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Parallel volcanic chains generated by plume-slab interaction

delete2026-08-30
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OA
AI
B
Ben Mather *
M
Maria Seton
S
Simon Williams
J
Joanne M. Whittaker
R
Rebecca Carey
M
Maëlis Arnould
N
Nicolas Coltice
A
A. F. Rogers
S
Saskia Ruttor
O
Oliver Nebel
C
Christopher M. Gonzalez
DOI：10.1016/j.gr.2026.08.002delete
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Abstract

Abstract

En 中文
• Subducting slabs deflect upwelling mantle plumes which can result in plume branches around the slab. • Plume branching caused by subducting slabs can sustain long-lived parallel volcanic chains. • Plume branching can explain the close spacing and geochemical similarity of the Tasmantid and Lord Howe hotspot chains in the Tasman Sea.

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Gondwana Research cover
Gondwana Research
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