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Abstract. The thermotectonic evolution of the East Alpine Rhenodanubian flysch zone (RDFZ) and the collisional history along the orogenic front is reconstructed using apatite fission-track (FT) thermochronology. The apatite FT data provides evidence for a burial depth of at least 6km for the samples, which were totally reset. Burial was not deeper than 11km, since the zircon fission-track system was...
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