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《Chinese Journal of Geophysics》 2011-01
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Rayleigh wave tomography of the phase velocity in North China

PAN Jia-Tie,WU Qing-Ju,LI Yong-Hua,ZHANG Feng-Xue,ZHANG Guang-Cheng Institute of Geophysics,China Earthquake Administration,Beijing 100081,China  
Using the teleseismic data recorded by 190 broadband stations and 8 very broadband stations of the portable seismic array in North China during Oct.2006 to May.2009,short period(10~60 s)inter-station phase dispersions of fundamental Rayleigh waves are obtained by the method of frequency and time analysis of wavelet transformation.A total of 1587 independent dispersion curves were then arranged into a tomographic inversion scheme to obtain the pure-path phase velocity dispersion at 0.5° by 0.5° grids in this region.It shows that the S-wave structure of the crust and upper mantle beneath North China is heterogeneous.The phase velocity distribution at period of 10 s is related with the geologic units on the surface,but the effect of topography becomes weaker in the longer periods(15 s).In the middle period part(30 s),the difference of phase velocity between the eastern NCC and central NCC reveals the difference of composition in the middle-lower crust.At the same time,the gradient zone of phase velocity is very close to the gravity gradient zone of the Taihangshan on the map of period 30 s,and it indicates that there are many differences in the crustal structures on the two sides of the gravity gradient zone.Compared with the phase velocity maps of short periods,the lateral heterogeneity of phase velocity becomes much weaker in the longer period(60 s)maps.Compared with that in typical Craton,the phase velocity of NCC is much slower at periods of 10-60 s,whose dispersion characteristic is very similar with that in the typical rift regions of the world(e.g.Rio Grande Rift).It indicates the NCC has been obviously eroded and breached.
【Fund】: 国家自然科学基金(40774039 90814013);; 科技部科技基础性工作专项(2006FY110100)资助
【CateGory Index】: P631.4
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