Continental extension may occur in two main different modes, narrow and wide rifting, which
mainly differ in the width of the deformed region. A third mechanism, the core complex, has …

Oceanic core complexes are the uplifted footwalls of very-large-offset low-angle normal
faults that exhume lower crust and mantle rocks onto the seafloor at slow-spreading ridges …

The" magmatic budget hypothesis" proposes that variability in magma supply is the primary
control on the large-scale hydrothermal distribution pattern along oceanic spreading ridges …

Abstract The Reykjanes Ridge is a key setting to study plate boundary processes overlaid
on a regional mantle melting anomaly. The ridge originated as one arm of a ridge-ridge …

Bathymetric, gravity, magnetic and backscattering strength data have been used to
characterise the segmentation of an 800 km long portion of the ultraslow-spreading …

In December 1995 we carried out a comprehensive controlled‐source electromagnetic
survey of the Valu Fa Ridge at 22° 25′ S in the Lau Basin. The Valu Fa Ridge is a back‐arc …

We report a comprehensive morphological, gravity and magnetic survey of the oblique-and
slow-spreading Reykjanes Ridge near the Iceland mantle plume. The survey extends from …

We utilize imaging data from the Galileo spacecraft to investigate band formation on one of
Jupiter's moons, Europa. Bands are polygonal features first observed in Voyager data close …

This paper is the first in a series of three (this issue) which present the results of the
RAMESSES study (Reykjanes Axial Melt Experiment: Structural Synthesis from …

Plume–ridge interaction in the Reykjanes Ridge and Iceland region is graphically
demonstrated by several V-shaped ridges surrounding the spreading axis, indicating mantle …