The stress dependence of olivine creep rate: Implications for extrapolation of lab data and interpretation of recrystallized grain size
The stress dependence of olivine creep rate: Implications for extrapolation of lab data and interpretation of recrystallized grain size
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DOI：
10.1016/j.epsl.2015.02.013
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发表时间：
2015-05-15
影响因子：
5.3
通讯作者：
Kohlstedt, D. L.
中科院分区：
文献类型：
--
作者：
Hirth, G.;Kohlstedt, D. L.
Based on measured values for the stress exponent, n approximate to 3.5, combined with the empirically determined relationship between dislocation density and stress (rho proportional to sigma(1.37)) and an analysis of diffusion kinetics in olivine, we conclude that silicon pipe diffusion limits strain rate in the dislocation creep regime. Furthermore, assuming that steady state recrystallized grain size is set by a dynamic balance between strain energy density (associated with dislocations) and surface energy density (associated with grain boundaries), the resulting dependence of recrystallized grain size on stress accurately describes experimental observations when the empirical dislocation density versus stress relationship is accounted for (d proportional to 1/sigma(1.37)). The improved physical understanding of the stress dependence of creep rate provides justification for incorporation of experimentally derived flow laws into models of geodynamical process and grain size evolution. These lab constraints combined with independent analyses of the stress dependence of mantle viscosity based on geophysical data provide bounds on rheological properties such as the yield stress of the lithosphere. (C) 2015 Elsevier B.V. All rights reserved.
