Slab morphology and deformation beneath Izu-Bonin
Haijiang Zhang (),
Fan Wang,
Robert Myhill () and
Hao Guo
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Haijiang Zhang: University of Science and Technology of China
Fan Wang: University of Science and Technology of China
Robert Myhill: University of Bristol
Hao Guo: University of Science and Technology of China
Nature Communications, 2019, vol. 10, issue 1, 1-8
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.
Date: 2019
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Persistent link: https://EconPapers.repec.org/RePEc:nat:natcom:v:10:y:2019:i:1:d:10.1038_s41467-019-09279-7
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DOI: 10.1038/s41467-019-09279-7
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