Thermal properties of rocks at high temperatures
|Authors:||Mebed, M. M.|
|Volume Title:||High Temperatures. High Pressures|
|Source:||High Temperatures. High Pressures, 15(1), p.113-118. Publisher: Pion Limited, London, United Kingdom. ISSN: 0018-1544|
|Summary:||The thermal diffusivity (a), specific heat (Cp) and thermal conductivity (lambda) of granite, basalt, gabbro-diorite and microcline were measured from 350 to 1100 K. Above 500 K the observed behaviour of Cp is in accordance with the Dulong-Petit law. lambda decreases at a higher rate than T-1 for granite (wrongly attributed to graphite in the printed abstract). In basalt, lambda decreases more slowly than T-1; the same applies to gabbro-diorite and microcline. [C.M.B.H.]|
|Subjects:||Alkali feldspar; Basalts; Diorites; Feldspar group; Framework silicates; Gabbros; Granites; Heat flow; High temperature; Igneous rocks; Microcline; Plutonic rocks; Silicates; Specific heat; Temperature; Thermal conductivity; Thermal diffusivity; Thermal properties; Volcanic rocks|
|Copyright Information:||GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United Kingdom, Twickenham, United Kingdom|
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