Estimation of Geometrical Spreading Factor and Coda-Wave Attenuation Characteristics for the Saurashtra Horst in Western Deccan Volcanic Province, Gujarat, India

被引:1
作者
Bala, Indu [1 ,2 ]
Kumar, Santosh [1 ]
Sandhu, Manisha [1 ]
Chopra, Sumer [1 ,2 ]
Kumar, Dinesh [1 ]
机构
[1] Inst Seismol Res ISR, Gandhinagar, Gujarat, India
[2] Kurukshetra Univ, Dept Geophys, Kurukshetra, Haryana, India
关键词
FREQUENCY-DEPENDENT ATTENUATION; SHEAR-WAVES; S-WAVES; EARTHQUAKE SEQUENCE; CRUSTAL STRUCTURE; SOURCE PARAMETERS; PENINSULAR INDIA; P-WAVE; REGION; SCATTERING;
D O I
10.1785/0120230221
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
In the present study, we have estimated the coda Q (QC) and the geometrical spreading factor (gamma) for the Saurashtra region that is located in the western part of the Deccan Volcanic Province, Gujarat, India. The waveform data from the seismic network operated by the Institute of Seismological Research, Gandhinagar, are used for the analysis. We have used records of a total of 221 local earthquakes with epicentral distances less than 70 km from the seismic stations. The moment magnitude range of the earthquakes is 2.5-5.3, and the depth range is 1-22 km. The QC has been estimated at five central frequencies (1.5, 3, 6, 12, and 20 Hz) using 20, 30, and 40 s window lengths for vertical, north-south, and east- west components, respectively. The obtained QC values show that the attenuation in the region has a strong dependence on frequency and points toward a heterogeneous medium. The geometrical spreading factors are also estimated for two cases, that is, with and without Q at the same central frequencies and window lengths. The average geometrical spreading factors with Q are 1.37, 1.48, 1.40, 1.08, and 1.04, at central frequencies 1.5, 3, 6, 12, and 20 Hz, respectively, whereas it is 1.59, 1.53, 1.47, 1.19, and 1.14, respectively, in the absence of Q. The estimated values also indicate that the medium is heterogeneous in the Saurashtra region. The estimated region-specific coda Q and the geometrical spreading factor may help in the modeling of strong ground motions and assessment of the seismic hazard for the Saurashtra region.
引用
收藏
页码:2559 / 2575
页数:17
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