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Three tectonic foliations and their angular relation with bedding allow the determination of facing vs. vergence and fold interference pattern in polyphase low-grade metamorphic terrains, composed of Palaeozoic and Triassic turbiditic rocks cropping out in the inner part of the Northern Apennines (Mt Leoni area). The D 1 deformational event (Late Oligocene–Early Miocene) is typified by southeast-verging...
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