Thermal anisotropy - a factor contributing to the distribution of Caledonian metamorphic zones in the SW Scottish Highlands?
Abstract
The distribution of metamorphic zones in the SW Scottish Highlands may have been influenced by the bulk thermal anisotropy of the regional structure.
Published
1976-01-01
How to Cite
G. J. Borradaile. (1976). Thermal anisotropy - a factor contributing to the distribution of Caledonian metamorphic zones in the SW Scottish Highlands?. Netherlands Journal of Geosciences, 41-45. Retrieved from https://njgjournal.nl/index.php/njg/article/view/14344
Issue
Section
Regular paper
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