ISSN 2320-5407 International Journal of Advanced Research (2016), Volume 4, Issue (1): 107- 117
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[1] Jon Andersson. Environmental Impact Assessment , 2014 .
[2] Arjun Kumar,et al. Software to Estimate Earthquake Spectral and Source Parameters , 2012 .
[3] M. Fehler,et al. Seismic Wave Propagation and Scattering in the Heterogeneous Earth , 2012 .
[4] I. Parvez,et al. Attenuation of P, S and Coda Waves in the NW-Himalayas, India , 2012 .
[5] B. Rastogi,et al. Attenuation of High Frequency P and S Waves in the Gujarat Region, India , 2011 .
[6] S. Padhy,et al. Attenuation of high-frequency seismic waves in northeast India , 2010 .
[7] H. Hamzehloo,et al. Attenuation of high frequency P and S waves in the crust of the East-Central Iran , 2009 .
[8] Babita Sharma,et al. Attenuation of P- and S-waves in the Chamoli Region, Himalaya, India , 2009 .
[9] B. Rastogi,et al. Attenuation of High-Frequency Seismic Waves in Kachchh Region, Gujarat, India , 2008 .
[10] F. Pacor,et al. Body-wave Attenuation in the Region of Garda, Italy , 2008 .
[11] Babita Sharma,et al. Attenuation of P, S, and coda waves in Koyna region, India , 2007 .
[12] B. Rastogi,et al. Low Coda Qc in the Epicentral Region of the 2001 Bhuj Earthquake of Mw 7.7 , 2004 .
[13] Tae-Woong Chung,et al. Attenuation of High-Frequency P and S Waves in the Crust of Choongchung Provinces, Central South Korea , 2004 .
[14] A. Papageorgiou,et al. Analysis of S-Wave Attenuation in South-Central Alaska , 2004 .
[15] W. Walter,et al. Stable and Transportable Regional Magnitudes Based on Coda-Derived Moment-Rate Spectra , 2003 .
[16] R. Castro,et al. An attenuation study using earthquakes from the 1997 Umbria-Marche sequence , 2002 .
[17] Tae-Woong Chung,et al. Attenuation of High-Frequency P and S Waves in the Crust of Southeastern South Korea , 2001 .
[18] R. Shanker,et al. Rupture Mechanism of Chamoli Earthquake on 29 March 1999 and its Implications for Seismotectonics of Garhwal Himalaya , 2000 .
[19] F. Pacor,et al. P- and S-wave attenuation in the region of Marche, Italy , 1999 .
[20] M. Ohtake,et al. Frequency-dependent Attenuation of High-frequency P and S Waves in the Upper Crust in Western Nagano, Japan , 1998 .
[21] S. Gupta,et al. Coda Q Estimates in the Koyna Region, India , 1998 .
[22] Rachel E. Abercrombie,et al. Near-surface attenuation and site effects from comparison of surface and deep borehole recordings , 1997, Bulletin of the Seismological Society of America.
[23] Steven M. Day,et al. Control of strong motion by the upper 30 meters , 1996, Bulletin of the Seismological Society of America.
[24] Brian J. Mitchell,et al. ANELASTIC STRUCTURE AND EVOLUTION OF THE CONTINENTAL CRUST AND UPPER MANTLE FROM SEISMIC SURFACE WAVE ATTENUATION , 1995 .
[25] M. Ohtake,et al. Frequency‐Dependent Attenuation of P and S Waves In the Kanto Area, Japan, Based On the Coda‐Normalization Method , 1993 .
[26] Hiroki Sato. Thermal structure of the mantle wedge beneath northeastern Japan: Magmatism in an island arc from the combined data of seismic anelasticity and velocity and heat flow , 1992 .
[27] S. Sekiguchi. Three-dimensional Q structure beneath the Kanto-Tokai district, Japan , 1991 .
[28] J. Plantet,et al. Frequency Dependence and Spatial Distribution of Seismic Attenuation in France: Experimental Results and Possible Interpretations , 1991 .
[29] L. Kvamme,et al. Q in southern Norway , 1989 .
[30] T. Masuda. Corner frequencies and Q values of P and S waves by simultaneous inversion technique , 1988 .
[31] Susan E. Hough,et al. High-frequency spectra observed at Anza, California: Implications for Q structure , 1988 .
[32] M. Wyss,et al. Local seismic activity in the region of the Assam Gap, northeast India , 1983 .
[33] Robert B. Herrmann,et al. Modeling some empirical vertical component Lg relations , 1983 .
[34] R. Console,et al. Attenuation parameters for Friuli region from strong-motion accelerogram spectra , 1981 .
[35] T. Rautian,et al. The use of the coda for determination of the earthquake source spectrum , 1978, Bulletin of the Seismological Society of America.
[36] P. Molnar,et al. Preliminary analysis of the spectral content of P and S waves from local earthquakes in the Garm, Tadjikistan region , 1978, Bulletin of the Seismological Society of America.
[37] Don L. Anderson,et al. Velocity dispersion due to anelasticity; implications for seismology and mantle composition , 1976 .
[38] K. Aki,et al. Origin of coda waves: Source, attenuation, and scattering effects , 1975 .
[39] J. Brune,et al. Corner frequencies of P and S waves and models of earthquake sources , 1973, Bulletin of the Seismological Society of America.
[40] K. Aki. Analysis of the seismic coda of local earthquakes as scattered waves , 1969 .
[41] M. Ritzwoller,et al. Pure and Applied Geophysics , 2017 .
[42] A. Abdel-Fattah. Attenuation of body waves in the crust beneath the vicinity of Cairo Metropolitan area (Egypt) using coda normalization method , 2009 .
[43] Dinesh Kumar,et al. Attenuation of P and S waves in the Kachchh Region , 2008 .
[44] S. K. Acharyya,et al. Seismotectonic atlas of India and its environs , 2000 .
[45] I. Singh. GEOLOGICAL EVOLUTION OF GANGA PLAIN : AN OVERVIEW , 1996 .
[46] Vrijendra Singh,et al. Attenuation of coda waves in the Garhwal Himalaya, India , 1995 .
[47] Keiiti Aki,et al. Attenuation of shear-waves in the lithosphere for frequencies from 0.05 to 25 Hz , 1980 .