Mid-Ocean Ridge Basalts (MORB) from the Northern Central Indian Ridge (NCIR) were recovered between latitudes 3° and 11° S and are olivine tholeiite with higher abundances of K and Rb. They are of typical transitional MORB (T-MORB) variety and appear to have been generated from an enriched-mantle peridotite source. The primitive NCIR MORBs having Mg# > 0.68 are the product of partial melting at an estimated pressure of ~ 1 GPa. It is inferred that the magma was subsequently modified at a pressure > 1 GPa by crystal fractionation and spinel was the first mineral to crystallize followed by separation of relatively Fe-rich olivine with subsequent decrease in pressure. During progressive fractionation at lower pressure (between 1–0.5 GPa), the bulk composition of the magma became systematically depleted in MgO, and enriched in ΣFeO, TiO2, P2O5 and Na2O. There was, however, limited gradual depletion in Al2O3 and CaO and concomitant enrichment in K2O. With the progressive fractionation these basalts became gradually enriched in V, Co, Y, Zr and to some extent in Sr, and depleted in Ni and Cr. In addition, the ΣREE of the magma also increased with fractionation, without any change in (La/Yb)n value. Mid-Ocean Ridge Basalts (MORB) from the Northern Central Indian Ridge (NCIR) were recovered between latitudes 3 ° and 11 ° S and are olivine tholeiite with higher abundances of K and Rb. They are of transitional MORB (T-MORB) variety and appear to have been generated from an enriched-mantle peridotite source. The primitive NCIR MORBs having Mg #> 0.68 are the product of partial melting at an estimated pressure of ~ 1 GPa. It is inferred that the magma was succeeded modified at a pressure> 1 GPa by crystal fractionation and spinel was the first mineral to crystallize followed by separation of relatively Fe-rich olivine with subsequent decrease in pressure. During progressive fractionation at lower pressure (between 1-0.5 GPa), the bulk composition of the magma was systematically depleted in MgO, and enriched in ΣFeO, TiO2, P2O5 and Na2O. There was, however, limited gradual depletion in Al2O3 and CaO and concomitant enrichment in K2O. With the progressive fractionation These basalts have been gradually enriched in V, Co, Y, Zr and to some extent in Sr, and depleted in Ni and Cr. In addition, the ΣREE of the magma also increased with fractionation, without any change in (La / Yb) n value.