The combination of trace element and lead isotope ratio methods can complement the ability to trace bronze minerals. Previous measurements of the isotope ratio of bronzes in the cemetery of Guo State suggest that the bronze ore material may have originated at Zhongtiao Mountain in Shanxi and the middle and lower reaches of Yangtze River. The elemental analysis of this time shows that the trace elements of the bronzes are completely different from those of the Zhongtiao Mountain copper deposit in Shanxi, but have the same characteristics as those of the copper deposits and copper ingots from Tonglu Mountain in the middle and lower reaches of Yangtze River, and at ancient mining and smelting sites in southern Anhui. In addition, both trace elements and lead isotopes show that the bronzes of different tombs in the cemetery of Guo State share a consistent source of minerals, indicating that the source of bronzes unearthed from the cemetery of Guo State was relatively simple and stable.