Magnitude |
:2.9 |
| Date & Time (UTC) | 2018-02-08 16:20:55.4 |
| Date & Time (Local) | 1396/11/19 19:50:55.4 |
| Location | Lat:28.004 Lon: 57.738 |
| Region | Kerman Province, 7 km of Kahnuj |
Nearest Cities |
|
| 7 km North of Kahnuj, Kerman Province | |
| 30 km South East of Bolock, Kerman Province | |
| 34 km East of Mehrueye-e paeen, Kerman Province | |
| 42 km North of Bargah, Kerman Province | |
| 46 km East of Faryab, Kerman Province | |
| Depth | 18 km |
| Agency | |
Faults within 150 km: |
|
| JIROFT_F (Length: 144 km) , Distance to epicenter: 5 km | |
| SABZEVARAN_F (Length: 190 km) , Distance to epicenter: 6 km | |
| MAIN_ZAGROS_R_F (Length: 1106 km) , Distance to epicenter: 85 km | |
| Number of Phases | 6 |
| RMS | 0.1 |
| Number of Stations | 4 |
| Error in Latitude | >1.4 km |
| Error in Longitude | 2.9 km |
| Error in Depth | 5.3 km |
Download waveform in seisan format
to download seisan software Click here
to access information about IIEES stations Click here
Amplitude | ||||||||
| UID | Agency | Station | Component | Amplitude | Period | Arrival Time | Proccessing Time | Signal Clip |
| 128278 | IIEES | BNDS | E | 167.2 | 0.41 | 2018-02-08 16:21:45 | 2018-02-13 07:08:00 | n |
| 128279 | IIEES | KRBR | N | 62 | 0.73 | 2018-02-08 16:22:12 | 2018-02-13 07:08:00 | n |
Phase | ||||||||||||
| Agency | Station | Component | Phase Type | Phase Quality | First Motion | Observed Arrival Time | Time Residual | Loc. Flag | Input Weight | Distance | Azimuth | |
| IIEES | BNDS | Z | Pg | E | 2018-02-08 16:21:23 | -0.09 | y | 168 | 247 | |||
| IIEES | BNDS | E | Sg | E | 2018-02-08 16:21:43 | 0.07 | y | 168 | 247 | |||
| IIEES | KRBR | Z | Pn | E | 2018-02-08 16:21:32 | -0.03 | y | 239 | 337 | |||
| IIEES | KRBR | N | Sg | E | 2018-02-08 16:22:03 | 0.03 | y | 239 | 337 | |||
| IIEES | ZHSF | Z | Pn | E | 2018-02-08 16:21:45 | 0.1 | y | 346 | 58 | |||
| IIEES | BSRN | Z | Pn | E | 2018-02-08 16:21:59 | -0.09 | y | 459 | 17 | |||
کلیه حقوق مادی و معنوی این سایت متعلق به پژوهشگاه بین المللی زلزله شناسی و مهندسی زلزله می باشد.
