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- W2924908244 abstract "Abstract Seismic tomography provides unique constraints on the morphology, the deformation, and (indirectly) the rheology of subducting slabs. We use teleseismic double-difference P-wave tomography to image with unprecedented clarity the structural complexity of the Izu-Bonin slab. We resolve a tear in the slab in the mantle transition zone (MTZ) between 26.5° N and 28° N. North of the tear, the slab is folded in the MTZ. Immediately above the fold hinge, a zone of reduced P-wavespeed may result from viscous dissipation within an incipient shear zone. To the south of the tear, the slab overturns and lies flat at the base of the MTZ. The ~680 km deep 2015 Bonin earthquake (Mw~7.9) is located at the northernmost edge of the overturning part of the slab. The localised tearing, shearing and buckling of the Izu-Bonin slab indicates that it remains highly viscous throughout the upper mantle and transition zone." @default.
- W2924908244 created "2019-04-01" @default.
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- W2924908244 date "2019-03-21" @default.
- W2924908244 modified "2023-10-12" @default.
- W2924908244 title "Slab morphology and deformation beneath Izu-Bonin" @default.
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- W2924908244 doi "https://doi.org/10.1038/s41467-019-09279-7" @default.
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