Hidden role of garnet reveals how Earth’s 660-km seismic boundary forms
Peer-Reviewed Publication
Updates every hour. Last Updated: 23-Oct-2026 11:17 ET (23-Oct-2026 15:17 GMT/UTC)
Earth’s 660-km seismic discontinuity has long been attributed to ringwoodite breakdown, but this alone cannot explain complex seismic observations. Now, researchers have shown that the boundary forms through a coupled post-spinel transition involving majorite garnet, the mantle’s second most abundant mineral. This mechanism consistently explains seismic structure beneath subduction zones and mantle plumes and supports a compositionally homogeneous, pyrolite-like mantle, providing new insights into Earth’s deep interior and mantle dynamics.
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