Sea-level change during the Holocene in Sardinia and in the northeastern Adriatic (central Mediterranean Sea) from archaeological and geomorphological data
F Antonioli, M Anzidei, K Lambeck, R Auriemma… - Quaternary Science …, 2007 - Elsevier
We provide new data on relative sea-level change from the late Holocene for two locations
in the central Mediterranean: Sardinia and NE Adriatico. They are based on precise …
in the central Mediterranean: Sardinia and NE Adriatico. They are based on precise …
Tectonic evolution of arcuate mountain belts on top of a retreating subduction slab: The example of the Calabrian Arc
In this paper, new paleomagnetic results from the Calabrian Arc are presented, together with
a critical review of all paleomagnetic data collected in the last decades in southern Italy. Our …
a critical review of all paleomagnetic data collected in the last decades in southern Italy. Our …
The carbonate tectonic units of northern Calabria (Italy): a record of Apulian palaeomargin evolution and Miocene convergence, continental crust subduction, and …
In northern Calabria (Italy), the metasedimentary succession of the Lungro–Verbicaro
tectonic unit preserves mineral assemblages suggesting underthrusting to depths in excess …
tectonic unit preserves mineral assemblages suggesting underthrusting to depths in excess …
The evolution of the Calabrian Arc: Evidence from paleomagnetic and GPS observations
The present-day arcuate shape of the Calabrian Arc has been accomplished during
Neogene and Early Pleistocene by large and opposite vertical axis rotations along the two …
Neogene and Early Pleistocene by large and opposite vertical axis rotations along the two …
Oblique indentation in the Eastern Alps: Insights from laboratory experiments
CL Rosenberg, JP Brun, F Cagnard, D Gapais - Tectonics, 2007 - Wiley Online Library
Experimental models scaled for density and viscosity were performed to investigate the
effects of indentation obliquity and rheological stratification on the deformation patterns …
effects of indentation obliquity and rheological stratification on the deformation patterns …
Interaction of tectonic, sedimentary, and diapiric processes in the origin of chaotic sediments: An example from the Messinian of Torino Hill (Tertiary Piedmont Basin …
F Dela Pierre, A Festa, A Irace - Geological Society of …, 2007 - pubs.geoscienceworld.org
Geologic mapping and integrated stratigraphic and structural observations of a gypsum
quarry from northwestern Italy allow evaluation of the relative contributions, the time …
quarry from northwestern Italy allow evaluation of the relative contributions, the time …
Upper mantle flow in the western Mediterranean
Two cross-sections of the western Mediterranean Neogene-to-present back-arc basin are
presented, in which geological and geophysical data of the TRANSMED Project are tied to a …
presented, in which geological and geophysical data of the TRANSMED Project are tied to a …
The architecture of brittle postorogenic extension: Results from an integrated structural and paleomagnetic study in north Calabria (southern Italy)
An integrated structural and paleomagnetic study was carried out on Neogene-Quaternary
clastic sedimentary sequences exposed in north Calabria to define the brittle postorogenic …
clastic sedimentary sequences exposed in north Calabria to define the brittle postorogenic …
Travertines as hydrologic archives: the case of the Pontecagnano deposits (southern Italy)
E Anzalone, V Ferreri, M Sprovieri… - Advances in Water …, 2007 - Elsevier
Spring waters (17° C), rich in HCO3-–Mg2+ and flowing along artificial channels, precipitate
carbonate incrustations at Pontecagnano (Salerno, southern Italy). The incrustations have …
carbonate incrustations at Pontecagnano (Salerno, southern Italy). The incrustations have …
[PDF][PDF] Fault-generated mountain fronts and the identification of fault segments: implications for seismic hazard assessment
AM Blumetti, L Guerrieri - BOLLETTINO-SOCIETA GEOLOGICA …, 2007 - researchgate.net
Normal fault-generated mountain fronts (FGMF) are the geomorphic expression resulting
from repeated normal surface faulting events over a geologic time period. The evolution of …
from repeated normal surface faulting events over a geologic time period. The evolution of …