Intraplate volcanism triggered by bursts in slab flux

Long-lived, widespread intraplate volcanism without age progression is one of the most controversial features of plate tectonics. Previously proposed edge-driven convection, asthenospheric shear, and lithospheric detachment fail to explain the ~5000-km-wide intraplate volcanic province from eastern Australia to Zealandia. We model the subducted slab volume over 100 million years and find that slab flux drives volcanic eruption frequency, indicating stimulation of an enriched mantle transition zone reservoir. Volcanic isotope geochemistry allows us to distinguish a high-μ (HIMU) reservoir [>1 billion years (Ga) old] in the slab-poor south, from a northern EM1/EM2 reservoir, reflecting a more recent voluminous influx of oceanic lithosphere into the mantle transition zone. We provide a unified theory linking plate boundary and slab volume reconstructions to upper mantle reservoirs and intraplate volcano geochemistry.

Mather, B.R., Müller, R.D., Seton, M., Ruttor, S., Nebel, O. and Mortimer, N., 2020. Intraplate volcanism triggered by bursts in slab flux. Science Advances6(51), p.eabd0953.

Publicity:  The story was covered by IFL ScienceCOSMOS magazine, (US)German Science News RIA Science News (Russia) and in the The Conversation.
ABC Radio Sydney Breakfast
 (6.37am) interviewed Ben Mather from the School of Geosciences about volcanic activity along Australia’s east coast. He was also interviewed on ABC Radio Central West NSW (8.42am).