Abstract:Determination of the whole rock lead isotopic compositions of the Fenzishan and thePenglai groups gives two pb pb Pb pb isochron curves indicating the age of 2625.03 Ma and1165. 8 5MB,respectively. It is suggested that these data represent probably the ages when theFenzishan and the Penglai groupe were deposited. In the Light of the geochemical characterics oflead in sedimetation process the author infers that during sedimentation and diagenetic processes ofthe carbonate and clay rocks its pb isotopes...