| Author | |
| Date and time | 2016-02-17 07:08:38.5 UTC |
| Latitude | 33.810 |
| Longitude | 56.939 |
| Depth | 8 |
| Magnitude | 3.9 ML |
| Region | CENTRAL IRAN |
| Latest update | 2016-04-19 07:25:59.2 UTC |
| rms | -- s |
| N° phases used for the localisation | 20 |
| N° stations used for the localisation | 20 |
| Gap | 67.0 ° |
| 95% confidence ellipse | |
| semi major | -- |
| semi minor | -- |
| Azimuth | -- ° |
| Location Type | manual |
Download data for this event
Note: links can take up to 20 minutes from the earthquake to become available
| Network | code | Distance° | EvAz | A/M | Phase | Pick time | Residual | T | Author |
|---|---|---|---|---|---|---|---|---|---|
| IAFRZ | M | Pg | 2016-02-17 07:09:11.4 | 0.00 | T | ||||
| IAKL | 3.120 | 27 | M | Pn | 2016-02-17 07:09:30.9 | 0.00 | T | ||
| ANAR | 2.750 | 258 | M | Pn | 2016-02-17 07:09:24.8 | 0.00 | T | ||
| IANJ | 2.990 | 304 | M | Pn | 2016-02-17 07:09:28.5 | 0.00 | T | ||
| IBAF | 2.500 | 208 | M | Pn | 2016-02-17 07:09:21.5 | 0.00 | T | ||
| ICHK | 2.640 | 234 | M | Pn | 2016-02-17 07:09:23.3 | 0.00 | T | ||
| IDAH | 2.680 | 113 | M | Pn | 2016-02-17 07:09:24.4 | 0.00 | T | ||
| JRKH | 3.500 | 52 | M | Pn | 2016-02-17 07:09:36.0 | 0.00 | T | ||
| KHGB | 3.450 | 187 | M | Pn | 2016-02-17 07:09:35.4 | 0.00 | T | ||
| IKOO | 2.220 | 128 | M | Pn | 2016-02-17 07:09:17.6 | 0.00 | T | ||
| IKRD | 3.230 | 23 | M | Pn | 2016-02-17 07:09:38.0 | 0.00 | T | ||
| IMON | 2.360 | 104 | M | Pn | 2016-02-17 07:09:20.1 | 0.00 | T | ||
| SBZV | 2.630 | 12 | M | Pn | 2016-02-17 07:09:23.8 | 0.00 | T | ||
| ITBJM | M | Pn | 2016-02-17 07:09:30.3 | 0.00 | T | ||||
| ITEG | 1.770 | 121 | M | Pg | 2016-02-17 07:09:11.4 | 0.00 | T | ||
| TKDS | 0.250 | 142 | M | Pg | 2016-02-17 07:08:43.7 | 0.00 | T | ||
| TKDS | 0.250 | 142 | M | Sg | 2016-02-17 07:08:48.6 | 0.00 | T | ||
| TNSG | 0.310 | 299 | M | Pg | 2016-02-17 07:08:45.1 | 0.00 | T | ||
| TPRV | 0.810 | 195 | M | Pg | 2016-02-17 07:08:54.1 | 0.00 | T | ||
| TVBK | 3.820 | 182 | M | Pn | 2016-02-17 07:09:40.3 | 0.00 | T |