Porphyry-skarn　Cu　deposits　are　frequently　characterized　by　high　contents　of　dispersed　elements,　which　exhibit　significantly　diversified　enrichment　between　them.　However,　the　regularity　of　the　diversified　enrichment　remains　insufficiently　understood.　In　this　study,　the　primary　ore　minerals　present　in　the　Chengmenshan　deposit　were　investigated,　using　the　optical　microscope　and　scanning　electron　microscopy.　Additionally,　correlation　analysis,　cluster　analysis,　and　fractal　analysis　were　employed　to　explore　the　relationships　between　the　dispersed　elements　(Te,　Se,　Ga,　Ge,　Cd,　In,　and　Tl)　and　Bi　contents　in　the　drill　cores.　The　results　reveal　that　Te　is　predominantly　hosted　by　independent　minerals,　with　only　a　minor　fraction　incorporated　into　sulfides.　In　contrast,　other　dispersed　elements　are　incorporated　by　at　least　two　types　of　sulfide.　The　distribution　patterns　of　the　dispersed　elements　at　Chengmenshan　exhibit　multifractal　patterns,　except　for　Tl,　which　follows　a　simple　fractal　distribution　due　to　its　complex　occurrence.　The　enrichment　pattern　of　these　dispersed　elements　at　Chengmenshan　is　characterized　by　a　sequential　separation　and　spatial　dislocation.　The　pattern　is　likely　influenced　by　metallogenic　factors　such　as　temperature,　pH,　fS2,　and　fO2,　along　with　the　distinctive　geochemical　properties　of　the　dispersed　elements.　This　research　demonstrates　that　an　understanding　of　the　diversified　enrichment　regularity　of　these　dispersed　elements　could　be　instrumental　in　identifying　independent　deposits　of　these　elements.　Furthermore,　a　primary　halo　distribution　model　for　the　dispersed　elements　in　the　Chengmenshan　deposit　has　been　developed,　which　may　serve　as　a　valuable　reference　for　studying　the　genesis　of　associated　dispersed　element　deposits　and　for　the　prospecting　and　exploration　of　deeply　buried　targets.　©　2025　China　University　of　Geosciences.　All　rights　reserved.