Attenuation of High-Frequency P and S Waves in the Crust of Central and Western Tien Shan

Attenuation of High-Frequency P and S Waves in the Crust of Central and Western Tien Shan
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天山中西地壳高频纵横波的衰减

DOI:
10.1007/s00024-020-02504-1
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发表时间:
2020-05
影响因子:
2
通讯作者:
Huang Zongying
Huang Zongying
中科院分区:
地球科学3区
文献类型:
--
作者:
Ma Xiaolong;Huang Zongying

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In order to better understand the attenuation characteristics in the crust of the central and western Tien Shan orogenic belt, we investigate bothQpandQsvalues by applying the extended coda-normalization method. We estimate the frequency-dependent attenuation of both P and S waves in the frequency band of 1.0–20.0 Hz using data from local networks. The average frequency relations ofQpandQshave been derived asQp= (61 ± 9)  ×f(1.21±0.08)andQs= (77 ± 6) ×f(1.11±0.04)by fitting a power-law frequency dependence model for the study region. The lowQ0and highηvalues indicate that the central and western Tien Shan is a tectonically and seismically active region. We also find lateral variations of bothQp,sandQs/Qpvalues, reflecting complex tectonic structures in the study area. In general, the relatively high-attenuation areas corresponding to tectonically active regions are found beneath mountainous ranges in the central Tien Shan whereas the relatively low-attenuation areas are associated with stable regions, such as Fergana Basin and Issyk-Kul Lake. Besides, regions in the central Tien Shan withQs/Qp> 1 are likely partially saturated with fluids or rich in scattering heterogeneities, whereas regions in the western Tien Shan displayQs/Qp< 1, possibly suggesting almost complete fluid saturation.
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