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