In this study we compare three pairs of conjugate rifted margins that are often referred to as
archetypes of rift systems. Despite numerous differences, a remarkable first-order structural …

Crustal rheology controls the style of rifting and ultimately the architecture of rifted margins.
Here we review the formation of three magma-poor margin pairs, Iberia-Newfoundland, the …

When continents break apart, continental crust and lithosphere are thinned until break-up is
achieved and an oceanic basin is formed. The most remarkable and least understood …

Abstract The Bay of Biscay and the Pyrenees correspond to a Lower Cretaceous rift system
including both oceanic and hyperextended rift domains. The transition from preserved …

The third edition of this widely acclaimed textbook provides a comprehensive introduction to
all aspects of global tectonics, and includes major revisions to reflect the most significant …

We present a new analysis of the lithospheric architecture of Africa, and its evolution from ca.
3.6 Ga to the present. Upper-lithosphere domains, generated or reworked in different time …

The rifting of continents involves faulting (tectonism) and magmatism, which reflect the strain-
rate and temperature dependent processes of solid–state deformation and decompression …

In classical rift models, deformation is either uniformly distributed leading to symmetric fault
bounded basins overlying stretched ductile lower crust (eg pure shear McKenzie model) or …

Amerasia Basin is the product of two phases of counterclockwise rotational opening about a
pole in the lower Mackenzie Valley of NW Canada. Phase 1 opening brought ocean …

We focus on the southern North Atlantic rifted margins to investigate the partitioning and
propagation of deformation in hyperextended rift systems using plate kinematic modeling …