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The Marmolada-Vernel thrust system superimposed on the Contrin-San Nicolò-Lagusel diapiric anticline visible in cross-section.
Thrusting is consistent with Paleogene alpine orogenetic compressions directed toward the observer (SW). The diapiric nucleus and ladinian magmatic dikes cutting the folded beds suggest a middle Triassic age for the ENE-WSW trending fold.

Photo by Marcello Lancietti

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