Three-Dimensional P-Wave Velocity Structure of Tehran from Local Micro-Earthquake Tomography

Tehran region is located at the southern foothills of central Alborz Mountains which is one of the most seismically active regions due to the convergence between the Arabian and the Eurasian plates. In this study, 3-D crustal velocity structure of Tehran region was investigated using first P-wave ar...

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Bibliographic Details
Published in:Pure and applied geophysics 2019-11, Vol.176 (11), p.4783-4796
Main Authors: Shirzad, Taghi, Naghavi, Mojtaba, Afra, Mahsa, YaminiFard, Farzam
Format: Article
Language:English
Subjects:
Anomalies
Bedrock
Disaster management
Earth and Environmental Science
Earth Sciences
Earthquake engineering
Earthquakes
Emergency preparedness
Foothills
Geophysics/Geodesy
Least squares method
Mitigation
Mountains
Organizations
Plate tectonics
Profiles
Seismic activity
Seismic engineering
Seismic wave velocities
Seismology
Tectonics
Thickness
Thin films
Tomography
Velocity
Wave velocity
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Summary:Tehran region is located at the southern foothills of central Alborz Mountains which is one of the most seismically active regions due to the convergence between the Arabian and the Eurasian plates. In this study, 3-D crustal velocity structure of Tehran region was investigated using first P-wave arrival times of events with magnitudes less than 4. Data used was recorded by the stations from Tehran Disaster Management and Mitigation Organization, Iranian Seismological Center and International Institute of Earthquake Engineering and Seismology from 2004 to 2018. In order to obtain the crustal velocity structure of Tehran, iterative, damped least-squares method was used to solve/obtain earthquake parameters and velocity structures, simultaneously. Final results show three tectonic characteristics in the study area including high velocity anomalies in northern and eastern Tehran Mountains, and low velocity anomaly in triangular Tehran basin, so that the separation of the eastern Tehran Mountains and Tehran basin is especially sharp in cross-section profiles. Moreover, some low velocity anomalies are appeared around major faults in the study area (e.g. North Tehran Fault). The tomographic maps also show that the Tehran region contains of an upper crust layer with the thickness of 6 km which is located over middle crust layer bedrock with constant velocity up to 15 km. This upper crust layer consists of a sedimentary layer (~ 3 km thickness) overlaid a basement layer. Moreover, the thick and thin upper crust layers are separated by North Tehran and Kosar/Ghasr-Firooz faultsystems from the Tehran basin, respectively.
ISSN:0033-4553
1420-9136
DOI:10.1007/s00024-019-02269-2