
doi: 10.1007/bf01821135
The Virani ophiolite complex consists of metamophosed ultramafics, mafics, and cherts, and forms an allochthonous sheet that structurally overlies a sequence of metamorphosed flysch-type deposits. The complex and structurally underlying metamorphosed sedimentary rocks have been affected by three phases of folding. The first and second phases of folding produced isoclinal folds with subparallel trends and nearly-horizontal axes which resulted in the apparent interlayered character of the rock units.
550.geology, Article
550.geology, Article
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