Depth dependence of thermal transport properties for typical crustal rocks

Details Depth dependence of thermal transport properties for typical crustal rocks Depth dependence of thermal transport properties for typical crustal rocks

Jan 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992pepi...69..299s&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 69, Issue 3-4, p. 299-303.

Physics

8

Scientific paper

Thermal conductivity and thermal diffusivity were measured for a collection of granitic samples at high pressures (up to 500 MPa) and high temperatures (up to 750°C). The depth dependence was calculated from these results. As typical constituents of the lower crust, high-grade metamorphic rocks of the granulite facies were investigated. The thermal diffusivity was measured up to 1.8 GPa and 800°C under quasihydrostatic conditions. Thermal conductivity was calculated taking into account the temperature dependence of the specific heat from literature data. The depth dependence of the thermal transport properties was obtained from the experimental results using a graphical method.

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