Author/Authors :
Pourmohammad Shahvar, Mohammad Road, Housing and Urban Development Research Center, BHRC, Tehran, Iran , Eshaghi, Attieh Road, Housing and Urban Development Research Center, BHRC, Tehran, Iran , Farzanegan, Esmaeil Road, Housing and Urban Development Research Center, BHRC, Tehran, Iran , Mirzaei Alavijeh, Hossein Road, Housing and Urban Development Research Center, BHRC, Tehran, Iran
Abstract :
In this study, seismological aspects of the 2017 Sarpol-e Zahab earthquake has been
investigated. The Sarpol-e Zahab earthquake, of magnitude 7.3 (Mw), occurred in
southwestern Iran on November 12, 2017. Here, we investigated the properties of
the strong ground motions of the earthquake using the records provided by Iranian
Strong Motion Network (ISMN). At Sarpol-e Zahab (SPZ) station, about 30 km
south of the epicenter, the recorded peak ground acceleration (PGA) and
peak ground velocity (PGV) in both horizontal and vertical components were
remarkably large, and visual inspection of the velocity time history reveals a
pulse-like shape. Besides, the response spectra of the recordings were determined
and were compared to the 2800 seismic code spectrum. Furthermore, the
earthquake engineering parameters for this earthquake were estimated and were
compared with the values of other large destructive earthquakes in Iran. Finally,
based on the recorded strong motion data and observed information such as the
macroseismic intensity, ShakeMaps of this earthquake have been generated, which
clearly shows the most affected areas that needed the immediate assistance and aid
after the earthquake. These maps are fundamental for earthquake rapid response
procedures and the earthquake crisis management.
Keywords :
Sarpol-e Zahab , Strong motion , Response spectra , Shakemap