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- W2017486680 abstract "Synopsis Semipelitic rocks of the Crinan Subgroup Dalradian are, under certain conditions, susceptible to in situ reconstitution to form coarse-grained rock, originally mapped as ‘older granite’. The conditions necessary involve extensive shearing allowing fluids to percolate the rock, and increased heat flow from associated basic magmas. A belt of complexes formed in this way can be traced across the N E and Central Highlands of Scotland, and includes the Pannanich Hill Complex. Though the reconstitution of the complexes was probably diachronous along the belt, they all formed during the later part of the Caledonian Orogeny. During the reconstitution, some silicate melt may have formed and migrated along the shear zones, possibly to give the truly intrusive ‘older granites’." @default.
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- W2017486680 date "1991-12-01" @default.
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- W2017486680 title "The Pannanich Hill Complex and the origin of Crinan Subgroup migmatites in the North-eastern and Central Highlands" @default.
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- W2017486680 doi "https://doi.org/10.1144/sjg27020147" @default.
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