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《Chinese Journal of Geophysics》 2013-01
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Joint P-and S-receiver function inversion based on the Bayesian theory

WANG Jun1,2,LIU Qi-Yuan1* 1 State Key Laboratory of Earthquake Dynamics,Institute of Geology,China Earthquake Administration,Beijing 100029,China 2 Institute of Earthquake Science,China Earthquake Administration,Beijing 100036,China  
S-receiver function is valuable for investigating the lithosphere velocity structure.Using synthetic seismogram technique,we have studied dynamic characteristics of S-receiver functions.Based on the Bayesian inversion theory and non-linear inversion technique of the complex spectral ratio of the P-receiver function,a joint P-and S-receiver function inversion technique is proposed in this study.Our results show that(1) epicenter distances are limited to 55°~80° for the S-receiver function inversion and the magnitude of events used in the inversion should be larger than 5.0 for a good enough signal to noise ratio;(2) the SLP conversion on the lithosphere-asthenosphere boundary(LAB) with gradient structure is weaker than that on the sharp LAB,and the sediment is in favor of the SLP conversion at LAB;(3) since the radial component of S-receiver functions is not a delta pulse,the multi-channel maximal likelihood deconvolution technique for three-component receiver function estimation not relying on the source equalization assumption is more suitable for estimating S-receiver function;(4) numerical tests demonstrate that when the deviation of initial model is within 20% from the true model,our method can well predict the model parameters of the crust and upper mantle down to 300 km depth;(5) observational data tests demonstrate that the resultant S-wave velocities at depth larger than 100 km are less well constrained.
【Fund】: 国家自然科学基金(40774019)资助
【CateGory Index】: P315
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