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Coda Q estimation for Kinnaur region and surrounding part of NW Himalaya

  • Naresh KumarEmail author
  • Dhirendra Nath Yadav
ORIGINAL ARTICLE
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Abstract

Spatial variation of coda wave attenuation is obtained for the Kinnaur Himalaya using the single backscattering model based on the data of 376 local earthquakes ranging in magnitude from 1.5 to 4.5. A frequency-dependent S-coda wave quality factor, Qc = 69f 1.0 (Qc = Q0f n), is obtained at eight central frequencies between 1.5 and 24 Hz for epicenter distance ≤ 30 km. The “n” values are found to vary highly, maximum in the tectonically and seismically active High Himalaya, intermediate in the seismically active Kaurik-Chango region, and least in the Spiti valley. Q0 (Qc at 1 Hz) is high in the High Himalaya, with values ranging from 87 to 109 which matches with already published works. It decreases towards NNE, the value is lowest in the Tethys Himalaya which varies between 49 and 55. To investigate attenuation with increasing depth, the Qc is estimated at eight coda wave window lengths between 20 and 90 s. With increasing window length, equivalent to increasing lapse times, the Q0 increases from 46 ± 3 to 493 ± 34 and n value decreases from 1.07 to 0.58. Further by dividing the entire coda wave data into four groups of epicenter distances, i.e., 0–25, 26–50, 51–75, and 76–100 km, Qc relations are estimated to vary as 111f 0.93, 183f 0.80, 264f 0.73, and 296f 0.71, respectively, for four groups. The increase of Qc with increasing lapse time is interpreted as a decrease of heterogeneity with depth. The data is reasonably fit in the power-law decay of turbidity.

Keywords

Quality factor Coda wave Kinnaur Himalaya Lapse time Heterogeneity 

Notes

Acknowledgments

We are thankful to Director WIHG, Dehradun, for giving permission to publish this work. Mr. Chandan Bora is thanked for executing the station installation and data collection; Monika Wadhwan is thanked for assisting in analyzing data. We thank the supporting staff of WIHG for helping to collect the seismic data from Kinnaur seismic network. The authors thank Prof. B.R. Arora for fruitful discussions and valuable suggestions. NK thanks European Commision for Marie Curie fellowship and International Centre for Theoretical Physics (ICTP), Trieste, Italy for Regular Associate fellowship. Editor and anonymous reviewer are thanked for constructive suggestions and modifications.

References

  1. Aki K (1969) Analysis of the seismic coda of local earthquakes as scattered waves. J Geophys Res 74:615–631CrossRefGoogle Scholar
  2. Aki K, Chouet B (1975) Origin of the coda waves: source, attenuation and scattering effects. J Geophys Res 80:3322–3342CrossRefGoogle Scholar
  3. Akinci A, Taktak AG, Ergintav S (1994) Attenuation of coda waves in Western Anatolia. Phys Earth Planet Inter 87:155–165CrossRefGoogle Scholar
  4. Akinci A, Ibáñez JM, Del Pezzo E, Morales J (1995) Geometrical spreading and attenuation of Lg waves: a comparison between Western Anatolia (Turkey) and southern Spain. Tectonophysics 250:47–50CrossRefGoogle Scholar
  5. Akinci A, Malagnini L, Herrmann RB, Kalafat D (2014) High frequency attenuation in the Lake Van region, eastern Turkey. Bull Seismol Soc Am 104:1400–1409CrossRefGoogle Scholar
  6. Ashish, Padhi A, Rai SS, Gupta S (2009) Seismological evidence for shallow crustal melt beneath the Garhwal High Himalaya, India: implications for the Himalayan channel flow. Geophys J Int 177:1111–1120CrossRefGoogle Scholar
  7. Banerjee P, Bürgmann R, Nagarajan B, Apel E (2008) Intraplate deformation of the Indian subcontinent. Geophys Res Lett 35:L18301CrossRefGoogle Scholar
  8. Banghar AR (1976) Mechanism solution of Kinnaur (Himachal Pradesh, India) earthquake of January 19, 1975. Tectonophysics 31:T5–T11CrossRefGoogle Scholar
  9. Barros LB, Assumpcao M, Quintero R, Ferreira VM (2011) Coda wave attenuation in the Parecis Basin, Amazon craton, Brazil: sensitivity to basement depth. J Seismol 15:391–409CrossRefGoogle Scholar
  10. Baruah S, Hazarika D, Kalita A, Goswami S (2010) Intrinsic and scattering attenuation in Chedrang fault and its vicinity—the rupture area of great Assam earthquake of 12 June 1897 (M=8.7). Curr Sci 99(6):775–784Google Scholar
  11. Beaumont C, Jamieson RA, Nguyen MH, Lee B (2001) Himalayan tectonics explained by extrusion of a low-viscosity crustal channel coupled to focused surface denudation. Nature 414(6865):738–742CrossRefGoogle Scholar
  12. Burchfiel BD, Zhiliang C, Hodges KV et al (1992) The South Tibetan detachment system, Himalayan orogen: extension contemporaneous with and parallel to shortening in a collisional mountain belt. Geol Soc Am Spec Pap 269:1–41Google Scholar
  13. Caldwell WB, Klemperer SL, Rai SS, Lawrence JF (2009) Partial melt in the upper-middle crust of the northwest Himalaya revealed by Rayleigh wave dispersion. Tectonophysics 477:58–65CrossRefGoogle Scholar
  14. Canas JA, Pujades LG, Blanco MJ, Soler V, Carracedo JC (1995) Coda-Q distribution in the Canary Islands. Tectonophy 246(4):245–261CrossRefGoogle Scholar
  15. Dubey AK (2014) Understanding an orogenic belt: structural evolution of the Himalaya, Vol 401. Springer, Berlin.  https://doi.org/10.1007/978-3-319-05588-6. CrossRefGoogle Scholar
  16. Epard JL, Steck A (2004) The eastern prolongation of the Zanskar shear zone (western Himalaya). Eclogae Geol Helv 97:193–212CrossRefGoogle Scholar
  17. Escudero CR, Garcia-Millan N, Escalona-Alcazar F (2016) Attenuation of coda waves in Western Mexico using local seismicity. Bull Seismol Soc Am 106(6):2545–2557CrossRefGoogle Scholar
  18. Farrokhi M, Hamzehloo H, Rahimi H, Allamehzadeh M (2015) Estimation of coda-wave attenuation in the central and eastern Alborz, Iran. Bull Seismol Soc Am 105(3):1756–1767CrossRefGoogle Scholar
  19. Galluzzo D, La Rocca M, Margerin L, Del Pezzo E, Scarpa R (2015) Attenuation and velocity structure from diffuse coda waves: constraints from underground array data. Phys Earth Planet Inter 240:34–42CrossRefGoogle Scholar
  20. Gansser A (1964) Geology of the Himalayas. Wiley Interscience, New York 298 ppGoogle Scholar
  21. Gao LS, Biswas NN, Lee LC, Aki K (1983) Effects of multiple scattering on coda waves in three dimensional medium. Pure Appl Geophys 121:3–15CrossRefGoogle Scholar
  22. Garzanti E (1999) Stratigraphy and sedimentary history of the Nepal Tethys Himalaya passive margin. J Asian Earth Sci 17(5):805–827CrossRefGoogle Scholar
  23. Gholamzadeh A, Rahimi H, Yaminifard F (2014) Spatial and temporal variation of coda-wave attenuation in the Faryab region, southeast of the Sanandaj–Sirjan zone, using aftershocks of the Tiab earthquake of 28 February 2006. Bull Seismol Soc Am 104(1):529–539CrossRefGoogle Scholar
  24. Giampiccolo E, Tusa G, Langer H, Gresta S (2002) Attenuation in southeastern Sicily (Italy) by applying different coda methods. J Seismol 6:487–501CrossRefGoogle Scholar
  25. Gupta SC, Kumar A (2002) Seismic wave attenuation characteristics of three Indian regions: A comparative study. Curr Sci 88(4):407–413Google Scholar
  26. Gupta SC, Singh VN, Kumar A (1995) Attenuation of coda waves in the Garhwal Himalayas, India. Phys Earth Planet Inter 87:247–253CrossRefGoogle Scholar
  27. Gupta AK, Sutar AK, Chopra S, Kumar S, Rastogi BK (2012) Attenuation characteristic of coda waves in Mainland Gujarat (India). Tectonophysics 530-531:264–271CrossRefGoogle Scholar
  28. Gusev AA (1995) Vertical profile of turbidity and coda Q. Geophys J Int 123:665–672Google Scholar
  29. Havskov J, Ottemoller L (2003) SEASAN: The earthquake analysis software for Windows, Solaris and Linux, Version 8.0. Institute of Solid Earth Physics, University of Bergen, NorwayGoogle Scholar
  30. Havskov J, Malone S, McCloug D, Crosson R (1989) Coda Q for the state of Washington. Bull Seismol Soc Am 79:1024–1038Google Scholar
  31. Havskov J, Sørensen MB, Vales D, Özyazıcıoğlu M, Sánchez G, Li B (2016) Coda Q in different tectonic areas, influence of processing parameters. Bull Seismol Soc Am 106:956–970CrossRefGoogle Scholar
  32. Hazarika D, Sen K, Kumar N (2014) Characterizing the intracrustal low velocity zone beneath Northwest India-Asia collision zone. Geophys J Int 199:1338–1353CrossRefGoogle Scholar
  33. Hodges KV (2016) Crustal decoupling in collisional orogenesis: examples from the East Greenland Caledonides and Himalaya. Annu Rev Earth Planet Sci 44:685–708CrossRefGoogle Scholar
  34. Jain SK, Gupta SC, Kumar A (2015) Attenuation of coda waves in the Garhwal Lesser Himalaya India. J Seismol 19:355–369CrossRefGoogle Scholar
  35. Jin A, Aki K (1988) Spatial and temporal correlation between coda Q and seismicity in China. Bull Seismol Soc Am 78:741–769Google Scholar
  36. Jin A, Aki K (1989) Spatial and temporal correlation between coda Q−1 and seismicity and its physical mechanism. J Geophys Res 94:14041–14059CrossRefGoogle Scholar
  37. Kayal JR (2001) Microearthquake activity in some parts of the Himalaya and the tectonic model. Tectonophysics 339:331–351CrossRefGoogle Scholar
  38. Khattri K, Rai K, Jain AK, Sinvhal H, Gaur VK, Mithal RS (1978) The Kinnaur earthquake, Himachal Pradesh, India, of 19 January, 1975. Tectonophysics 49:1–21CrossRefGoogle Scholar
  39. Klemperer SL, Kennedy BM, Sastry SR, Makovsky Y, Harinarayana T, Leech ML (2013) Mantle fluids in the Karakoram fault: helium isotope evidence. Earth Planet Sci Lett 366:59–70CrossRefGoogle Scholar
  40. Kumar N (2018) Crustal velocity structure and seismotectonic of Kinnaur region of NW Himalaya: new constraints based on micro-earthquake activity. J Geody (under review)Google Scholar
  41. Kumar N, Parvez IA, Virk HS (2005) Estimation of coda wave attenuation for NW Himalaya region using local earthquakes. Phys Earth Planet Inter 151:243–258CrossRefGoogle Scholar
  42. Kumar P, Yuan X, Kind R, Ni J (2006) Imaging the colliding Indian and Asian lithospheric plates beneath Tibet. J Geophys Res 111:B06308.  https://doi.org/10.1029/2005JB003930 CrossRefGoogle Scholar
  43. Kumar N, Sharma J, Arora BR, Mukhopadhyay S (2009) Seismotectonic model of the Kangra-Chamba sector of NW Himalaya: constraints from joint hypocenter determination and focal mechanism. Bull Seismol Soc Am 99(1):95–109CrossRefGoogle Scholar
  44. Kumar N, Arora BR, Mukhopadhyay S, Yadav DK (2013) Seismogenesis of clustered seismicity beneath the Kangra–Chamba sector of northwest Himalaya: constraints from 3D local earthquake tomography. J Asian Earth Sci 62:638–646CrossRefGoogle Scholar
  45. Kumar N, Mate S, Mukhopadhyay S (2014) Estimation of Qp and Qs of Kinnaur Himalaya. J Seismol 18:47–59CrossRefGoogle Scholar
  46. Kumar A, Sinvhal A, Joshi A, Kumar D, Kumar P (2015) Coda wave attenuation characteristics for Kumaon and Garhwal Himalaya. India. Nat Hazards 75:1057–1074CrossRefGoogle Scholar
  47. Le Fort P (1975) Himalayas: the colliding range, present knowledge of the continental arc. Am J Sci 275:1–44CrossRefGoogle Scholar
  48. Liu G, Einsele G (1994) Sedimentary history of the Tethyan basin in the Tibetan Himalayas. Int J Earth Sci 83(1):32–61Google Scholar
  49. Lorenzo SD, Pezzo ED, Bianco F (2013) Qc, Qβ, Qi and Qs attenuation parameters in the Umbria-Marche (Italy) region. Phys Earth Planet Inter 218:19–30CrossRefGoogle Scholar
  50. Mahood M (2014) Attenuation of high-frequency seismic waves in eastern Iran. Pure App Geophys 171:2225–2240Google Scholar
  51. Mahood M, Hamzehloo H (2009) Estimation of coda wave attenuation in east central Iran. J Seismol 13:125–139CrossRefGoogle Scholar
  52. Mandal P, Joshi SJ, Kumar S, Bhunia R, Rastogi BK (2004) Low coda Qc in the epicentral region of the 2001 Bhuj earthquake of Mw 7.7. Pure Appl Geophys 161:1635–1654CrossRefGoogle Scholar
  53. Mukhopadhyay S, Tyagi C (2007) Lapse time and frequency dependent attenuation characteristics of coda waves in the northwestern Himalayas. J Seismol 11(2):149–158CrossRefGoogle Scholar
  54. Mukhopadhyay S, Sharma J, Del-Pezzo E, Kumar N (2010) Study of attenuation mechanism for Garhwal-Kumaon Himalayas from analysis of coda of local earthquakes. Phys Earth Planet Inter 180:7–15CrossRefGoogle Scholar
  55. Najman Y, Johnson K, White N, Grahame O (2004) Evolution of the Himalayan foreland basin, NW India. Basin Res 16:1–24CrossRefGoogle Scholar
  56. Oreshin SI, Kiselev SG, Vinnik LP, Surya Prakasam K, Rai SS, Makeyeva L, Savvin Y (2008) Crust and mantle beneath western Himalaya, Ladakh and western Tibet from integrated seismic data. Earth Planet Sci Lett 271:75–87CrossRefGoogle Scholar
  57. Padhy S (2009) Inversion of seismogram envelopes using a multiple isotropic scattering model in Garhwal Himalaya. Bull Seismol Soc Am 99(2A):726–740CrossRefGoogle Scholar
  58. Parvez IA, Sutar AK, Mridula M, Mishra SK, Rai SS (2008) Coda Q estimates in the Andaman Islands using local earthquakes. Pure App Geophys 165:1861–1878CrossRefGoogle Scholar
  59. Paul A, Gupta SC, Pant CC (2003) Coda Q estimates for Kumaon Himalaya. Proc Ind Acad Sci (Earth Planet Sci) 112(4):569–576Google Scholar
  60. Pujades L, Canas JA, Egozcue JJ et al (1991) Coda Q distribution in the Iberian Peninsula. Geophys J Int 100:285–301CrossRefGoogle Scholar
  61. Pulli JJ (1984) Attenuation of coda waves in New England. Bull Seismol Soc Am 74:1149–1166Google Scholar
  62. Rahimi H, Hamzehloo H (2008) Lapse time and frequency-dependent attenuation of coda waves in the Zagros continental collision zone in southwestern Iran. J Geophys Eng 5(2):173–185CrossRefGoogle Scholar
  63. Rahimi H, Motaghi K, Mukhopadhyay S, Hamzehloo H (2010) Variation of coda wave attenuation in the Alborz region and central Iran. Geophys J Int 181(3):1643–1654Google Scholar
  64. Rai SS, Ashish A, Padhi A, Sarma PR (2009) High crustal seismic attenuation in Ladakh-Karakoram. Bull Seismol Soc Am 99:407–415CrossRefGoogle Scholar
  65. Rautian TG, Khalturin VI (1978) The use of coda for determination of the earthquake source spectrum. Bull Seismol Soc Am 68:923–948Google Scholar
  66. Rautian TG et al (1981) Experimental studies of seismic coda. Nauka, Moscow (in Russian)Google Scholar
  67. Sato H (1977) Energy propagation including scattering effect. J Phys Earth 25:27–41CrossRefGoogle Scholar
  68. Sato H (1988) Fractal interpretation of the linear relation between logarithms of maximum amplitude and hypocentral distance. Geophys Res Lett 15:373–375CrossRefGoogle Scholar
  69. Sato H, Fehler M (1998) Seismic wave propagation and scattering in the heterogeneous earth. AIP Press/Springer-Verlag, New York, pp 1–308Google Scholar
  70. Schelling D, Arita A (1991) Thrust tectonics, crustal shortening and the structure of the far-eastern Nepal Himalayas. Tectonics 10:851–862CrossRefGoogle Scholar
  71. Seeber A (1984) The geodynamic history of the Himalaya. In Zagros, Hindu Kush, Himalaya: Geodynamic Evolution, HK Gupta and FM Delany (Editors), Geodynamic Series, Vol. 3, American Geophysical Union, Washington, D.C., 111–121Google Scholar
  72. Sen K, Das S, Mukherjee BK, Sen K (2013) Bimodal stable isotope signatures of Zildat Ophiolitic M’elange, Indus Suture Zone, Himalaya: implications for emplacement of an ophiolitic m’elange in a convergent setup. Int J Earth Sci 102:2033–2042CrossRefGoogle Scholar
  73. Sertcelik F (2012) Estimation of coda wave attenuation in the East Anatolia Fault Zone Turkey. Pure Appl Geophys 169:1189–1204CrossRefGoogle Scholar
  74. Singh C, Bharathi VKS, Chadha RK (2012) Lapse time and frequency-dependent attenuation characteristics of Kumaun Himalaya. J Asian Earth Sci 54-55:64–71CrossRefGoogle Scholar
  75. Spudich P, Iida M (1993) The seismic coda, site effects and scattering in alluvial basins studied by using aftershocks of the 1986 North Palm Springs, California, earthquake as source array. Bull Seismol Soc Am 83:1721–1743Google Scholar
  76. Srivastava P, Ray Y, Phartiyal B, Sharma A (2013) Late Pleistocene-Holocene morphosedimentary architecture, Spiti River, arid higher Himalaya. Int J Earth Sci 102:1967–1984CrossRefGoogle Scholar
  77. Thakur VC (1992) Geology of Western Himalaya. Pregamon Press, Oxford 366 ppGoogle Scholar
  78. Thakur VC, Sriram V, Mundepi AK (2000) Seismotectonics of the great 1905 Kangra earthquake meizoseismal region in Kangra-Chamba, NW Himalaya. Tectonophysics 326:289–298CrossRefGoogle Scholar
  79. Thiede RC, Arrowsmith JR, Bookhagen B, McWilliams M, Sobel ER, Strecker MR (2006) Dome formation and extension in the Tethyan Himalaya, Leo Pargil, NW India. Geol Soc Am Bull 118:635–650CrossRefGoogle Scholar
  80. Tripathi JN, Singh P, Sharma ML (2012) Variation of seismic coda wave attenuation in the Garhwal region, northwestern Himalaya. Pure Appl Geophys 169:71–88CrossRefGoogle Scholar

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© Springer Nature B.V. 2019

Authors and Affiliations

  1. 1.Wadia Institute of Himalayan GeologyDehradunIndia
  2. 2.Atomic Mineral Directorate for Exploration and ResearchHyderabadIndia
  3. 3.Applied GeophysicsIndian Institute of Technology (3 ISM)DhanbadIndia

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