The study on the lead and zinc mineralization in Tiran and compare it with the global lead and zinc deposits, the deposit was part of the Mississippi Valley type of deposits. Under study of geological Ore deposit is located in area of Sanandaj - Sirjan and Malayer - Isfahan of metallogeny zone. This Ore deposit include 5 stratigraphic units, which are units of the K1 (Lump lime thick layer) and K2 (sandy limestone shale) are directly related to the mineralization. Mineralization occurred by high-grade vein in the collision between the two units. Mineralization in this Ore deposit has a direct relationship with faults and fractures , So that the majority of ore mineralization located in the fault across the region and in the North West - South East which is that concurrent Zagros . The main minerals of Ore deposit are sphalerite and galena and important alteration include silicification and dolomitization. With the aim of achieving a factor to identify the fertile and infertile units, samples were take from four profiles of fertile and 2 profiles of infertile and 78 samples were analyzed ICP-MS. With classical univariate statistical analysis hierarchical cluster analysis methods, main component analysis, multiple regression principal component regression method for identifying a factor fertile units of sterilization was introduced, in the next step if the fertility of the sampled units, relationship to estimate the distance between the veins of ore samples were obtained on the basis of multi-element standards.