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《Chinese Journal of Geophysics》 2013-08
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Feasibility analysis of short-period seismograph receiver function——An example of Hotan Seismic Array,Xinjiang

TANG Ming-Shuai1,GE Can2,3*,ZHENG Yong2,WANG Hai-Tao1 1 Earthquake Administration of Xinjiang Uygur Autonomous Region.Urumqi 830011,China 2 State Key Laboratory of Geodesy and Earth Geodynamics,Institute of Geodesy and Geophysics, Chinese Academy of Sciences,Wuhan 430077,China 3 School of Earth Sciences,University of Chinese Academy of Sciences,Beijing 100049,China  
Using the teleseismic waveform data recorded by 9 sub-stations(including 1 set of broadband and 9 sets of short-period seismographs) of Hotan Seismic Array with an aperture about 3 km in 3 years,we studied and analysed the stability and reliability of short-period seismograph receiver function.By comparative analysis of the receiver function waveforms isolated from teleseismic waveform data recorded by short-period and broadband seismographs,the following results are obtained.(1) Receiver functions of short-period and broadband seismographs are very consistent and highly stable,they have good linear correlation(correlation coefficient 0.9),but Ps seismic phases have small amplitude difference(about 20%),whenever the Gaussian coefficient value is 1.5 or 2.5.(2) The short-period seismograph receiver functions can replace broadband seismograph receiver functions,if a method using the seismic phase arrival time of receiver functions is adopted(such as grid-stacking-search method).(3) The result may cause wrong interpretation(e.g.,the lower crust low-velocity layer) if only the waveform data of short-period seismograph receiver functions are used to invert for crustal S-wave velocity structure,because there exist large velocity deviations(about 0.3 km/s) from lower crust to upper mantle,due to lack of low frequency information under 0.155 Hz and the nonlinear amplitude response under 1 Hz of the short-period seismographs;so additional data sensitive to wave velocity value(such as surface wave dispersion) are needed for joint analysis.
【Fund】: 国家自然科学基金(41104037 41174086);; 地震公益性行业科研专项项目(201308013);; 中国地震局“测震台网青年骨干培养”专项(20130216);; 新疆地震科学基金项目(201103)联合资助
【CateGory Index】: P315
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