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On subducting slab entrainment of buoyant asthenosphere
Author(s) -
Phipps Morgan J.,
Hasenclever Jörg,
Hort M.,
Rüpke L.,
Parmentier E. M.
Publication year - 2007
Publication title -
terra nova
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.353
H-Index - 89
eISSN - 1365-3121
pISSN - 0954-4879
DOI - 10.1111/j.1365-3121.2007.00737.x
Subject(s) - asthenosphere , geology , subduction , slab , entrainment (biomusicology) , geophysics , lithosphere , mantle (geology) , boundary layer , slab window , seismology , mechanics , oceanic crust , tectonics , philosophy , physics , rhythm , aesthetics
Laboratory and numerical experiments and boundary layer analysis of the entrainment of buoyant asthenosphere by subducting oceanic lithosphere implies that slab entrainment is likely to be relatively inefficient at removing a buoyant and lower viscosity asthenosphere layer. Asthenosphere would instead be mostly removed by accretion into and eventual subduction of the overlying oceanic lithosphere. The lower (hot) side of a subducting slab entrains by the formation of a ∼10–30 km‐thick downdragged layer, whose thickness depends upon the subduction rate and the density contrast and viscosity of the asthenosphere, while the upper (cold) side of the slab may entrain as much by thermal ‘freezing’ onto the slab as by mechanical downdragging. This analysis also implies that proper treatment of slab entrainment in future numerical mantle flow experiments will require the resolution of ∼10–30 km‐thick entrainment boundary layers.