The Cambrian and Ordovician strata are scattered mostly in the region from Hetangou to Tianlinbei. They are composed of a series of structural slabs distributing latitudinally and were formed in the Mesozoic by thrust-napping. Since the of the Lower Cambrian Semagou Formation covers the Archaeozoic metamorphic rocks with anglulare conformity, it may be concluded that the Mesoproterozoic Shinagan Group is absent in the region. The connection of the Cambrian and Ordovician is parallel unconformity, implying that a tectonic movement must have taken place between the Cambrian and Ordovician, which is a part of the rising process of the North China Plate. The forming mechanism of the movement may have some connections with the collision between the North China Plate and the massif in the Paleo -Asia ocean. The discovery of the movement has a great significance in recovering the tectonic evolution history of the North China Plate.