Fig. 8From: Variations of crustal thickness and average Vp/Vs ratio beneath the Shanxi Rift, North China, from receiver functionsSynthetic receiver function test. a The crustal velocity model with a 1-km-thick sedimentary layer. b Synthetic receiver function from model in a. c H-κ stacking of RF in b. d The crustal velocity model with a "transitional Moho". e Synthetic receiver function from model in d. f H-κ stacking of RF in eBack to article page