The thorough interpretation of the South Atlantic long offset seismic lines provides a new
view of the magmatic and crustal architecture and of the evolution of the conjugate volcanic …

It is well established that sedimentary margins grow by sediments bypassing through shelf-
and slope-incising canyons onto the basin floor and by sediments being deposited …

Abstract The Late Cretaceous record offshore Argentina comprises an extensive
hybrid/mixed (turbidite-contourite) depositional system over 280,000 km 2. This offers a key …

Global sedimentary hiatuses are well-documented in ancient pelagic sediment, and include
Paleocene, Eocene-Oligocene boundary, and Miocene hiatuses. Less clear is the extent of …

The identification of several Cretaceous to Paleogene mixed turbidite-contourite systems
along the upper to middle continental slope of Nova Scotia provides a unique opportunity to …

In recent decades, Miocene marine transgressions in South America have sparked ongoing
debates concerning their boundaries, number of events, regional connectivity, and the …

Strain style, magnitude and distribution within mass‐transport complexes (MTCs) are
important for understanding the process evolution of submarine mass flows and for …

Abstract The Late Cretaceous is a critical period in the evolution of the South Atlantic.
Significant changes in the tectonic configuration of continental landmasses and marine …

Plastered drifts are a complex type of contouritic drift, very common along continental slopes,
although their precise sedimentary stacking pattern and long-term evolution are not well …

Hyperextended basins are increasingly recognized along the outboard parts of continental
margins as aborted basins created during continental break‐up. Many of the concepts for …