Plume-slab interaction
Exploring the interaction between mantle plumes and subducting slabs in the Tasman Sea region, focusing on the three parallel hotspot tracks — Tasmantid, Lord Howe, and Cosgrove — …
Parallel volcanic chains generated by plume-slab interaction (invited)
Deep mantle plumes are buoyant upwellings rising from the Earth’s core-mantle boundary to its surface, and describing most hotspot chains. Mechanisms to explain dual chains of …
Slab-induced plume branching connects parallel hotspot chains
We propose that slab-induced plume branching can explain the formation of parallel hotspot chains observed in the oceanic and continental record. Using plate tectonic …
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. The eastern margin of Australia and Zealandia has …
DP20
Eruption and disuption: how Earth's deep interior and surface communicate
