As a medium-low temperature tectonic altered hydrothermal Au deposit,Longshan Au ore field in Guigang is controlled by SN strike faulted structure and its ore-forming matters are derived from deep strata. Centered on Pingtianshan rock body and generated from deep mineral-bearing hydrothermal solution,metal-logenic series of a set of ore-forming development stages is formed under the condition of pneumato-hydro-thermal mineralization.At different structures and lithological parts,a set of different types of Au deposit compositions is formed and is characterized by multi-phase multi-period mineralization and concentration.