Search Results - "Yaminifard, F."

Complex co- and postseismic faulting of the 2017–2018 seismic sequence in western Iran revealed by InSAR and seismic data by Fathian, A., Atzori, S., Nazari, H., Reicherter, K., Salvi, S., Svigkas, N., Tatar, M., Tolomei, C., Yaminifard, F.

“…The largest earthquake in the Zagros Mountains struck the city of Azgeleh on the Iran–Iraq border on 12 November 2017. This Mw 7.3 earthquake was followed by…”
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High‐Resolution Local Earthquake Tomography Beneath the Zagros Simply Folded Belt (SFB): Implications for an Inhomogeneous Low‐Velocity Layer and Diapirism in the Upper Crust by Kianimehr, H., Kissling, E., Yaminifard, F., Tatar, M.

“…Abstract Hormuz salt formation is considered the origin of the evaporated salt deposits in the Zagros and its ductile behavior has been known as the reason for…”
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Regional minimum 1-D P-wave velocity model for a new seismicity catalogue with precise and consistent earthquake locations in southern Iran by Kianimehr, H., Kissling, E., Yaminifard, F., Tatar, M.

“…For faster and more robust ray tracing in 1-D velocity models and also due to the lack of reliable 3-D models, most seismological centers use 1-D models for…”
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Source process and slip model of 2005 Dahuiyeh‐Zarand earthquake (Iran) using inversion of near‐field strong motion data by Rouhollahi, R., Ghayamghamian, M. R., Yaminifard, F., Suhadolc, P., Tatar, M.

“…SUMMARY On 2005 February 22, the Dahuiyeh‐Zarand earthquake, Mw 6.5, struck one of the most seismically active regions in south‐central Iran, east of Zarand…”
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Crustal velocity structure in the southern edge of the Central Alborz (Iran) by Abbassi, A., Nasrabadi, A., Tatar, M., Yaminifard, F., Abbassi, M.R., Hatzfeld, D., Priestley, K.

“…Inversion of local earthquake travel times and joint inversion of receiver functions and Rayleigh wave group velocity measurements were used to derive a simple…”
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Aftershocks study of the 2006 Silakhur earthquake (Zagros, Iran): seismological evidences for a pull-apart basin along the Main Recent Fault, Doroud segments by Sepahvand, M. R., Yaminifard, F., Tatar, M., Abbassi, M. R.

“…The Doroud segment of the Main Recent Fault (“MRF”) is studied by installing a local seismic network of 35 short-period stations for a period of 13 weeks from…”
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High‐Resolution Earthquake Local Tomography Beneath the Zagros Simply Folded Belt (SFB): Implications for an Inhomogeneous Low‐Velocity Layer and Diapirism in the Upper Crust by Kianimehr, H., Kissling, E., Yaminifard, F., Tatar, M.

“…Hormuz salt formation is considered the origin of the evaporated salt deposits in the Zagros and its ductile behavior has been known as the reason for the…”
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Active faulting of the southeastern-most Zagros (Iran): Microearthquake seismicity and crustal structure by Yaminifard, F., Sedghi, M. Hassanpour, Gholamzadeh, A., Tatar, M., Hessami, K.

“…► Studied region in this paper located in the southeastern-most Zagros. ► Studied region also mainly includes the Khurgu earthquake region, Ms=7. ► We recorded…”
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Aftershock analysis of the 2005 November 27 (Mw 5.8) Qeshm Island earthquake (Zagros-Iran): Triggering of strike-slip faults at the basement by Yaminifard, F., Tatar, M., Hessami, K., Gholamzadeh, A., Bergman, E.A.

“…► We installed 17 seismic stations after 2005 Qeshm earthquake for aftershock study. ► In this study we analysis 2617 aftershocks and calculate 183 focal…”
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Source process and slip model of 2005 Dahuiyeh-Zarand earthquake (Iran) using inversion of near-field strong motion data: Source process of 2005 Dahuiyeh-Zarand EQ by Rouhollahi, R., Ghayamghamian, M. R., Yaminifard, F., Suhadolc, P., Tatar, M.

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