Thermal Conductivity 18 pp 653-660 | Cite as
Heat Transport in Geologic Media: What We Can Learn in the Laboratory
Chapter
Abstract
Based on a study of a variety of minerals of the feldspar and the pyroxene groups, it is suggested that lamellar structures with a spacing of the order of tens of Å are responsible for the low thermal conductivity observed in these minerals above 100 K.
Keywords
Thermal Conductivity Lamellar Structure Rock Salt Phonon Scattering Amorphous Solid
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© Purdue Research Foundation 1985