Hossein Memarian

Hossein Memarian


Research Focus & Metrics

Academic Career Length

24Years (2003-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 May 2012 in Journal of Petroleum Science and Engineering
Verified
Journal Article
Closed access
FKF. Khoshbakht
F. Khoshbakht
MAM. Azizzadeh
M. Azizzadeh
HMHossein Memarian
Hossein Memarian
GNG.H. Nourozi
G.H. Nourozi
SMS.A. Moallemi
S.A. Moallemi

1 July 2009 in Journal of Petroleum Science and Engineering
Verified
Journal Article
Closed access
FKF. Khoshbakht
F. Khoshbakht
HMHossein Memarian
Hossein Memarian
MMM. Mohammadnia
M. Mohammadnia

1 May 2010 in Journal of Petroleum Science and Engineering
Verified
Journal Article
Closed access
BTBehzad Tokhmchi
Behzad Tokhmchi
HMHossein Memarian
Hossein Memarian
Reza  RezaeeReza Rezaee
Reza Rezaee

17 March 2013 in Journal of Seismology
Verified
Journal Article
Closed access
PDF file
SKSepideh Karimiparidari
Sepideh Karimiparidari
MZMehdi Zaré
Mehdi Zaré
HMHossein Memarian
Hossein Memarian
AKAndrzej Kijko
Andrzej Kijko

Verified
Journal Article
Open access
PDF file
FKFarnaz Kamranzad
Farnaz Kamranzad
HMHossein Memarian
Hossein Memarian
MZMehdi Zare
Mehdi Zare
The megacity of Tehran, the capital of Iran, is subjected to a high earthquake risk. Located at the central part of the Alpine–Himalayan seismic belt, Tehran is surrounded by several active faults that show some M7+ historical earthquake records. The high seismic hazard in combination with a dense population distribution and several vulnerability factors mean Tehran is one of the top 20 worldwide megacities at a high earthquake risk. This article aims to prepare an assessment of the present-day earthquake risk in Tehran. First, the earthquake risk components including hazard, exposure, and vulnerability are evaluated based on some accessible GIS-based datasets (e.g., seismicity, geology, active faults, population distribution, land use, urban fabric, buildings’ height and occupancy, structure types, and ages, as well as the vicinity to some critical infrastructures). Then, earthquake hazard maps in terms of PGA are prepared using a probabilistic approach as well as a surface rupture width map. Exposure and vulnerability maps are also provided deterministically in terms of population density and hybrid physical vulnerability, respectively. Finally, all these components are combined in a spatial framework and an earthquake risk map is provided for Tehran.

29 September 2009 in Journal of Geophysics and Engineering
Verified
Journal Article
Closed access
BTB Tokhmechi
B Tokhmechi
HMHossein Memarian
Hossein Memarian
HNH A Noubari
H A Noubari
BMB Moshiri
B Moshiri