In the past two decades, the mobility of mid-ocean ridges relative to the mantle (absolute migration) have been correlated with major observable features, such as, spreading asymmetry and asymmetry in the abundance of seamounts. The mobility of mid-ocean ridges is also thought to be an important factor that influences the diversity of ridge-crest basalts. However, the mobility of mid-ocean ridges have not yet been defined and mapped. The absolute migration of global mid-ocean ridges since 85 Ma has been computed and mapped. Global mid-ocean ridges have migrated extensively at varying velocities during that period. Presently, the fast-migrating ridges are the Pacific-Antarctic ridges, migrating at velocities between 3.3 and 5.5 cm/yr. The slow-migrating ridges are the Mid-Atlantic and the southwest Indian ridges migrating at velocities between 0.3 and 2.0 cm/yr. Comparison of these results with mantle tomography results shows that the slow-migrating ridges have deeper depth of origin than the fast-migrating suggesting a correlation between the absolute migration velocity and the depth of origin of ridges. Furthermore, the southwest Indian ridge appears to be tapping the same portion of mantle as did the Central Indian ridge. These results have important thermo-chemical implications, such as variations in the extent of melting and mineralogical composition of the mantle beneath different ridges, which may influence mantle dynamic
ME Kamwaya (Sat,) studied this question.