Metamorphism of the Scourian Complex, NW Scotland

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Abstract
The rocks of the Scourian Complex have been intensively studied, but there is still no consensus as to the conditions of the granulite‐facies metamorphism preserved in these rocks. Recent estimates of these conditions fall into two groups, one at 820‐920°C and ca. 11 kbar and the second at ca. 1000°C and >12 kbar. Investigation of a variety of rocks shows that the recorded conditions vary with grain‐size, with higher‐grade conditions recorded by the cores of coarser (ca. 10 mm) crystals, and lower‐grade conditions recorded by the rims of coarser grains and by finer grains. This observation suggests that re‐equilibration during recovery of these rocks to the surface has been important which may account for the discrepancy in estimated P‐T conditions. Revised estimates of the equilibration conditions of the Scourian Complex of T > 1000°C and P > 8.5 kbar are presented. The conditions suggested for the peak of metamorphism mean that the role of anatexis in the genesis of these rocks must be considered and the nature of the fluid phase thoroughly investigated.