Abstract: The Lushan copper deposit occurred in the dark gray or black silty mudstone at the bottom of the Xuanwei Formation (P₃x), and the volcano breccia hematite bed at the top of the third section of Emeishan basalt (βP³). These ore-host strata with a new ore type were recognized as new copper mineralized horizons in Guizhou Province. The element zoning sequence in the ore-bearing rock from top to bottom is Ti-Cu-Fe, which is in accordance with the characteristics of the weathering and leaching copper deposit from basalt. The geological characteristics of the Lushan copper deposit was summarized by a detailed study, which provided some new ideas for the exploration of the same type copper deposit.