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Crustal thicknesses and Poissonʼs ratios in the Ordos block and surrounding regions were estimated by the use of the H–k stacking method on teleseismic receiver functions. The data came from 353 temporary and permanent seismic stations in 2006–2011. Results show that the crustal thickness and Poissonʼs ratio gently vary within the Ordos block, with an average of 41.3 km and 0.265, respectively, consistent...
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