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The Balkans are an E-W trending thrust belt mainly of Palaeogene age, generated by a left-lateral transpression with maximum stress-oriented N30°E. The transpressive nature of the Balkans may be deduced from theen echelon pattern of folds and thrusts which is due to oblique shortening with respect to pre-existing Mesozoic E-W trending crustal anisotropies between the Moesia Platform and the Balkans...
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