COMPUTING MAXIMUM SEISMIC ACCELERATION OF NORTH TABRIZ FAULT USING EARTHQUAKE SIMULATION BASED ON FINITE FAULT SOURCE

Q: How can I download an article?

To download an article from SID, first log in to the site, search for the article title, and click on the 'Download Article' option.

Q: How can I download an ISI article?

To download an ISI article on SID, enter the keyword or article title in the search bar, view the relevant results, click on the desired article, and select the 'Download Article' option.

Q: How can I access the SID database?

To access the SID database, visit SID.ir, create an account, and log in to access scientific resources.

Q: Is downloading articles from SID free?

Some articles on SID are available for free, while others require payment. Details are specified on the article's page.

AMIRANLOU H.; POURKERMANI M.; DABIRI R.; QORESHI M.; BOUZARI S.

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2017 | Volume:27 | Issue:105 Page(s): 193-198

Download Full-Text

Persian Verion

View:

1,097

Download:

Cites:

Information Journal Paper

Title

COMPUTING MAXIMUM SEISMIC ACCELERATION OF NORTH TABRIZ FAULT USING EARTHQUAKE SIMULATION BASED ON FINITE FAULT SOURCE

Author(s)

Keywords

MAXIMUM ACCELERATIONQ2

GROUND MOTIONQ2

NORTH TABRIZ FAULTQ2

FINITE FAULT SOURCEQ1

Abstract

The occurrence of historical and instrumental earthquakes near the NORTH TABRIZ FAULT in NW Iran is an evidence for seismic activity of this fault, which recorded historical earthquakes with magnitudes greater than 7.Inthis study, existing experimental relations, historical seismicity, and the fault geometry were used to define a Mw 7.7 earthquake scenario. The stochastic finite fault modeling based on a dynamic comer frequency shows a good agreement between maximum estimated acceleration and common attenuation patterns. The derived shake map illustrates that the stongest GROUND MOTION is observed in the NW, Nand NE of the tabriz city along a zone parallel to the fault. In addition, the MAXIMUM ACCELERATION derived from simulation is almost equal to that computed from attenuation patterns.

Cites

No record.

References

No record.

Cite

APA: Copy

AMIRANLOU, H., POURKERMANI, M., DABIRI, R., QORESHI, M., & BOUZARI, S.. (2017). COMPUTING MAXIMUM SEISMIC ACCELERATION OF NORTH TABRIZ FAULT USING EARTHQUAKE SIMULATION BASED ON FINITE FAULT SOURCE. GEOSCIENCES, 27(105 ), 193-198. SID. https://sid.ir/paper/32269/en

Vancouver: Copy

AMIRANLOU H., POURKERMANI M., DABIRI R., QORESHI M., BOUZARI S.. COMPUTING MAXIMUM SEISMIC ACCELERATION OF NORTH TABRIZ FAULT USING EARTHQUAKE SIMULATION BASED ON FINITE FAULT SOURCE. GEOSCIENCES[Internet]. 2017;27(105 ):193-198. Available from: https://sid.ir/paper/32269/en

IEEE: Copy

H. AMIRANLOU, M. POURKERMANI, R. DABIRI, M. QORESHI, and S. BOUZARI, “COMPUTING MAXIMUM SEISMIC ACCELERATION OF NORTH TABRIZ FAULT USING EARTHQUAKE SIMULATION BASED ON FINITE FAULT SOURCE,” GEOSCIENCES, vol. 27, no. 105 , pp. 193–198, 2017, [Online]. Available: https://sid.ir/paper/32269/en

Related Journal Papers