Recognition of the causative fault of the 2017 MW 4.9 Malard (Tehran, Iran) earthquake from directivity analysis of the recorded ground motions-Reference-Cited by-同舟云学术

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Recognition of the causative fault of the 2017 MW 4.9 Malard (Tehran, Iran) earthquake from directivity analysis of the recorded ground motions

Published:2023-12 Issue: Volume:345 Page:107116
ISSN:0031-9201
Container-title:Physics of the Earth and Planetary Interiors
language:en
Short-container-title:Physics of the Earth and Planetary Interiors

Author:

Naserieh Saeid,Pakzad Mehrdad,Ghofrani Hadi,Dezvareh Mohsen,Karkooti Ehsan,Moradi Ali,Shahvar Mohammad

Publisher

Elsevier BV

Subject

Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics

Reference65 articles.

1. Accommodation of late Cenozoic oblique shortening in the Alborz range, northern Iran;Allen;J. Struct. Geol.,2003

2. A History of Persian Earthquakes;Ambraseys,1982

3. Wrinkle-like slip pulse on a fault between different materials;Andrews;J. Geophys. Res.,1997

4. Effects of fault finiteness on near-source ground motion;Archuleta;Bull. Seismol. Soc. Am.,1981

5. Attenuation of the Lg phase and site response for the eastern Canada telemetered network;Atkinson;Seismol. Res. Lett.,1989

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