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Diffusion Creep in Perovskite: Implications for the Rheology of the Lower Mantle

Karato, Shun-Ichiro, Li, Ping·1992·Science

Abstract

High-temperature creep experiments on polycrystalline perovskite (CaTiO 3 ), an analog of (Mg,Fe)SiO 3 perovskite of the lower mantle, suggest that (grain size-sensitive) diffusion creep is important in the lower mantle and show that creep rate is enhanced by the transformation from the orthorhombic to the tetragonal structure. These observations suggest that grain-size reduction after a subducting slab passes through the 670-kilometer discontinuity or after a phase transformation from orthorhombic to tetragonal in perovskite will result in rheological softening in the top portions of the lower mantle.

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Metadata

Authors
Karato, S.-I., & Li, P.
Venue
Science
Published
1992-03-06
Volume
255
Issue
5049
Pages
1238-1240
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W1973811075
Cited by
164
References
0
FWCI
15.10
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Diffusion Creep in Perovskite: Implications for the Rheology of the Lower Mantle. https://app.cochat.ai/papers/10.1126/science.255.5049.1238
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Karato, S.-I., & Li, P. (1992). Diffusion Creep in Perovskite: Implications for the Rheology of the Lower Mantle. Science. https://doi.org/10.1126/science.255.5049.1238

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