The paper presents SHRIMP U-Pb dating results of zircon from south Luohansi group(the sediment wedge of forearc basin), cropping out from the north Qinling to Heihe River Xiaowangjian Huangcaoping. The age of crystal tuff obtained was 491±5 Ma. The obtained age indicates that this group is through Ordovician. Combined to granite belt of Caledonian stage widely grown in northern side of Shangdan belt, and the newest age information measured by predecessors in other places, the important evidence of isotopes chronology was offered to subduction of northern Qinling Paleozoic Oceanic basin and plate convergence.