Space and Time Evolution of the Rupture for the 2010 August 27 Mw 5.8 Kuh-zar earthquake
This study investigated the spatiotemporal slip distribution of the 2010 August 27 Mw 5.8 Kuh-zar earthquake. Using the constrained non-negative least-squares linear slip inversion method, we calculated the amount of displacement on the fault plane. The spatial slip distribution of this earthquake h...
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Damghan university
2020-04-01
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Series: | Iranian Journal of Astronomy and Astrophysics |
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Online Access: | https://ijaa.du.ac.ir/article_182_5877754e20f659760b712c9017cb6405.pdf |
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author | Nazila Asaadi Sonia Bazargan |
author_facet | Nazila Asaadi Sonia Bazargan |
author_sort | Nazila Asaadi |
collection | DOAJ |
description | This study investigated the spatiotemporal slip distribution of the 2010 August 27 Mw 5.8 Kuh-zar earthquake. Using the constrained non-negative least-squares linear slip inversion method, we calculated the amount of displacement on the fault plane. The spatial slip distribution of this earthquake has been estimated by Bazargan et al. (2018), while the delta is 0.1 s ( delta is sampling rate means10 samples in 1 second). Here, we re-evaluated the slip with delta = 0.2 s to improve their result. A great many inversions were carried to determine the optimal parameters used in the process such as rupture velocity and rise time. In this study, we used the same rupture velocity and rise time, namely 2.55 km/s and 1.8 s. In general, the rupture velocity is 80% to 90% of the shear wave velocity, except for the propagation of ultrasonic faults, in which it has dimensions equal to the P-wave velocity. Selecting the size of the rupture rate has a significant effect on the size of the slip and its area. Since the slip inversion results can have a high level of uncertainty, we tried to develop the previous results by using different delta and adding time evolution to the calculations. The spatiotemporal slip distribution of this event got a data fit of 48% with an 8 cm peak slip. |
format | Article |
id | doaj-art-d3025a9235504ea2bcbc38d36fbde604 |
institution | Kabale University |
issn | 2322-4924 2383-403X |
language | English |
publishDate | 2020-04-01 |
publisher | Damghan university |
record_format | Article |
series | Iranian Journal of Astronomy and Astrophysics |
spelling | doaj-art-d3025a9235504ea2bcbc38d36fbde6042025-01-12T10:10:45ZengDamghan universityIranian Journal of Astronomy and Astrophysics2322-49242383-403X2020-04-0171253110.22128/ijaa.2020.407.1085182Space and Time Evolution of the Rupture for the 2010 August 27 Mw 5.8 Kuh-zar earthquakeNazila Asaadi0Sonia Bazargan1Physics Department, Zanjan University, Zanjan, IranInstitute of Geophysics, University of Tehran, Tehran, IranThis study investigated the spatiotemporal slip distribution of the 2010 August 27 Mw 5.8 Kuh-zar earthquake. Using the constrained non-negative least-squares linear slip inversion method, we calculated the amount of displacement on the fault plane. The spatial slip distribution of this earthquake has been estimated by Bazargan et al. (2018), while the delta is 0.1 s ( delta is sampling rate means10 samples in 1 second). Here, we re-evaluated the slip with delta = 0.2 s to improve their result. A great many inversions were carried to determine the optimal parameters used in the process such as rupture velocity and rise time. In this study, we used the same rupture velocity and rise time, namely 2.55 km/s and 1.8 s. In general, the rupture velocity is 80% to 90% of the shear wave velocity, except for the propagation of ultrasonic faults, in which it has dimensions equal to the P-wave velocity. Selecting the size of the rupture rate has a significant effect on the size of the slip and its area. Since the slip inversion results can have a high level of uncertainty, we tried to develop the previous results by using different delta and adding time evolution to the calculations. The spatiotemporal slip distribution of this event got a data fit of 48% with an 8 cm peak slip.https://ijaa.du.ac.ir/article_182_5877754e20f659760b712c9017cb6405.pdfthe 2010 juh-zar earthquakeseismic dataslip inversion |
spellingShingle | Nazila Asaadi Sonia Bazargan Space and Time Evolution of the Rupture for the 2010 August 27 Mw 5.8 Kuh-zar earthquake Iranian Journal of Astronomy and Astrophysics the 2010 juh-zar earthquake seismic data slip inversion |
title | Space and Time Evolution of the Rupture for the 2010 August 27 Mw 5.8 Kuh-zar earthquake |
title_full | Space and Time Evolution of the Rupture for the 2010 August 27 Mw 5.8 Kuh-zar earthquake |
title_fullStr | Space and Time Evolution of the Rupture for the 2010 August 27 Mw 5.8 Kuh-zar earthquake |
title_full_unstemmed | Space and Time Evolution of the Rupture for the 2010 August 27 Mw 5.8 Kuh-zar earthquake |
title_short | Space and Time Evolution of the Rupture for the 2010 August 27 Mw 5.8 Kuh-zar earthquake |
title_sort | space and time evolution of the rupture for the 2010 august 27 mw 5 8 kuh zar earthquake |
topic | the 2010 juh-zar earthquake seismic data slip inversion |
url | https://ijaa.du.ac.ir/article_182_5877754e20f659760b712c9017cb6405.pdf |
work_keys_str_mv | AT nazilaasaadi spaceandtimeevolutionoftheruptureforthe2010august27mw58kuhzarearthquake AT soniabazargan spaceandtimeevolutionoftheruptureforthe2010august27mw58kuhzarearthquake |