI: 76
Azm: 351
|
PI: 0
Azm: 81
|
PI: 14
Azm: 171
|
Stk: 4
Dp: 47
Slip: 110
|
Stk: 157
Dp: 47
Slip: 70
|
GS RAS Federal research center, Geophysical survey of Russian Academy of Sciences
|
|
PI: 75
Azm: 351
|
PI: 0
Azm: 81
|
PI: 15
Azm: 171
|
Stk: 6
Dp: 47
Slip: 111
|
Stk: 157
Dp: 47
Slip: 69
|
NEIC National Earthquakes Information Center of US Geological Service
|
|
PI: 71
Azm: 344
|
PI: 3
Azm: 82
|
PI: 19
Azm: 173
|
Stk: 9
Dp: 50
Slip: 115
|
Stk: 153
Dp: 45
Slip: 63
|
GCMT Lamont-Doherty Earth Observatory Global CMT Columbia University, USA
|
|