Abstract:Based on the contrast between characteristic lithology combination in lower Cambrian in stratigraphic region in North China and characteristic lithology combination sequences in Luzhong area, according to the sedimentary framework named as “two gray and two red”, continuous succession of lithostragraphic units have been established as follows: Yutaishan formation— Liguan formation—Yuliangcun formation—Mantou formation. The bottom layers of Huoshan formation in Shanxi province and other areas in western Shanxi province and Mantou formation are quite the same.