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The Morello Tectonic Unit in the Tuscan Apennines (Italy) represents the result of tectonosedimentary deformation, occurring in the frontal part of the non-metamorphosed Ligurian Accretionary Wedge, which consists of ophiolitic slices imbricated with a sedimentary succession containing ophiolite-bearing sedimentary mélanges. Geological mapping and structural and stratigraphic observations allow us to document that (1) the ophiolite-bearing sedimentary mélanges formed by gravitational reworking of material sourced from intrabasinal structural highs facing the oceanic basin environment from the Jurassic to early Eocene, before the middle Eocene accretion stage, and (2) the ophiolitic tectonic slices represent the scraping off at shallow structural levels of part of this sequence of crustal oceanic highs. The final internal architecture of the shallow frontal portion of the Ligurian Accretionary Wedge does not differ from those observed in metamorphosed orogenic belts and exhumed accretionary complexes throughout the world (e.g. blueschist and eclogite units of the Western Alps). This suggests that to the classical model of subduction and metamorphism followed by accretion and mélange formation (i.e. underplating), a model in which frontal accretion and ophiolite mélange formation at a shallow level are followed by underthrusting and subduction can be added, providing additional constraints for a better reconstruction of the evolution of orogenic belts and accretionary complexes. Thematic collection: This article is part of the Ophiolites, melanges and blueschists collection available at: https://www.lyellcollection.org/topic/collections/ophiolites-melanges-and-blueschists [ABSTRACT FROM AUTHOR]