The Mănăila ore deposit lies in the Tulgheş Group a Cambrian-Ordovician island arc complex metamorphosed under greenschist facies conditions. Mănăila ore deposits together with other deposits located in the Tg3 formation of the Tulgheş Group is considered by severals authors to be of Kuroko type. The main purpose of the paper is to present the geochemical interpretation for REE, and selected trace from the Mănăila ore, Romania. The study was conducted on a series of ten samples collected from the Mănăila ore deposit separated in rock samples and mineralized samples. The data obtained from the analyses of REE was normalized to the chondritic value and plotted in spider diagrams. For the rock samples the range of REE contents is : 5.1 - 58.6 μg·g^-1 for La, 9.8 – 110 μg·g^-1 for Ce, 1.1 – 12.2 μg·g^-1for Pr, 4.8 – 40.9 μg·g^-1 for Nd, 1.1 – 7.3 μg·g^-1 for Sm, 0.21 – 1.54 μg·g^-1 for Eu, 1.71 – 7.3 for Gd, 0.28 – 1.05 μg·g^-1 for Tb, 1.5 – 6 μg·g^-1 for Dy, 0.33 -1.3 μg·g^-1 for Ho, 0.99 - 4.2 μg·g^-1 for Er, 0.15 – 0.63 μg·g^-1 for Tm, 1 – 4.1 μg·g^-1 for Yb, 0.14 -0.58 μg·g^-1 for Lu. The range of REE contents for mineralized samples is:3.9 – 4.2 μg·g^-1 for La, 8.3 – 9.8 μg·g^-1 for Ce, 0.93 – 1.1 μg·g^-1 for Pr, 3.2 – 4.5 μg·g^-1 for Nd, 0.74 – 1.2 μg·g^-1 for Sm, 0.15 – 0.2 μg·g^-1 for Eu, 1.2 -1.3 μg·g^-1 for Gd, 0.25 – 0.27 μg·g^-1 for Tb, 1.4-1.7 μg·g^-1 for Dy, 0.34-0.42 μg·g^-1 for Ho, 0.94-1.1 μg·g^-1 for Er, 0.16-0.16 μg·g^-1 for Tm, 0.95-1.1 μg·g^-1 for Yb, 0.14-0.18 μg·g^-1 for Lu,. An Eu anomaly is visible for the both group of samples, which in case of the mineralized samples is slightly more pronounced.