The widely debated late Oligocene-middle Miocene Numidian Fm (NF) consists of
supermature quartzose sediments deposited in the Maghrebian Flysch Basin (MFB) …

Abstract The Apennines-Sicilian-Maghrebian fold-and-thrust belt originated from the
subduction of the Alpine Tethys and the later collision of drifted continental blocks against …

It is unanimously acknowledged that the Corsica‐Sardinia microplate rotated
counterclockwise (CCW) by 40–50° between 21 and 15 Ma, synchronous with Liguro …

Understanding the evolution of submarine channel‐lobe systems on salt‐influenced slopes
is challenging as these systems react to subtle, syn‐depositional changes in sea‐floor …

Seafloor topography affects the sediment gravity flows that interact with it. Understanding
this interaction is critical for accurate predictions of sediment distribution and …

Abstract The Monte San Nicola area (Southern Sicily) offers a spectacular exposure of open-
marine sediments that were employed in 1998 for defining the Global Stratotype Section and …

Thirteen seismic reflection profiles and field observations have been used to build a three-
dimensional watertight geological model of the sub-surface architecture of the Trapanese …

The northwest (NW) Borneo margin is one of the geologically most complex regions of
Southeast Asia characterized by a steep slope gradient and an extensive deepwater fold …

Abstract The Numidian Sandstones are widespread throughout the western Mediterranean,
from Spain and North Africa to southern Italy. They consist of intercalations of thick ultra …

Structural evolution of thrust wedges is influenced by syn-kinematic deposition ahead and
upon them. It dampens uplift of synclines and promotes amplification of anticlines. High …