L Federico

Biographic Data

ID8536637
NAMEL Federico
GIVEN NAMESL
FAMILY NAMEFederico
SIGNATUREFEDERICO L
AFFILIATIONSUniversity of Genoa
ORCID0000-0002-1994-973X
VERIFIEDYes
TOTAL WORKS6
TOTAL CITATIONS0
WORKS AS AUTHOR6
WORKS AS EDITOR0
FIRST PUBLICATION YEAR2015
LATEST PUBLICATION YEAR2023
H-INDEX0

  • D Modelling of Late Quaternary coastal evolution between Albenga and Loano (Western Liguria, Italy)

    Open AccessDanilo Morelli, Michele Locatelli et al.ARTICLEJournal of Maps2023

    Seismic lines and sediment cores collected along the shelf between Albenga and Loano (Liguria, NW Italy) allowed an unprecedented reconstruction of the characters and distribution of late Quaternary transgressive littoral deposits. Multiple seismic lines datasets and stratigraphic logs were managed within a single, GIS-based software. This approach allowed the merging, analysis, and interpretation of multimethodological datasets, greatly increasi…

  • Late orogenic tectonics in the Ligurian Alps (Italy)

    Open AccessL Federico, Laura Crispini et al.ARTICLEJournal of Maps2022

    This new map at 1:25,000 scale covers an area in the Western Alps (Italy), where the HP metamorphic basement is covered by a (predominantly clastic) late- and post-orogenic upper Eocene-lower Miocene cover. This provides unequivocal evidence that exhumation of the metamorphic units was accomplished by the lower Oligocene. The basement is made up of tectonic units with different metamorphic peaks that coupled during the exhumation path. Both basem…

  • A mountain slope deformation in an alpine metaophiolitic massif (Ligurian Alps, Italy)

    Open AccessFrancesco Faccini, L Federico et al.ARTICLEJournal of Maps2021

    Deep-seated gravitational slope deformation (DsGSD) represents a relevant geological-geomorphological feature of the landscape and has drawn scientific attention for the past several decades. During a detailed fieldwork in the Ligurian Alps, we identified areas (larger than ca 5 km2), characterized by very low percentage of outcrops, with rock blocks on the watershed and many morpho-tectonic evidences. Through the integration of geological-geomor…

  • Geology of the southern Monviso metaophiolite complex (W-Alps, Italy)

    Open AccessMichele Locatelli, L Federico et al.ARTICLEJournal of Maps2019

    The Monviso metaophiolite complex (W. Alps) is an almost intact fragment of Tethyan oceanic lithosphere metamorphosed to eclogite-facies peak metamorphic conditions during Alpine subduction. This 1:20.000 scale geological map encompasses, in an area of ∼35 km2, the Monviso Unit (MU) and the Lago Superiore Unit (LSU). Major focus was given to the Lower Shear Zone sub-unit (LSZ), where in the strongly deformed serpentinite-rich matrix are embedded …

  • Stratigraphic vs structural contacts in a late orogenic basin

    Open AccessL Federico, Laura Crispini et al.ARTICLEJournal of Maps2016

    This geological map (1:10.000 scale) of the ‘Sassello Basin’ remnant covers an area of about 33.4 km2 of Liguria (NW Italy); it highlights the occurrence of two main types of contacts between the sediments of the Tertiary Piedmont Basin and the metamorphic substratum (Voltri Unit): (i) stratigraphic and (ii) structural (thrust or steeply dipping faults). (i) Stratigraphic contacts are represented by the main transgressive surface and the nonconfo…

  • Geology of the Pontinvrea area (Ligurian Alps, Italy)

    Open AccessL Federico, Laura Crispini et al.ARTICLEJournal of Maps2015

    This geological map at the 1:10,000 scale shows the structural setting of two poly-deformed metaophiolite units, with different metamorphic peak conditions, i.e. the blueschist facies Montenotte Unit and the eclogite facies Voltri Unit, in a selected area of 8.2 km 2 within the Ligurian Alps (northern Italy). This study focuses on the tectonic contact between the two tectono-metamorphic units and on their relationships with the Oligocene sediment…