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Estimation of Coda Wave Attenuation in Northern Morocco

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Abstract

We studied the attenuation of coda waves and its frequency and lapse-time dependence in northern Morocco. We analysed coda waves of 66 earthquakes recorded in this region during 2008 for four lapse time windows of length 30, 40, 50, and 60 s, and at five frequency bands with central frequency in the range of 0.75–12 Hz. We determined the frequency dependent Q c relation for the horizontal (NS and EW) and vertical (Z) component seismograms. We analyzed three-component broadband seismograms of 66 local earthquakes for determining coda-Q based on the single back-scattering model. The Q c values show strong frequency dependence in 1.5–12 Hz that is related to high degree of heterogeneity of the medium. The lapse time dependence of Q c shows that Q 0 (Q c at 1 Hz) significantly increases with lapse time that is related to the depth dependence of attenuation and hence of the level of heterogeneity of the medium. The average frequency-dependent Q c(f) values are \(Q_{\text{c}} = (143.75 \pm 1.09)f^{(0.864 \pm 0.006)},\) \(Q_{\text{c}} = (149.12 \pm 1.08)f^{(0.85 \pm 0.005)}\) and \(Q_{\text{c}} = (140.42 \pm 1.81)f^{(0.902 \pm 0.004)}\) for the vertical, north–south and east–west components of motion, respectively. The frequency-dependent Q c(f) relations are useful for evaluating source parameters (Singh et al. 2001), which are the key inputs for seismic hazard assessment of the region.

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References

  • Aki, K. (1969). Analysis of the seismic coda of local earthquakes: source, attenuation and scattering effects. Journal of Geophysical Research, 74(2), 615–631.

    Article  Google Scholar 

  • Aki, K., & Chouet, B. (1975). Origin of coda waves: source, attenuation, and scattering effects. Journal of Geophysical Research, 80(23), 3322–3342.

    Article  Google Scholar 

  • Akinci, A., Taktak, A. G., & Ergintav, S. (1994). Attenuation of coda waves in Western Anatolia. Physics of the Earth and Planetary Interiors, 87(1–2), 155–165.

    Article  Google Scholar 

  • Badawy, A., & Morsy, M. A. (2012). Seismic Wave Attenuation in the Greater Cairo Region. Egypt. Pure and applied geophysics, 169(9), 1589–1600.

    Article  Google Scholar 

  • Biescas, B., Rivera, Z., & Zapata, J. A. (2007). Seismic attenuation of coda waves in the eastern region of Cuba. Tectonophysics, 429(1), 99–109.

    Article  Google Scholar 

  • Boulanouar, A., El Moudnib, L., Ford, S., Harnafi, M., Villasenor, A., Gallart, J., et al. (2016). Coda wave attenuation tomography in Northern Morocco. Journal of Materials and Environmental Science, 7(8), 2880–2885.

    Google Scholar 

  • Boulanouar, A., El Moudnib, L., Harnafi, M., Cherkaoui, T. E., Rahmouni, A., Boukalouch, M., et al. (2013). Spatial variation of coda wave attenuation using aftershocks of the Al Hoceima earthquake of 24 February, 2004. Morocco. Natural Science, 5(08), 72.

    Article  Google Scholar 

  • Cherkaoui, T. E., & El Hassani, A. (2012). Seismicity and seismic hazard in Morocco: 1901–2010. Bulletin de l’Institut Scientifique, Rabat, Section Sciences de la Terre, 34, 45–55.

    Google Scholar 

  • Cherkaoui, T. E., Hatzfeld, D., Jebli, H., Medina, F., & Caillot, V. (1990). Etude microsismique de la region d’Al Hoceima. Bulletin de l’Institut Scientifique, 14, 25–34.

    Google Scholar 

  • Del Pezzo, E., De Martino, S., De Miguel, F., Ibanez, J., & Sorgente, A. (1991). Characteristics of the seismic attenuation in two tectonically active zones of Southern Europe. Pure and Applied Geophysics, 135(1), 91–106.

    Article  Google Scholar 

  • Del Pezzo, E., De Natale, G., Scarcella, G., & Zollo, A. (1985). Qc of three component seismograms of volcanic microearthquakes at Campi Flegrei volcanic area—southern Italy. Pure and Applied Geophysics, 123(5), 683–696.

    Article  Google Scholar 

  • Del Pezzo, E., & Patané, D. (1992). Coda Q dependence on time, frequency and coda duration interval at Mt. Etna, Sicily. In E. Del Pezzo & D. Patanè (Eds.), Volcanic seismology (pp. 109–119). Heidelberg: Springer.

  • El Moudnib, L., Villaseñor, A., Harnafi, M., Gallart, J., Pazos, A., Serrano, L., et al. (2015). Crustal structure of the Betic-Rif system, western Mediterranean, from local earthquake tomography.Tectonophysics. Tectonophysics, 643, 94–105.

    Article  Google Scholar 

  • Fehler, M., Hoshiba, M., Sato, H., & Obara, K. (1992). Separation of scattering and intrinsic attenuation for the Kanto-Tokai region, Japan, using measurements of S-wave energy versus hypocentral distance. Geophysical Journal International, 108(3), 787–800.

    Article  Google Scholar 

  • Frankel, A., & Wennerberg, L. (1987). Energy-flux model of seismic coda: separation of scattering and intrinsic attenuation. Bulletin of the Seismological Society of America, 77(4), 1223–1251.

    Google Scholar 

  • Gao, L. S., Lee, L. C., Biswas, N. N., & Aki, K. (1983). Comparison of the effects between single and multiple scattering on coda waves for local earthquakes. Bulletin of the Seismological Society of America, 73(2), 377–389.

    Google Scholar 

  • Giampiccolo, E., Tusa, G., Langer, H., & Gresta, S. (2002). Attenuation in southeastern Sicily (Italy) by applying different coda methods. Journal of Seismology, 6(4), 487–501.

    Article  Google Scholar 

  • Gupta, S. C., Teotia, S. S., Rai, S. S., & Gautam, N. (1998). Coda Q estimates in the Koyna region, India. Pure and Applied Geophysics, 153(2–4), 713.

    Article  Google Scholar 

  • Havskov, J., Malone, S., McClurg, D., & Crosson, R. (1989). Coda Q for the state of Washington. Bulletin of the Seismological Society of America, 79(4), 1024–1038.

    Google Scholar 

  • Havskov, J., Ottemoller, L. (2003). SEISAN: the earthquake analysis software for windows, Solaris, Linux, and Mac OSX Version 8.0. http://www.geo.uib.no/Seismologi/SOFTWARE/. Accessed 4 March 2014.

  • Hoshiba, M. (1997). Seismic coda wave envelope in depth-dependent S wave velocity structure. Physics of the Earth and Planetary Interiors, 104(1–3), 15–22.

    Article  Google Scholar 

  • Ibanez, J. M., Del Pezzo, E., De Miguel, F., Herraiz, M., Alguacil, G., & Morales, J. (1990). Depth-dependent seismic attenuation in the Granada zone (Southern Spain). Bulletin of the Seismological Society of America, 80(5), 1232–1244.

    Google Scholar 

  • Inmaculada, S., Dapeng, Z., José, M., & Federico, T. (2003). Seismic tomography from local crustal earthquakes beneath eastern Rif Mountains of Morocco. Tectonophysics. https://doi.org/10.1016/S0040-1951(03)00100-8.

    Google Scholar 

  • Khattach, D., Houari, M. R., Corchete, V., Chourak, M., El Gout, R., & Ghazala, H. (2013). Main crustal discontinuities of Morocco derived from gravity data. Journal of Geodynamics, 68, 37–48.

    Article  Google Scholar 

  • Kopnichev, Y. (1977). The role of multiple scattering in the formation of a seismogram’s tail. Izvestiya, Earth Phys., 13, 394–398.

    Google Scholar 

  • Kumar, N., Parvez, I. A., & Virk, H. S. (2005). Estimation of coda wave attenuation for NW Himalayan region using local earthquakes. Physics of the Earth and Planetary Interiors, 151(3), 243–258.

    Article  Google Scholar 

  • Lee, W. S. (1999). Q estimates using the coda waves in the Kyeongsang Basin. Thesis for an M.S. Degree. Department of Geological Science: Graduate School Seoul National University.

  • Li, B. J., Qin, J. Z., Qian, X. D., & Ye, J. Q. (2004). The coda attenuation of the Yao’an area in Yunnan Province. Acta Seismologica Sinica, 17(1), 47–53.

    Article  Google Scholar 

  • Ma’hood, M., & Hamzehloo, H. (2009). Estimation of coda wave attenuation in East Central Iran. Journal of Seismology, 13(1), 125–139.

    Article  Google Scholar 

  • Mamdouh, A. M., El Hady, S., Mahmoud, S. M., & Awad, E. A. M. (2013). Lateral variations of coda Q and attenuation of seismic waves in the Gulf of Suez. Egypt. Arabian Journal of Geosciences, 6(1), 1–11.

    Article  Google Scholar 

  • Margerin, L., Campillo, M., & Tiggelen, B. (1998). Radiative transfer and diffusion of waves in a layered medium: new insight into coda Q. Geophysical Journal International, 134(2), 596–612.

    Article  Google Scholar 

  • Masahiro, K. (1992). Dependence of coda Q on frequency and lapse time. Journal of Physics of the Earth, 40(2), 421–445.

    Article  Google Scholar 

  • Mayeda, K., Koyanagi, S., Hoshiba, M., Aki, K., & Zeng, Y. (1992). A comparative study of scattering, intrinsic, and coda Q—1 for Hawaii, Long Valley, and central California between 1.5 and 15.0 Hz. Journal of Geophysical Research: Solid. Earth, 97(B5), 6643–6659.

    Google Scholar 

  • Medina, F., & El Alami, S. O. (2006). Focal mechanisms and state of stress in the Al Hoceima area (Central Rif, Morocco). Bulletin de l’Institut Scientifique, Rabat, 28, 19–30.

    Google Scholar 

  • Mukhopadhyay, S., & Tyagi, C. (2007). Lapse time and frequency-dependent attenuation characteristics of coda waves in the Northwestern Himalayas. Journal of Seismology, 11(2), 149–158.

    Article  Google Scholar 

  • Padhy, S., & Subhadra, N. (2010). Attenuation of high-frequency seismic waves in northeast India. Geophysical Journal International, 181(1), 453–467.

    Article  Google Scholar 

  • Parvez, I. A., Sutar, A. K., Mridula, M., Mishra, S. K., & Rai, S. S. (2008). Coda Q estimates in the Andaman Islands using local earthquakes. Pure and Applied Geophysics, 165(9), 1861–1878.

    Article  Google Scholar 

  • Phillips, W. S., & Aki, K. (1986). Site amplification of coda waves from local earthquakes in central California. Bulletin of the Seismological Society of America, 76(3), 627–648.

    Google Scholar 

  • Pujades, L. G., Canas, J. A., Egozcue, J. J., Puigvi, M. A., Gallart, J., Lana, X., et al. (1990). Coda-Q distribution in the Iberian Peninsula. Geophysical Journal International, 100(2), 285–301.

    Article  Google Scholar 

  • Pulli, J. J. (1984). Attenuation of coda waves in New England. Bulletin of the Seismological Society of America, 74(4), 1149–1166.

    Google Scholar 

  • Rahimi, H., & Hamzehloo, H. (2008). Lapse time and frequency-dependent attenuation of coda waves in the Zagros continental collision zone in Southwestern Iran. Journal of Geophysics and Engineering, 5(2), 173.

    Article  Google Scholar 

  • Rautian, T. G., & Khalturin, V. I. (1978). The use of the coda for determination of the earthquake source spectrum. Bulletin of the Seismological Society of America, 68(4), 923–948.

    Google Scholar 

  • Sato, H., Fehler, M. C., & Maeda, T. (2012). Seismic wave propagation and scattering in the heterogeneous earth (Vol. 496). Berlin: Springer.

    Book  Google Scholar 

  • Singh, D. D., Govoni, A., & Bragato, P. L. (2001). Coda Qc attenuation and source parameter analysis in Friuli (NE Italy) and its vicinity. Pure and Applied Geophysics, 158(9–10), 1737–1761.

    Google Scholar 

  • Singh, S., & Herrmann, R. B. (1983). Regionalization of crustal coda Q in the continental United States. Journal of Geophysical Research: Solid Earth, 88(B1), 527–538.

    Article  Google Scholar 

  • Steck, L. K., Prothero, W. A., & Scheimer, J. (1989). Site-dependent Coda Q at mono craters, California. Bulletin of the Seismological Society of America, 79(5), 1559–1574.

    Google Scholar 

  • Timoulali, Y., Hahou, Y., Jabour, N., Merrouch, R., & El Kharrim, A. (2014). Main features of the deep structure by local earthquake tomography and active tectonics: case of Rif Mountain (morocco) and Betic Cordillera (Spain). Journal of Seismology, 18(2), 221–234.

    Article  Google Scholar 

  • Tuvè, T., Bianco, F., Ibáñez, J., Patanè, D., Del Pezzo, E., & Bottari, A. (2006). Attenuation study in the Straits of Messina area (southern Italy). Tectonophysics, 421(3), 173–185.

    Article  Google Scholar 

  • Wennerberg, L. (1993). Multiple-scattering interpretations of coda-Q measurements. Bulletin of the Seismological Society of America, 83(1), 279–290.

    Google Scholar 

  • Wessel, P., & Smith, W. H. (1998). New, improved version of generic map** tools released. Eos, Transactions American Geophysical Union, 79(47), 579.

    Article  Google Scholar 

  • Woodgold, C. R. D. (1994). Coda Q in the Charlevoix, Quebec, region: lapse-time dependence and spatial and temporal comparisons. Bulletin of the Seismological Society of America, 84(4), 1123–1131.

    Google Scholar 

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Acknowledgements

We sincerely thank the anonymous reviewers and the Editor Professor Ruben Tatevossian for their constructive comments that improved the quality of the paper. We thank the Scientific Institute of Rabat/Morocco for providing the data used in this study. Some of the figures were produced using the Generic Map** Tools software (Wessel and Smith 1998).

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Correspondence to Abderrahim Boulanouar.

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Boulanouar, A., Moudnib, L.E., Padhy, S. et al. Estimation of Coda Wave Attenuation in Northern Morocco. Pure Appl. Geophys. 175, 883–897 (2018). https://doi.org/10.1007/s00024-017-1726-4

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