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 …

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 …

Our capability to reconstruct past landscapes and the processes that shape them underpins
our understanding of paleo-Earth. We take advantage of a global-scale landscape evolution …

Thick packages of lavas forming seaward‐dipping reflectors (SDRs) are diagnostic features
of volcanic passive margins. Despite their significance to continental breakup studies, their …

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 …

We have interpreted 27,550 km of deep-penetrating, 2D-seismic reflection profiles across
the South Atlantic conjugate margins of Uruguay/Southern Brazil and Namibia. These …

Abstract The Early Cretaceous (135–130 Ma) continental rupture of Western Gondwana to
form the South American and African plates closely paralleled the elongate trends of …

Seaward dipping reflectors (SDRs) are a key feature within the continent to ocean transition
zone of volcanic passive margins. Here we conduct an automated pre-stack depth-migration …