The Tianjiaba Formation, Zhoujiawan Formation and Jishan Formation in the Early Cretaceous Huicheng Basin are glutenite sedimentary successions. Paleocurrent and conglomerate composition indicate sediments are proximal developed from the southern and northern margin. Heavy mineral analysis result suggests source rock of Early Cretaceous sandstones are predominant magmatic rocks, minor metamorphic rocks and sedimentary rocks. Geochemical data for these rocks suggest a continental island arc setting and continental active margin. Together with regional geological evidence, the sediments were deposited in a pull-apart basin.