Coda Q in Eastern Indian shield
Abstract We have analyzed 16 earthquake waveform data recorded during the period from 2006 to 2013 at broadband station lying at the premises of Indian School of Mines, Dhanbad in the Eastern Indian Shield region. Coda window lengths of 30, 40 and 50 s were selected after thorough analysis of the wa...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Khan, Prosanta K. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Schlagwörter: |
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| Anmerkung: |
© Akadémiai Kiadó 2015 |
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| Übergeordnetes Werk: |
Enthalten in: Acta geodaetica et geophysica Hungarica - Budapest : Akad. Kiadó, 1997, 51(2015), 2 vom: 05. Juli, Seite 333-346 |
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| Übergeordnetes Werk: |
volume:51 ; year:2015 ; number:2 ; day:05 ; month:07 ; pages:333-346 |
| Links: |
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| DOI / URN: |
10.1007/s40328-015-0129-1 |
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SPR037151355 |
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| 520 | |a Abstract We have analyzed 16 earthquake waveform data recorded during the period from 2006 to 2013 at broadband station lying at the premises of Indian School of Mines, Dhanbad in the Eastern Indian Shield region. Coda window lengths of 30, 40 and 50 s were selected after thorough analysis of the waveforms. The Coda Q ($ Q_{c} $) values were computed using single back scattered method. The earthquakes parameters were compiled from catalogue of Indian Meteorological Department (Nodal agency under Govt. of India for record keeping and data sharing), New Delhi. The estimated average $ Q_{c} $ values for three coda windows 30, 40 and 50 s are $ Q_{c} $ = 259.$ 1f^{0.808} $, $ Q_{c} $ = 275.$ 9f^{0.764} $ and $ Q_{c} $ = 397.$ 1f^{0.651} $, respectively. The average $ Q_{c} $ value estimated from the $ Q_{c} $ values for the time windows 30, 40 and 50 s is found to be $ Q_{c} $ = 313.$ 2f^{0.73} $. Thus, the attenuation follows the power law relationships (e.g., $ Q_{c} $ = $ Q_{0} %$ f^{n} $), and the moderate to higher values of frequency parameters (n) obviously show that the $ Q_{c} $ value is a strong function of frequency. The increasing values of $ Q_{0} $ with increasing lapse time indicating the depth dependency of attenuation, and accounts for decreasing heterogeneity towards deeper level beneath the study area. | ||
| 650 | 4 | |a Attenuation of coda waves |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Single back scattering method |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Coda Q |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Lapse time |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Eastern India Shield |7 (dpeaa)DE-He213 | |
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| 700 | 1 | |a Tarafder, Gaurab |4 aut | |
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10.1007/s40328-015-0129-1 doi (DE-627)SPR037151355 (SPR)s40328-015-0129-1-e DE-627 ger DE-627 rakwb eng Khan, Prosanta K. verfasserin aut Coda Q in Eastern Indian shield 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Akadémiai Kiadó 2015 Abstract We have analyzed 16 earthquake waveform data recorded during the period from 2006 to 2013 at broadband station lying at the premises of Indian School of Mines, Dhanbad in the Eastern Indian Shield region. Coda window lengths of 30, 40 and 50 s were selected after thorough analysis of the waveforms. The Coda Q ($ Q_{c} $) values were computed using single back scattered method. The earthquakes parameters were compiled from catalogue of Indian Meteorological Department (Nodal agency under Govt. of India for record keeping and data sharing), New Delhi. The estimated average $ Q_{c} $ values for three coda windows 30, 40 and 50 s are $ Q_{c} $ = 259.$ 1f^{0.808} $, $ Q_{c} $ = 275.$ 9f^{0.764} $ and $ Q_{c} $ = 397.$ 1f^{0.651} $, respectively. The average $ Q_{c} $ value estimated from the $ Q_{c} $ values for the time windows 30, 40 and 50 s is found to be $ Q_{c} $ = 313.$ 2f^{0.73} $. Thus, the attenuation follows the power law relationships (e.g., $ Q_{c} $ = $ Q_{0} %$ f^{n} $), and the moderate to higher values of frequency parameters (n) obviously show that the $ Q_{c} $ value is a strong function of frequency. The increasing values of $ Q_{0} $ with increasing lapse time indicating the depth dependency of attenuation, and accounts for decreasing heterogeneity towards deeper level beneath the study area. Attenuation of coda waves (dpeaa)DE-He213 Single back scattering method (dpeaa)DE-He213 Coda Q (dpeaa)DE-He213 Lapse time (dpeaa)DE-He213 Eastern India Shield (dpeaa)DE-He213 Bhukta, Kuntal aut Tarafder, Gaurab aut Enthalten in Acta geodaetica et geophysica Hungarica Budapest : Akad. Kiadó, 1997 51(2015), 2 vom: 05. Juli, Seite 333-346 (DE-627)364470852 (DE-600)2110468-2 1587-1037 nnns volume:51 year:2015 number:2 day:05 month:07 pages:333-346 https://dx.doi.org/10.1007/s40328-015-0129-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 51 2015 2 05 07 333-346 |
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10.1007/s40328-015-0129-1 doi (DE-627)SPR037151355 (SPR)s40328-015-0129-1-e DE-627 ger DE-627 rakwb eng Khan, Prosanta K. verfasserin aut Coda Q in Eastern Indian shield 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Akadémiai Kiadó 2015 Abstract We have analyzed 16 earthquake waveform data recorded during the period from 2006 to 2013 at broadband station lying at the premises of Indian School of Mines, Dhanbad in the Eastern Indian Shield region. Coda window lengths of 30, 40 and 50 s were selected after thorough analysis of the waveforms. The Coda Q ($ Q_{c} $) values were computed using single back scattered method. The earthquakes parameters were compiled from catalogue of Indian Meteorological Department (Nodal agency under Govt. of India for record keeping and data sharing), New Delhi. The estimated average $ Q_{c} $ values for three coda windows 30, 40 and 50 s are $ Q_{c} $ = 259.$ 1f^{0.808} $, $ Q_{c} $ = 275.$ 9f^{0.764} $ and $ Q_{c} $ = 397.$ 1f^{0.651} $, respectively. The average $ Q_{c} $ value estimated from the $ Q_{c} $ values for the time windows 30, 40 and 50 s is found to be $ Q_{c} $ = 313.$ 2f^{0.73} $. Thus, the attenuation follows the power law relationships (e.g., $ Q_{c} $ = $ Q_{0} %$ f^{n} $), and the moderate to higher values of frequency parameters (n) obviously show that the $ Q_{c} $ value is a strong function of frequency. The increasing values of $ Q_{0} $ with increasing lapse time indicating the depth dependency of attenuation, and accounts for decreasing heterogeneity towards deeper level beneath the study area. Attenuation of coda waves (dpeaa)DE-He213 Single back scattering method (dpeaa)DE-He213 Coda Q (dpeaa)DE-He213 Lapse time (dpeaa)DE-He213 Eastern India Shield (dpeaa)DE-He213 Bhukta, Kuntal aut Tarafder, Gaurab aut Enthalten in Acta geodaetica et geophysica Hungarica Budapest : Akad. Kiadó, 1997 51(2015), 2 vom: 05. Juli, Seite 333-346 (DE-627)364470852 (DE-600)2110468-2 1587-1037 nnns volume:51 year:2015 number:2 day:05 month:07 pages:333-346 https://dx.doi.org/10.1007/s40328-015-0129-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 51 2015 2 05 07 333-346 |
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10.1007/s40328-015-0129-1 doi (DE-627)SPR037151355 (SPR)s40328-015-0129-1-e DE-627 ger DE-627 rakwb eng Khan, Prosanta K. verfasserin aut Coda Q in Eastern Indian shield 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Akadémiai Kiadó 2015 Abstract We have analyzed 16 earthquake waveform data recorded during the period from 2006 to 2013 at broadband station lying at the premises of Indian School of Mines, Dhanbad in the Eastern Indian Shield region. Coda window lengths of 30, 40 and 50 s were selected after thorough analysis of the waveforms. The Coda Q ($ Q_{c} $) values were computed using single back scattered method. The earthquakes parameters were compiled from catalogue of Indian Meteorological Department (Nodal agency under Govt. of India for record keeping and data sharing), New Delhi. The estimated average $ Q_{c} $ values for three coda windows 30, 40 and 50 s are $ Q_{c} $ = 259.$ 1f^{0.808} $, $ Q_{c} $ = 275.$ 9f^{0.764} $ and $ Q_{c} $ = 397.$ 1f^{0.651} $, respectively. The average $ Q_{c} $ value estimated from the $ Q_{c} $ values for the time windows 30, 40 and 50 s is found to be $ Q_{c} $ = 313.$ 2f^{0.73} $. Thus, the attenuation follows the power law relationships (e.g., $ Q_{c} $ = $ Q_{0} %$ f^{n} $), and the moderate to higher values of frequency parameters (n) obviously show that the $ Q_{c} $ value is a strong function of frequency. The increasing values of $ Q_{0} $ with increasing lapse time indicating the depth dependency of attenuation, and accounts for decreasing heterogeneity towards deeper level beneath the study area. Attenuation of coda waves (dpeaa)DE-He213 Single back scattering method (dpeaa)DE-He213 Coda Q (dpeaa)DE-He213 Lapse time (dpeaa)DE-He213 Eastern India Shield (dpeaa)DE-He213 Bhukta, Kuntal aut Tarafder, Gaurab aut Enthalten in Acta geodaetica et geophysica Hungarica Budapest : Akad. Kiadó, 1997 51(2015), 2 vom: 05. Juli, Seite 333-346 (DE-627)364470852 (DE-600)2110468-2 1587-1037 nnns volume:51 year:2015 number:2 day:05 month:07 pages:333-346 https://dx.doi.org/10.1007/s40328-015-0129-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 51 2015 2 05 07 333-346 |
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10.1007/s40328-015-0129-1 doi (DE-627)SPR037151355 (SPR)s40328-015-0129-1-e DE-627 ger DE-627 rakwb eng Khan, Prosanta K. verfasserin aut Coda Q in Eastern Indian shield 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Akadémiai Kiadó 2015 Abstract We have analyzed 16 earthquake waveform data recorded during the period from 2006 to 2013 at broadband station lying at the premises of Indian School of Mines, Dhanbad in the Eastern Indian Shield region. Coda window lengths of 30, 40 and 50 s were selected after thorough analysis of the waveforms. The Coda Q ($ Q_{c} $) values were computed using single back scattered method. The earthquakes parameters were compiled from catalogue of Indian Meteorological Department (Nodal agency under Govt. of India for record keeping and data sharing), New Delhi. The estimated average $ Q_{c} $ values for three coda windows 30, 40 and 50 s are $ Q_{c} $ = 259.$ 1f^{0.808} $, $ Q_{c} $ = 275.$ 9f^{0.764} $ and $ Q_{c} $ = 397.$ 1f^{0.651} $, respectively. The average $ Q_{c} $ value estimated from the $ Q_{c} $ values for the time windows 30, 40 and 50 s is found to be $ Q_{c} $ = 313.$ 2f^{0.73} $. Thus, the attenuation follows the power law relationships (e.g., $ Q_{c} $ = $ Q_{0} %$ f^{n} $), and the moderate to higher values of frequency parameters (n) obviously show that the $ Q_{c} $ value is a strong function of frequency. The increasing values of $ Q_{0} $ with increasing lapse time indicating the depth dependency of attenuation, and accounts for decreasing heterogeneity towards deeper level beneath the study area. Attenuation of coda waves (dpeaa)DE-He213 Single back scattering method (dpeaa)DE-He213 Coda Q (dpeaa)DE-He213 Lapse time (dpeaa)DE-He213 Eastern India Shield (dpeaa)DE-He213 Bhukta, Kuntal aut Tarafder, Gaurab aut Enthalten in Acta geodaetica et geophysica Hungarica Budapest : Akad. Kiadó, 1997 51(2015), 2 vom: 05. Juli, Seite 333-346 (DE-627)364470852 (DE-600)2110468-2 1587-1037 nnns volume:51 year:2015 number:2 day:05 month:07 pages:333-346 https://dx.doi.org/10.1007/s40328-015-0129-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 51 2015 2 05 07 333-346 |
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10.1007/s40328-015-0129-1 doi (DE-627)SPR037151355 (SPR)s40328-015-0129-1-e DE-627 ger DE-627 rakwb eng Khan, Prosanta K. verfasserin aut Coda Q in Eastern Indian shield 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Akadémiai Kiadó 2015 Abstract We have analyzed 16 earthquake waveform data recorded during the period from 2006 to 2013 at broadband station lying at the premises of Indian School of Mines, Dhanbad in the Eastern Indian Shield region. Coda window lengths of 30, 40 and 50 s were selected after thorough analysis of the waveforms. The Coda Q ($ Q_{c} $) values were computed using single back scattered method. The earthquakes parameters were compiled from catalogue of Indian Meteorological Department (Nodal agency under Govt. of India for record keeping and data sharing), New Delhi. The estimated average $ Q_{c} $ values for three coda windows 30, 40 and 50 s are $ Q_{c} $ = 259.$ 1f^{0.808} $, $ Q_{c} $ = 275.$ 9f^{0.764} $ and $ Q_{c} $ = 397.$ 1f^{0.651} $, respectively. The average $ Q_{c} $ value estimated from the $ Q_{c} $ values for the time windows 30, 40 and 50 s is found to be $ Q_{c} $ = 313.$ 2f^{0.73} $. Thus, the attenuation follows the power law relationships (e.g., $ Q_{c} $ = $ Q_{0} %$ f^{n} $), and the moderate to higher values of frequency parameters (n) obviously show that the $ Q_{c} $ value is a strong function of frequency. The increasing values of $ Q_{0} $ with increasing lapse time indicating the depth dependency of attenuation, and accounts for decreasing heterogeneity towards deeper level beneath the study area. Attenuation of coda waves (dpeaa)DE-He213 Single back scattering method (dpeaa)DE-He213 Coda Q (dpeaa)DE-He213 Lapse time (dpeaa)DE-He213 Eastern India Shield (dpeaa)DE-He213 Bhukta, Kuntal aut Tarafder, Gaurab aut Enthalten in Acta geodaetica et geophysica Hungarica Budapest : Akad. Kiadó, 1997 51(2015), 2 vom: 05. Juli, Seite 333-346 (DE-627)364470852 (DE-600)2110468-2 1587-1037 nnns volume:51 year:2015 number:2 day:05 month:07 pages:333-346 https://dx.doi.org/10.1007/s40328-015-0129-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 51 2015 2 05 07 333-346 |
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Coda window lengths of 30, 40 and 50 s were selected after thorough analysis of the waveforms. The Coda Q ($ Q_{c} $) values were computed using single back scattered method. The earthquakes parameters were compiled from catalogue of Indian Meteorological Department (Nodal agency under Govt. of India for record keeping and data sharing), New Delhi. The estimated average $ Q_{c} $ values for three coda windows 30, 40 and 50 s are $ Q_{c} $ = 259.$ 1f^{0.808} $, $ Q_{c} $ = 275.$ 9f^{0.764} $ and $ Q_{c} $ = 397.$ 1f^{0.651} $, respectively. The average $ Q_{c} $ value estimated from the $ Q_{c} $ values for the time windows 30, 40 and 50 s is found to be $ Q_{c} $ = 313.$ 2f^{0.73} $. Thus, the attenuation follows the power law relationships (e.g., $ Q_{c} $ = $ Q_{0} %$ f^{n} $), and the moderate to higher values of frequency parameters (n) obviously show that the $ Q_{c} $ value is a strong function of frequency. 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Abstract We have analyzed 16 earthquake waveform data recorded during the period from 2006 to 2013 at broadband station lying at the premises of Indian School of Mines, Dhanbad in the Eastern Indian Shield region. Coda window lengths of 30, 40 and 50 s were selected after thorough analysis of the waveforms. The Coda Q ($ Q_{c} $) values were computed using single back scattered method. The earthquakes parameters were compiled from catalogue of Indian Meteorological Department (Nodal agency under Govt. of India for record keeping and data sharing), New Delhi. The estimated average $ Q_{c} $ values for three coda windows 30, 40 and 50 s are $ Q_{c} $ = 259.$ 1f^{0.808} $, $ Q_{c} $ = 275.$ 9f^{0.764} $ and $ Q_{c} $ = 397.$ 1f^{0.651} $, respectively. The average $ Q_{c} $ value estimated from the $ Q_{c} $ values for the time windows 30, 40 and 50 s is found to be $ Q_{c} $ = 313.$ 2f^{0.73} $. Thus, the attenuation follows the power law relationships (e.g., $ Q_{c} $ = $ Q_{0} %$ f^{n} $), and the moderate to higher values of frequency parameters (n) obviously show that the $ Q_{c} $ value is a strong function of frequency. The increasing values of $ Q_{0} $ with increasing lapse time indicating the depth dependency of attenuation, and accounts for decreasing heterogeneity towards deeper level beneath the study area. © Akadémiai Kiadó 2015 |
| abstractGer |
Abstract We have analyzed 16 earthquake waveform data recorded during the period from 2006 to 2013 at broadband station lying at the premises of Indian School of Mines, Dhanbad in the Eastern Indian Shield region. Coda window lengths of 30, 40 and 50 s were selected after thorough analysis of the waveforms. The Coda Q ($ Q_{c} $) values were computed using single back scattered method. The earthquakes parameters were compiled from catalogue of Indian Meteorological Department (Nodal agency under Govt. of India for record keeping and data sharing), New Delhi. The estimated average $ Q_{c} $ values for three coda windows 30, 40 and 50 s are $ Q_{c} $ = 259.$ 1f^{0.808} $, $ Q_{c} $ = 275.$ 9f^{0.764} $ and $ Q_{c} $ = 397.$ 1f^{0.651} $, respectively. The average $ Q_{c} $ value estimated from the $ Q_{c} $ values for the time windows 30, 40 and 50 s is found to be $ Q_{c} $ = 313.$ 2f^{0.73} $. Thus, the attenuation follows the power law relationships (e.g., $ Q_{c} $ = $ Q_{0} %$ f^{n} $), and the moderate to higher values of frequency parameters (n) obviously show that the $ Q_{c} $ value is a strong function of frequency. The increasing values of $ Q_{0} $ with increasing lapse time indicating the depth dependency of attenuation, and accounts for decreasing heterogeneity towards deeper level beneath the study area. © Akadémiai Kiadó 2015 |
| abstract_unstemmed |
Abstract We have analyzed 16 earthquake waveform data recorded during the period from 2006 to 2013 at broadband station lying at the premises of Indian School of Mines, Dhanbad in the Eastern Indian Shield region. Coda window lengths of 30, 40 and 50 s were selected after thorough analysis of the waveforms. The Coda Q ($ Q_{c} $) values were computed using single back scattered method. The earthquakes parameters were compiled from catalogue of Indian Meteorological Department (Nodal agency under Govt. of India for record keeping and data sharing), New Delhi. The estimated average $ Q_{c} $ values for three coda windows 30, 40 and 50 s are $ Q_{c} $ = 259.$ 1f^{0.808} $, $ Q_{c} $ = 275.$ 9f^{0.764} $ and $ Q_{c} $ = 397.$ 1f^{0.651} $, respectively. The average $ Q_{c} $ value estimated from the $ Q_{c} $ values for the time windows 30, 40 and 50 s is found to be $ Q_{c} $ = 313.$ 2f^{0.73} $. Thus, the attenuation follows the power law relationships (e.g., $ Q_{c} $ = $ Q_{0} %$ f^{n} $), and the moderate to higher values of frequency parameters (n) obviously show that the $ Q_{c} $ value is a strong function of frequency. The increasing values of $ Q_{0} $ with increasing lapse time indicating the depth dependency of attenuation, and accounts for decreasing heterogeneity towards deeper level beneath the study area. © Akadémiai Kiadó 2015 |
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