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Estimation of thermal conductivity from the mineral composition: Influence of fabric and anisotropy
Author(s) -
Pribnow Daniel,
Umsonst Thorsten
Publication year - 1993
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/93gl02135
Subject(s) - thermal conductivity , anisotropy , isotropy , quartz , mineral , mineralogy , materials science , geology , gneiss , thermal , conductivity , composite material , thermodynamics , metamorphic rock , petrology , metallurgy , optics , chemistry , physics
Measured values of thermal conductivity from crystalline rocks are compared with values calculated from the mineral content using the layered model. First, thermal conductivity is estimated using data based on quasi‐isotropic mixtures of fragments or powder. Second, the approach is applied on core data considering the anisotropy of some rock forming minerals. The numerical value of estimated thermal conductivity is controlled by the quartz content. Sheet‐silicates control anisotropy and fabric in gneisses and their thermal consequences. If information about the fabric of the rock is available, the anisotropy of minerals can be considered in a layered model and this improves the estimation of thermal conductivity from mineral contents.