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| в условиях амфиболитовой фации (Later steeply dipping mylonite zones, formed under lower amphibolite-facies conditions, strike 75° and locally truncate earlier structures.; We present data from the Lewisian Complex, NW Scotland, where a suite of mafic dykes have undergone metamorphism and deformation at amphibolite facies. ArcticFox) | |||
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