Many continental rifts are subjected to volcanism in tandem with rifting, which has raised a
long-standing debate about whether magmatism is the cause or the consequence of plate …

Abstract The North Atlantic, extending from the Charlie Gibbs Fracture Zone to the north
Norway-Greenland-Svalbard margins, is regarded as both a classic case of structural …

Physical models predict that multiphase rifts that experience a change in extension direction
between stretching phases will typically develop non-colinear normal fault sets …

The central Nanling region in South China was the site of uplift, extensional deformation,
granite magmatism and hydrothermal activity from 180 to 150 Ma. Information on the age …

We present here a synthesis of the evolution of rifted continental margin systems in the Gulf
of Aden. These margins are volcanic to the West of the Gulf of Aden, where they are …

Many rifts develop through multiphase extension; it can be difficult, however, to determine
how strain is distributed during reactivation because structural and stratigraphic evidence …

This is the first detailed report and analyses of deformation from the W part of the Deccan
large igneous province (DLIP), Maharashtra, India. This deformation, related to the India …

The geometry and kinematics of rifts are strongly controlled by pre-existing structures that
may be present in both the crust and the mantle lithosphere. In the Gulf of Aden, the Tertiary …

The rift basins of Thailand exhibit remarkable diversity of fault displacement patterns, fault
length–displacement characteristics and mapped fault patterns during late rift, and post-rift …

We use scaled experimental (analog) models to investigate how the properties of a
population of pre-existing normal faults influence fault development during a subsequent …