The red marker on the map displays the epicenter of the earthquake, its focus was located on the territory of the island of Leyte, Philippines, at a depth of 10 km, 8 km south of Yaro, 26 km SW of Tacloban and 27 km E-SE of Kananga.
|
Time in origin (GMT) |
Latitude, degree |
Longitude, degree |
Depth, km |
Stations number |
Ms/N |
mb/N |
I0 (calculated) |
GAP |
Center |
| 1
|
08:03:54.1
|
11.12 |
124.8 |
10.0 |
66
|
6.6/32 |
6.3/45 |
9-9.5 |
55
|
GS RAS(Verified) Federal research center, Geophysical survey of Russian Academy of Sciences
|
|
2
|
08:03:55.5
|
10.99 |
124.49 |
10.0 |
24
|
|
6.4/22 |
8.5-9 |
|
GS RAS(Preliminary) Federal research center, Geophysical survey of Russian Academy of Sciences
|
|
3
|
08:03:58.3
|
11.11 |
124.8 |
10.0 |
199
|
Mw 6.5 |
|
|
74
|
CSEM European - Mediterranean seismological center
|
|
4
|
08:03:57.5
|
11.11 |
124.63 |
6.5 |
131
|
Mw 6.5 |
|
|
30
|
NEIC National Earthquakes Information Center of US Geological Service
|
Fig. 1 presents fragments of records obtained from digital stations Taejon (∆ 25.3º), Matsushiro (∆ 28.1º), Tennant Creek (∆ 32.3º), Vladivostok (∆ 32.5º), Ussuriysk (∆ 33.5º). Fig. 2 presents fragments of records obtained from digital stations Erimo (∆ 34.7º), Yuzhno-Sakhalinsk (∆ 38.8º), Ulaanbaatar (∆ 39.6º), Yakutsk (∆ 50.9º), Magadan (∆ 52.1º).
Image 1
Image 2
GS RAS registered one aftershock with М=4.8 in 2 hours 28 minutes after the main shock.
| N |
Time in origin (GMT) |
Latitude, degree |
Longitude, degree |
Depth, km |
Stations number |
Ms/N |
mb/N |
I0 (calculated) |
Region |
| 20172240
|
06/07/2017 10:31:49.0.0 |
11.2 |
124.95 |
10.0 |
16 |
|
4.8/10 |
4.5-5 |
Leyte, Philippines
|
The focal mechanism solution of the origin in stereographic projection on the lower hemisphere is shown in the table according to the data obtained in USGS NEIC with W-phase Moment Tensor (Mww) technique. The earthquake was caused by the prevalence of tension stresses (PL=0º) oriented to the south (Az=191º). The compression axes are directed to the west (Az=281º). The nodal plane NP1 strikes to the east (Stk=59º), NP2 strikes NW (Stk=324º). Both planes are inclined to the horizon at equal angles (the planes are steeply falling Dp=73º). The type of motion along both planes – slips with fault components (right latteral slip for NP1, left latteral for NP2). According to USGS NEIC Mo=7.056*10**18 N*m, Mww=6,5.
| Axes of main strengths |
Nodal planes |
Center |
|
| T |
P |
N |
NP1 |
NP2 |
PI: 0
Azm: 191
|
PI: 25
Azm: 281
|
PI: 65
Azm: 100
|
Stk: 59
Dp: 73
Slip: -162
|
Stk: 324
Dp: 73
Slip: -18
|
NEIC National Earthquakes Information Center of US Geological Service
|
|