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Seismic interferometry ambient noise tomography—a study in the north-central part of Iran

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Abstract

Seismic interferometry is one of the noteworthy new subsurface imaging methods that have been used in recent years in many tomographic studies. In this study, the interstation estimated Green functions extracted from the Rayleigh and Love wave ambient noise cross-correlations are used to obtain the Love and Rayleigh wave group velocity maps in different periods across the study area in order to determine the velocity anomalies and their corresponding geological structures within the crust. In the ambient noise method, the quality of the cross-correlations increases when longer time series of data are used, so we used 22 months of continuous data from the 17 broadband seismic stations as the primary database. After performing the initial corrections of the ambient noise data and obtaining the 3-month cross-correlation time series, the longer time series were obtained by stacking the 3-month time series with acceptable quality. In the next step, by using the time-frequency analysis and the estimated Green functions, the Love and Rayleigh wave dispersion curves were determined. Then, using the 2D tomography method, the Love and Rayleigh wave group velocity maps for the periods 10–25 s were produced. In the short periods, a low-velocity zone is observed in the Love and Rayleigh wave group velocity maps from the south Caspian basin toward central Iran, which is likely due to the effect of the thick alluvial deposits and the intermountain sediments in Alborz. At the longer periods, the Rayleigh and Love wave group velocity maps show a low-velocity zone in central Alborz, while in the eastern and western parts of Alborz, they show higher velocities, which is consistent with the prior studies. The dense path coverage permits to produce images that have substantially higher lateral resolution than is currently available from global and regional group velocity studies. Tomographic maps at high frequencies are well correlated with the upper crust structure and especially with sediment layer thickness.

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References

  • Abdetedal M, Shomali ZH, Gheitanchi MR (2014) Crust and upper mantle structures of the Makran subduction zone in south-east Iran by seismic ambient noise tomography. Solid Earth Discuss 6:1–34

    Google Scholar 

  • Allen MB, Ghassemi MR, Shahrabi M, Qorashi M (2003) Accommodation of late Cenozoic oblique shortening in the Alborz range, northern Iran. J Struct Geol 25(5):659–672

    Article  Google Scholar 

  • Ansaripour M, Rezapour M, Saygin E (2019) Shear wave velocity structure of Iranian plateau: using combination of ambient noise cross-correlations (C1) and correlation of coda of correlations (C3). Geophys J Int 218(3):1919–1938

    Article  Google Scholar 

  • Backus G, Gilbert F (1968) The resolving power of gross Karth data. Geophys J R Astron Soc 16:169–205

    Article  Google Scholar 

  • Bensen GD, Ritzwoller M.H, Barmin MP, Levshin AL, Lin F, Moschetti MP, Shapiro NM, Yang Y (2007) Processing seismic ambient noise data to obtain reliable broad-band surface wave dispersion measurements. Appl Geophys 153:563–585, Geophys J Int 169:1239-1260. doi:https://doi.org/10.1111/j.1365-246X.2007.03374

  • Ditmar PG, Yanovskya TB (1987) Generalization of Backus-Gilbert method for estimation of lateral variations of surface wave velocities. Phys Solid Earth, Izvestia Acad Sci USSR 23(6):470–477

    Google Scholar 

  • Dziewonski AM, Bloch S, Landisman M (1969) A technique for the analysis of transient seismic signals. Bull Seismol Soc Am 59:427–444

    Google Scholar 

  • Herrin E, Goforth T (1986) Phase analysis of Rayleigh waves from the Shagan River test site in the USSR. Bull Seismol Soc Am 76:1739–1754

    Google Scholar 

  • Hollingsworth J, Nazari H, Ritz J F, Salamati R, Talebian M, Bahroudi A, Walker RT, Rizza M, Jackson J (2010) Active tectonics of the east Alborz mountains, NE Iran: rupture of the left-lateral Astaneh fault system during the great 856 A.D. Qumis earthquake. J Geophys Res 115. doi: https://doi.org/10.1029/2009JB007185

  • Jackson J (1992) Partitioning of strike-slip and convergent motion between Eurasia and Arabia in eastern Turkey and the Caucasus. J Geophys Res 97:12471–12479

    Article  Google Scholar 

  • Jackson J, Mckenzie DP (1984) Active tectonics of the Alpine- Himalayan belt between western Turkey and Pakistan. Geophys J Roy Astr Soc 77:185–264

    Article  Google Scholar 

  • Jackson J, Priestley K, Allen M, Berberian M (2002) Active tectonics of the south Caspian basin. Geophys J Int 148:214–245

    Google Scholar 

  • Keilis-Borok VI (ed) (1986) Seismic surface waves in a laterally inhomogeneous Earth. Klumer Academic Publishers, Boston

    Google Scholar 

  • Laske G, Masters G (1997) A global digital map of sediment thickness. Eos 78(631)

  • Levshin AL, Pisarenko VF, Pogrebinsky GA (1972) On a frequency-time analysis of oscillations. Ann Geophys 28:211–218

    Google Scholar 

  • Levshin AL, Ratnikova L, Berger J (1992) Peculiarities of surface wave propagation across central Eurasia. Bull Seismol Soc Am 82:2464–2493

    Google Scholar 

  • Lin F, Moschetti MP, Ritzwoller MH (2008) Surface wave tomography of the western United States from ambient seismic noise: Rayleigh and Love wave phase velocity maps. Geophys J Int 173:281–298. https://doi.org/10.1111/j.1365-246X.2008.03720.x

    Article  Google Scholar 

  • Lobkis OI, Weaver RL (2001) On the emergence of the Green’s function in the correlations of a diffuse field. J Acoust Soc Am 110:3011–3017

    Article  Google Scholar 

  • Mottaghi AA, Rezapour M, Korn M (2013) Ambient noise surface wave tomography of the Iranian Plateau. Geophys J Int 193:452–462

    Article  Google Scholar 

  • Nicolson H, Curtis A, Baptie B, Galetti E (2010) Seismic interferometry and ambient noise tomography in the British isles. Proc Geol Assoc 123:74–86

    Article  Google Scholar 

  • Panza GF, Calcagnile G (1974a) Comparison of the multimode surface wave response in structures with and without a low velocity channel (Part I: dip-slip sources on a vertical fault plane). Pageoph 112:583–596

    Article  Google Scholar 

  • Panza GF, Calcagnile G (1974b) Comparison of the multimode surface wave response in structures with and without a low-velocity channel (Part II: Dip-slip sources). Pageoph 112:1031–1043

    Article  Google Scholar 

  • Panza GF, Calcagnile G (1975) Comparison of the multimode surface wave response in structures with and without a low velocity channel (Part III: Strike-slip sources). Pageoph 113:661–671

    Article  Google Scholar 

  • Panza GF, Schwab FA, Knopoff L (1973) Multimode surface waves for selected focal mechanism. I. Dip-slip sources on a vertical fault plane. Geophys J R Astron Soc 34:265–278

    Article  Google Scholar 

  • Rahimi H, Hamzehloo H, Vaccari F, Panza GF (2014) Shear-wave velocity tomography of the lithosphere–asthenosphere system beneath the Iranian Plateau. Bull Seismol Soc Am 104(6):2782–2798. https://doi.org/10.1785/0120130319

    Article  Google Scholar 

  • Rieben H (1966) Geological observations on alluvial deposits in Northern Iran. Geological Survey of Iran Report 9

  • Roux P, Sabra KG, Gerstoft P, Kuperman WA, Fehler MC (2005) P-waves from cross-correlation of seismic noise. Geophys Res Lett 32:L19393. https://doi.org/10.1029/2005GL023803

    Article  Google Scholar 

  • Russell DW, Herrman RB, Hwang H (1988) Application of frequency-variable filters to surface wave amplitude analysis. Bull Seismol Soc Am 78:339–354

    Google Scholar 

  • Sabra KG, Gerstoft P, Roux P, Kuperman WA, Fehler MC (2005) Surface wave tomography from microseism in southern California. Geophys Res Lett 32:L14311. https://doi.org/10.1029/2005GL023155

    Article  Google Scholar 

  • Shapiro NM, Singh SK (1999) A systematic error in estimating surface wave group-velocity dispersion curves and a procedure for its correction. Bull Seism Soc Am 89:1138–1142

  • Shirzad T, Shomali ZH (2013) Shallow crustal structures of the Tehran basin in Iran resolved by ambient noise tomography. Geophys J Int 196:1162–1176. https://doi.org/10.1093/gji/ggt449

    Article  Google Scholar 

  • Shirzad T, Shomali ZH (2014) Shallow crustal radial anisotropy beneath the Tehran basin of Iran from seismic ambient noise tomography. Phys Earth Planet Inter 231:16–29

    Article  Google Scholar 

  • Snieder R (2004) Extracting the Green’s function from the correlation of coda waves: a derivation based on stationary phase. Phys Rev E 69:046610

    Article  Google Scholar 

  • Sodoudi F, Yuan X, Kind R, Heit B, Sadidkhouy A (2009) Evidence for a missing crustal root and a thin lithosphere beneath the central Alborz by receiver function studies. Geophys J Int 177:733–742

    Article  Google Scholar 

  • Spetzler J, Trampert J, Snieder R (2002) The effects of scattering in surface wave tomography. Geophys J Int 149:755–767

    Article  Google Scholar 

  • Tatar M, Jackson J, Hatzfeld D, Bergman E (2007) The 2004 May 28 Baladeh earthquake (Mw 6.2) in the Alborz, Iran: over thrusting the south Caspian basin margin, partitioning of oblique convergence and the seismic hazard of Tehran. Geophys J Int 170:249–261

    Article  Google Scholar 

  • Vernant P, Nilforoushan F, Hatzfeld D, Abbassi MR, Vigny C, Masson F, Nankali H, Martinod J, Ashtiani A, Bayer R, Tavakoli F, Chery J (2004) Present-day crustal deformation and plate kinematics in the Middle East constrained by GPS measurements in Iran and northern Oman. Geophys J Int 157:381–398

    Article  Google Scholar 

  • Yang Y, Ritzwoller MH, Levshin AL, Shapiro NM (2007) Ambient noise Rayleigh wave tomography across Europe. Geophys J Int 168:259–274

    Article  Google Scholar 

  • Yanovskaya TB (1997) Resolution estimation in the problems of seismic ray tomography. Izvestiya, Phys Solid Earth 33(9):762–765

    Google Scholar 

  • Yanovskaya TB (2000) Development of methods for surface wave tomography based on the Backus-Gilbert approach. Comput Seismol Geodyn 7:5–16

    Google Scholar 

  • Yanovskaya TB, Ditmar PG (1990) Smoothness criteria in surface wave tomography. Geophys J Int 102:63–72

    Article  Google Scholar 

  • Yanovskaya TB, Kizima ES, Antonova LM (1998) Structure of the crust in the Black Sea and adjoining regions from surface wave data. J Seismol 2:303–316

    Article  Google Scholar 

  • Yoshizawa K, Kennett BLN (2002) Determination of the influence zone for surface wave paths. Geophys J Int 149:440–453

    Article  Google Scholar 

  • Zanchi A, Berra F, Mattei M, Ghasemi MR, Sabouri J (2006) Inversion tectonics in central Alborz, Iran. J Struct Geol 28:2023–2037

    Article  Google Scholar 

  • Zhou Y, Dahlen FA, Nolet G (2004) Three-dimensional sensitivity kernels for surface wave observables. Geophys J Int 158:142–168

    Article  Google Scholar 

Download references

Acknowledgements

The authors are thankful to the International Institute of Earthquake Engineering and Seismology (IIEES) for providing us with the database for this study.

Funding

The article is supported by the Iranian National Science Foundation (Grant Number 92008225).

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Authors and Affiliations

  1. Institute of Geophysics, University of Tehran, Tehran, Iran

    Mohsen Beygi Nya, Habib Rahimi & Hooshmand Zandi

Authors
  1. Mohsen Beygi Nya
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  2. Habib Rahimi
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  3. Hooshmand Zandi
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Corresponding author

Correspondence to Habib Rahimi.

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The authors declare that they have no competing interests.

Additional information

Responsible Editor: Narasimman Sundararajan

Highlights

Ambient noise tomography was used to construct the 2D group velocity maps of the north-central part of Iran.

The dense path coverage permits to produce images that have substantially higher lateral resolution than is currently available from global and regional group velocity studies.

Tomographic maps at high frequencies are well correlated with the upper crust structure and especially with sediments layers thickness.

Low- and high-velocity anomalies are observed that are consistent with the previous studies. These anomalies clearly show the major geological structures in the Alborz.

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Beygi Nya, M., Rahimi, H. & Zandi, H. Seismic interferometry ambient noise tomography—a study in the north-central part of Iran. Arab J Geosci 14, 408 (2021). https://doi.org/10.1007/s12517-021-06655-w

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