ABSTRACT: Several Pb-ln-Cu nuneraMzatioo» have been observed İn Çanakkale, Yenice province area. Ho   doubt most significant of these are Arapueandere? where two mining operations ore underway» and Kalkim - Handeresi vicinity where drilling work has been completed. Two points of view are accepted on the gemmas of mineraltatton in the Teflon, The Sofular and Kullum mmoralliy.aüon observed here are typical products of contact metainorphiwn. The harnfels zones observed here indicate that toe meéisonmtlo in toe FalizaMôns ar© formed as a result of intrusion oantact. There İş no disagreement on the genesis of these two mineraUEatlon, both Turkish and expatriate geologist —having conducted researches— concur on this. The Fb-Cu`mİnerali/ atioiLs in Arapueandere and Kurttas. are tot the same para^enesis, l^pe of deposits are in the form of veins. The geochemical analyses made for Pb miıit-ralizütlons tn Arapuçandere and Kurt taşı are of th© mam parageneste. Type of deposits are in ®LB form of veins. The geocAemlcal analyse» roa^ far Pb mtoaralimtton In arkoslc series and An mineralization to diabase in arapucäitdere vicinity have indicated that these rocks formed the preconcentoation sources for the said minerals. No close has been observée between the dasitte breccias and anoesited of Tertiary volcanism, analysethvlth regard to petrologieal ciuaUt`es and aa wall roota and mineraMzatton, On t^e other hand, tile Pb-Zn m tlıe pre-eoncentrated form remoMlteed especialtty during iuUUc intrusions in ttte region have been immediately imbedded In the joints an4 faults to the form of veto« upon contact with hydrometelflfc sulphurous gluttons,