Shanzhuping　deposit　is　located　in　the　southwestern　Zijinshan　ore　field,　Shanghang　County,　Fujian　Province,　develops　the　Au,　Cu　and　Mo　elements　anomaly,　and　forms　Au　and　Cu　deposit.　The　granodiorite　and　monzogranite　are　selected　for　carrying　on　petrology,　petrography,　whole　rock　geochemistry,　U-Pb　geochronology　and　Lu-Hf　isotope.　Here　we　report　the　monzogranite　and　granodiorite　206Pb/238U　weighted　mean　age　at　105.　2Ma　and　113.　4Ma.　Combined　with　the　zircon　characteristics　of　magma　oscillation　and　Th/U　ratios,　which　reveals　that　there　are　two　episodes　magmatic　activities　of　Late　Yanshanian.　The　granodiorite　and　monzogranite　share　geochemical　affinities　with　typical　island　arc,　enriched　Na　element　(Na2O/K2O　＞1),　light　rare　earth　element　(LREE),　large　icon　lithophile　element　(LIEE,　such　as　Ba　and　K),　and　U,　Th　and　Pb　etc.,　depleted　high　field　strength　element　(HFSE,　such　as　Nb,　Ta　and　Zr),　and　characterized　with　peraluminous　(A/CNK　with　1.　19　~　1.　68),　medium　(La/Yb)N(13.　6　~　17.　4),　and　high　Mg#(45.　89　~　48.　53);　slightly　negative　Eu　anomaly　(δEu　ranges　0.　79　to　0.　97),　and　slightly　positive　Ce　anomaly　(ranges　1.　0　~　1.　08).　The　peak　value　of　zircon　two-stage　Hf　model　age　(tDM2)　ranges　of　1.　05　~　1.　10Ga　and　0.　95　~　1.　OGa,　the　Hf(t)　ranges　of　-4.　47　~　+2.38　(mainly　negative　values)　and　-2.　73　~　+1.47　(mainly　positive　values),　respectively.　Based　on　previous　research　results　and　opinions　of　this　study,　we　infer　that　monzogranite　derived　from　melting　of　Mesoproterozoic　ancient　basement　in　upper　crust,　while　granodiorite　derived　from　the　Neoproterozoic　crustal　material　and　subjected　to　the　contamination　of　mantle　materials.　The　Shanzhuping　deposit　formed　in　Late　Yanshanian　island　arc　or　active　continent　margin　tectonic　setting,　which　is　closely　related　to　paleo-Pacific　plate　subducted　to　Eurasian　plate,　and　the　southwest　or　south　of　which　was　predicted　as　two　favorable　exploration　region.　©　2022　Science　Press.　All　rights　reserved.