Late Quaternary fluvial terraces of the Romagna and Marche Apennines, Italy: Climatic, lithologic, and tectonic controls on terrace genesis in an active orogen
KW Wegmann, FJ Pazzaglia - Quaternary Science Reviews, 2009 - Elsevier
We synthesize a new fluvial terrace chronostratigraphy of the Bidente and Musone Rivers
cast within a broader European framework, which forms the basis of a terrace genesis and …
cast within a broader European framework, which forms the basis of a terrace genesis and …
Morphotectonic evolution of the Adriatic piedmont of the Apennines: an advancement in the knowledge of the Marche-Abruzzo border area
M Della Seta, M Del Monte, P Fredi, E Miccadei… - Geomorphology, 2008 - Elsevier
This study focuses on the morphotectonic evolution of the Apennines Central Adriatic
piedmont, and in particular on the region along the Marche-Abruzzo border …
piedmont, and in particular on the region along the Marche-Abruzzo border …
Unraveling tectonic and climatic controls on synorogenic growth strata (Northern Apennines, Italy)
We develop a new high-resolution stratigraphic age model to unravel the contributions of
tectonic and climatic processes on early to late Pleistocene synorogenic growth strata. We …
tectonic and climatic processes on early to late Pleistocene synorogenic growth strata. We …
Pleistocene sea-level changes, sapping processes and development of valley networks in the Apulia region (southern Italy)
G Mastronuzzi, P Sansò - Geomorphology, 2002 - Elsevier
The central area of the Apulia region is characterized by a network of valleys with peculiar
features, locally called 'gravine'or 'lame'. They are short, straight valleys, deeply incised in …
features, locally called 'gravine'or 'lame'. They are short, straight valleys, deeply incised in …
Alluvial terraces on the Ionian coast of northern Calabria, southern Italy: Implications for tectonic and sea level controls
In this paper we present the results of an integrated geomorphological, pedological and
stratigraphical study carried out along the Ionian coast of northern Calabria (southern Italy) …
stratigraphical study carried out along the Ionian coast of northern Calabria (southern Italy) …
[HTML][HTML] Transient landscape and stratigraphic responses to drainage integration in the actively extending central Italian Apennines
AH Geurts, AC Whittaker, RL Gawthorpe, PA Cowie - Geomorphology, 2020 - Elsevier
Drainage networks in continental rifts are generally reported as dynamic features that
produce transitions between endorheic and exorheic conditions. While this is of major …
produce transitions between endorheic and exorheic conditions. While this is of major …
Paleogeographic and paleodrainage changes during Pleistocene glaciations (Po Plain, northern Italy)
The Po Basin, a Pliocene marine gulf between the Alps and the Apennines, was filled
progressively from west to east and finally capped by fluvial sediments during the …
progressively from west to east and finally capped by fluvial sediments during the …
Middle Eocene to Early Miocene sedimentary evolution of the western Lombardian segment of the South Alpine foredeep (Italy)
A Di Giulio, B Carrapa, R Fantoni, L Gorla… - International Journal of …, 2001 - Springer
The main steps of the sedimentary evolution of the west Lombardian South Alpine foredeep
between the Eocene and the Early Miocene are described. The oldest is a Bartonian …
between the Eocene and the Early Miocene are described. The oldest is a Bartonian …
Quaternary evolution of the" Castelluccio di Norcia" basin (Umbro-Marchean Apennines, central Italy)
M Coltorti, P Farabollini - Alpine and Mediterranean Quaternary, 1995 - amq.aiqua.it
Castelluccio di Norcia is a closed depression, 12 km in length and 8 km in width, located in
the southern part of the Umbro-Marchean Apennines, westward from the highest reliefs of …
the southern part of the Umbro-Marchean Apennines, westward from the highest reliefs of …
[HTML][HTML] The interplay between adjacent Adige and Po alluvial systems and deltas in the late Holocene (Northern Italy)
The alluvial plain behind the southern Venice Lagoon, in northern Italy, is characterised by
the presence of a complex network of alluvial ridges formed by the aggradation of channel …
the presence of a complex network of alluvial ridges formed by the aggradation of channel …
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