Original paper
Plume‐Induced Subduction Initiation: Single‐Slab or Multi‐Slab Subduction?
Abstract
Initiation of subduction following the impingement of a hot buoyant mantle plume is one of the few scenarios that allow breaking the lithosphere and recycling a stagnant lid without requiring any preexisting weak zones. Here, we investigate factors controlling the number and shape of retreating subducting slabs formed by plume-lithosphere interaction. Using 3-D thermomechanical models we show that the deformation regime, which defines formation...
Paper Details
Title
Plume‐Induced Subduction Initiation: Single‐Slab or Multi‐Slab Subduction?
Published Date
Feb 1, 2020
Volume
21
Issue
2
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History