Thermal diffusivity and conductivity of olivine, wadsleyite and ringwoodite to 20 GPa and 1373 K

By Yousheng Xu, T. Shankland, S. Linhardt, D. Rubie, F. Langenhorst, Kurt Klasinski. 2004

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A new large-volume multianvil system (2004, methodology): “Large sample volumes are also essential for many physical property measurements, such as thermal diffusivity, electrical conductivity and elastic properties using ultrasonic measurements (e.g.Xu et al., 2004).”
Temperature, lithosphere‐asthenosphere boundary, and heat flux beneath the Antarctic Plate inferred from seismic velocities (2015, background): “…show that conductivity depends inversely on temperature for minerals of the crust (1.5–4.0Wm 1K 1) [Clauser and Huenges, 1995;Whittington et al., 2009] and upper mantle (olivine, wadsleyite, and ringwoodite) (2 5 Wm 1K 1) [Schatz and Simmons, 1972; Xu et al., 2004;McKenzie et al., 2005].”