Regional fluid and metal mobility in the
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D. Craw
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Article
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1990
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Springer
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English
โ 936 KB
A prominent set of veins was formed during post-metamorphic deformation of the Caledonian Dalradian metamorphic belt. These veins are concentrated in dilational zones in fold hinges, but apophyses follow schistosity and fold axial surface fractures. The veins are most common in the cores of regional