Adriano Zanferrari

Looking inside Late Variscan tectonics: structural and metamorphic heterogeneity of the Eastern Southalpine Basement (NE Italy)

The Eastern Southalpine Basement on the southern side of the Brixen granodiorite pluton is comprised of two rock volumes separated by a shear zone and characterised by contrasting thermo-mechanical evolutions. The first rock volume appears in three different areas within hectometric folds consisting of amphibolite-facies paragneiss with polyphase structural and metamorphic evolution: a) D1 developed in HT-MP conditions: the assemblage Qtz + Pl + Bt + Kfs + Grt assemblage is preserved within D1 microlithons ; b) D2 is recorded in HT-LP conditions. Assemblages Bt + And + Crd, and Qtz + Kfs + Sil + Pl + Crn, developed within the differentiated S2 layering ; c) D3 developed in greenschist-facies, characterized by assemblage Ser + Qtz + Chl + Ab ; d) the contact aureole of the Brixen granodiorite pluton generating static growth of biotite, andalusite II and cordierite II at 282 ±14 Ma. The second rock volume corresponds to the Brixen – Sarntal metamorphic basement described in the literature, and consists of greenschistfacies metapelite. Field relationships indicate that HT-LP metamorphism took place before emplacement of the Brixen granodiorite and that paragneiss and metapelite were probably coupled at 320Ma, whereas the metamorphic aureole statically overprints the dynamic events and seals the contact.

The Friulian-Venetian Basin II: paleogeographic evolution and subsidence analysis from micropaleontological constraints

During the Cenozoic, the Friulian-Venetian Basin (FVB, NE Italy) underwent a complex evolution, related to the inherited Mesozoic sea-bottom topography and the load exerted by the main tectonic phases which affected the three surrounding belts: the Dinarides to the east, the Southern Alps to the north and the Northern Apennines to the south-west. The study of the foraminiferal assemblages from over 500 samples collected from 13 key wells provides important constraints on the paleobathymetric changes which occurred into the basin through time. Moreover, the defined bathymetric ranges, together with information on both thickness of the different depositional units and depositional geometries (derived from 2D seismic), were used as input in geohistory analysis in order to reconstruct the subsidence/uplift trends occurred in different sectors of the basin, as a response to collisional tectonics acting along basin boundaries. The collected results show that the overall depositional architecture of the FVB is the result of six main tectono-depositional phases (Lutetian, Chattian, Langhian, Tortonian, Piacenzian and Quaternary) characterised by paleobathymetric variations and subsidence/uplift trends reflecting the change in the tectonic control of the basin and the balance between subsidence and sediment supply. In particular, the easternmost sector of the FVB evolved as a Dinaric foredeep during Lutetian time. Since Chattian time (Cavanella Group), a moderate subsidence phase characterised by faint flexure to the north occurred, which was followed by a Langhian accentuated subsidence phase, consistent with the development of a Southalpine system. The accommodation space was progressively outpaced by the sediment flux during Serravallian-Messinian time as demonstrated by an overall shallowing upward trend recorded in this stratigraphic interval. A new basin configuration occurred during Piacenzian, when a complex geometry was developed due to the concurrent flexural load of the Southern Alps, to the North, and of the Apennines, to the South. Unlike the previous stratigraphic intervals, the Quaternary sedimentary sequence eventually shows a broadly symmetrical geometry with fast and relatively homogeneous subsidence all over the basin, overbalanced by the sedimentary supply. The observed symmetrical subsidence distribution could be interpreted as a consequence of both vanishing tectonic control and increase of sedimentary input related to increasing climatic variability.