A Strong Ground Motion Catalogue of Selected Records for Shallow Crustal, Near Field Earthquakes in Iran

محورهای موضوعی : Mineralogy

Maryam Sedghi ¹ (Department of Geology, North Tehran Branch, Islamic Azad University, Tehran, Iran|Iranian Red Crescent Society (IRCS), Tehran, Iran)
Arezou Dorostian ² (Department of Geology, North Tehran Branch, Islamic Azad University, Tehran, Iran)
Mehdi Zare ³ (International Institute of Earthquake Engineering and Seismology (IIEES), Tehran, Iran)
Mohsen Pourkermani ⁴ (Department of Geology, North Tehran Branch, Islamic Azad University, Tehran, Iran)

تاریخ دریافت : 1398/03/14 تاریخ پذیرش : 1398/07/23 تاریخ انتشار : 1399/01/13

کلید واژه: Strong motion, Near fault, Catalogue, Earthquake,

چکیده مقاله :

Understanding strong ground motions in the near-fault areas is important for seismic risk assessment in densely populated areas. In the past, lack of information on strong ground motion for large and moderate earthquakes led to the use of mainly far field large and moderate earthquake records in equations for calculation of the strong ground motion parameters. In this article, we collected and generated a seismic catalogue with a data set of corrected and processed 217 triaxial near source strong ground motion and accelerometric data recorded from 1976 to 2018 obtained from 30 shallow crustal earthquakes with a focal depth below 30 km from different regions including 24 in Iran, 5 in California and one in Italy (because of the lack of Iranian near-field accelerograms) in different stations. These data were recorded (129 Iranian records, 88 from California and Italy) with a source-to-site distance less than 80 km and earthquakes between Mw = 5 and 7.5. Receiver function method was used for site classification for these records. The percentage of processed data in this study was 18%, 43%, 33% and 6% for the different site classes of 1, 2, 3, and 4. In the final catalog, records in which their PGA≥ 100 cm /s2, were reported. This near source ground motion database also contains information about ground motion, source parameters and is fundamental for dynamic research in earthquake engineering for the estimation of strong ground motion parameters (PGA, PGV, PGD and frequency content of response spectra) of moderate-to-large earthquakes.

منابع و مأخذ:

1. Aki K (1968) Seismic displacements near a fault, Journal of Geophysical Research 73:5359-5376.


2. Akkar S, Bommer JJ (2007) Prediction of elastic displacement response spectra in Europe and the Middle East, Earthquake Engineering & Structural Dynamics 36:1275-1301.


3. Ambraseys N, Melville C (1982) A History of Persian Earthquakes ̧Cambridge University Press. London.


4. Ambraseys N, Smit P, Douglas J, Margaris B, Sigbjörnsson R, Olafsson S, Suhadolc P, Costa G (2004) Internet site for European strong-motion data, Bollettino di geofisica teorica ed applicata 45:113-129.


5. Boore DM, Zoback MD (1974) Near-field motions from kinematic models of propagating faults, Bulletin of the Seismological Society of America 64:321-342.


6. Bouchon M (1979) Predictability of ground displacement and velocity near an earthquake fault: An example: The Parkfield earthquake of 1966, Journal of Geophysical Research: Solid Earth 84:6149-6156.


7. Campbell KW, Bozorgnia Y (2013) NGA-West2 Campbell-Bozorgnia ground motion model for the horizontal components of PGA, PGV, and 5%-damped elastic pseudo-acceleration response spectra for periods ranging from 0.01 to 10 sec. Pacific Earthquake Engineering Research Center,


8. Chu D, Gordon RG (1998) Current plate motions across the Red Sea, Geophysical Journal International 135:313-328.


9. Code IS (2005) Iranian code of practice for seismic resistant design of buildings, Standard.


10. Council BSS (2000) The 2000 NEHRP recommended provisions for new buildings and other structures: Part I (Provisions) and Part II (Commentary), FEMA 368:369.


11. Engdahl ER, van der Hilst R, Buland R (1998) Global teleseismic earthquake relocation with improved travel times and procedures for depth determination, Bulletin of the Seismological Society of America 88:722-743.


12. Forootan M, Silakhori E, Alvandi E (2015) Soil Liquefaction Hazard Zonation Map for Kordkuy County, Golsetan Province Using Model SWM, IRANIAN JOURNAL OF EARTH SCIENCES 7:46-49.


13. Gutenberg B, Richter CF (1944) Frequency of earthquakes in California, Bulletin of the Seismological Society of America 34:185-188.


14. Hanks TC, Kanamori H (1979) A moment magnitude scale, Journal of Geophysical Research: Solid Earth 84:2348-2350.


15. Hartzell SH (1978) Earthquake aftershocks as Green's functions, Geophysical Research Letters 5:1-4.


16. Haskell NA (1969) Elastic displacements in the near-field of a propagating fault, Bulletin of the Seismological Society of America 59:865-908.


17. Israel M, Kovach RL (1977) Near-field motions from a propagating strike-slip fault in an elastic half-space, Bulletin of the Seismological Society of America 67:977-994.


18. Kramer S (1996) Geotechnical Earthquake Engineering. Prentice-Hall, Inc, New Jersey:348-422.


19. Levy N, Mal A (1976) Calculation of ground motion in a three-dimensional model of the 1966 Parkfield earthquake, Bulletin of the Seismological Society of America 66:405-423.


20. Maggi A, Priestley K, Jackson J (2002) Focal depths of moderate and large size earthquakes in Iran, Journal of Seismology and Earthquake Engineering 4:1-10.


21. Pecknold DA, Riddell R (1978) Effect of initial base motion on response spectra, Journal of the Engineering Mechanics Division 104:485-491.


22. Theodulidis N, Bard P-Y (1995) Horizontal to vertical spectral ratio and geological conditions: an analysis of strong motion data from Greece and Taiwan (SMART-1), Soil dynamics and earthquake engineering 14:177-197.


23. Zaré M (2007) Spectral Demand Curves Based on the Selected Strong Motion Records in Iran, Journal of Seismology and Earthquake Engineering 9:111-123.