The geochemistry and petrogenesis of the acidic-intermediate dyke and lava of the second cycle of Yixian Formation are studied. The result shows that the dykes have an average Mg# value of 36.68, with average Na2O/K2O = 1.07. In trace element spider diagram, the dykes are characterized by enriched Rb, Ba and K and depleted Nb, Ta, P, Ti and Sr. In addition, the rocks present a pronounced negative Eu anomaly, overlapped LREE pattern with that of lava and a strong fractionation in HREE in chondrite-normalized REE pattern, with an average Y/Yb ratio of 10.1 and (Ho/Yb)N = 1.13.