The intrusive magmatism of Tertiary age call be seen neM the village of Pantelej in the Vardar zone, the Republic of Macedonia. This intrusive magmatism is present as a relatively smaller pluton built up of quartzmonzonites and monzonites. The chemical cOll1positioll of the rocks is very similar to the composition of the volcanic rocks that occur in the wider vicinity of the Kratovo - Zletovll volcanic area. The paper also presents data related to the contents of strOlltiull1 isotopes
