This study examines shear wave splitting of core-refracted seismic phases from earthquakes to determine seismic anisotropy in unexplored areas of Central India. Understanding seismic anisotropy is essential for gaining insights into past geodynamic processes and current tectonic activities in the area. Our findings show that mantle deformation is influenced by both present plate motion and prior orogenic events, such as subduction, collision, and mantle plume activity within the study region.