Research suggests that the Zagros' lithospheric keel is inducing a diversion of mantle flow beneath the Iranian plateau. However, the relationship between this phenomenon and other geological processes is still being studied, with some research focusing on upper mantle forces and tectonics in nearby regions. The specific mechanisms and effects of this mantle flow diversion are not entirely clear, with various studies exploring related topics such as crustal structure and seismic anisotropy in different areas.