The organic geochemistry study on the black and red-beds of Cretaceous sediments from Chuangde section of Gyangzê in southern Tibet shows that the Organic carbon content of black beds is 5 to 10 times that of red beds, the predominant carbon number of the normal alkane in the black and red bed sediments are nC23 and nC25, respectively; The parent organic matter of both black and red beds was predominantly aquatic plants, and algae and bacteria with minor being terrestrial matter.