Kyanite in the mainland Lewisian complex.

A. C. Barnicoat, I. Cartwright, M. J. O'Hara

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Abstract

Kyanite is considered to have been the stable Al2SiO5 polymorph during Badcallian metamorphism in both the Stoer and Scourie areas of NW Scotland. T estimates of 900-1000oC for these areas imply minimum P of 12-14 kbar. Crustal thickening sufficient to give such P is known from the Alps and Himalayas; the rocks of the Scourie complex may have formed in a similar environment. - R.A.H.

Original languageEnglish
Pages (from-to)209-213
Number of pages5
JournalScottish Journal of Geology
Volume23
Issue number2
DOIs
Publication statusPublished - 1 Jan 1987
Externally publishedYes

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