Lattice thermal conductivity of MgO at conditions of Earth's interior
Author:
Publisher
Proceedings of the National Academy of Sciences
Subject
Multidisciplinary
Reference38 articles.
1. Interpretation of the D″ zone at the base of the mantle: Dependence on assumed values of thermal conductivity
2. Can large increases in viscosity and thermal conductivity preserve large-scale heterogeneity in the mantle?
3. The core–mantle boundary layer and deep Earth dynamics
4. The combined influences of variable thermal conductivity, temperature- and pressure-dependent viscosity and core–mantle coupling on thermal evolution
5. Core–mantle boundary heat flow
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