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- W2213765030 endingPage "1352" @default.
- W2213765030 startingPage "1349" @default.
- W2213765030 abstract "The viscosity structure of Earth's deep mantle affects the thermal evolution of Earth, the ascent of mantle plumes, settling of subducted oceanic lithosphere, and the mixing of compositional heterogeneities in the mantle. Based on a reanalysis of the long-wavelength nonhydrostatic geoid, we infer viscous layering of the mantle using a method that allows us to avoid a priori assumptions about its variation with depth. We detect an increase in viscosity at 800- to 1200-kilometers depth, far greater than the depth of the mineral phase transformations that define the mantle transition zone. The viscosity increase is coincident in depth with regions where seismic tomography has imaged slab stagnation, plume deflection, and changes in large-scale structure and offers a simple explanation of these phenomena." @default.
- W2213765030 created "2016-06-24" @default.
- W2213765030 creator A5004361222 @default.
- W2213765030 creator A5073439468 @default.
- W2213765030 creator A5087428632 @default.
- W2213765030 date "2015-12-10" @default.
- W2213765030 modified "2023-10-12" @default.
- W2213765030 title "Viscosity jump in Earths mid-mantle" @default.
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- W2213765030 doi "https://doi.org/10.1126/science.aad1929" @default.
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- W2213765030 hasPublicationYear "2015" @default.
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