Oceanic transform faults play an essential role in plate tectonics. Yet to date, there is no
unifying explanation for the global trend in broad-scale transform fault topography, ranging …

Lithospheric plates diverge at mid-ocean ridges and asthenospheric mantle material rises in
response. The rising material decompresses, which can result in partial melting, potentially …

Oceanic transform faults (OTFs) facilitate hydrothermal circulation which can modify the fault
zone materials and affect their rheological evolution. However, the depth extent and …

Abyssal T‐waves are seismo‐acoustic waves originating from abyssal oceans. Unlike
subduction‐zone‐generated slope T‐waves which are generated through multiple …

The depths of most moderate‐sized oceanic earthquakes are poorly constrained because of
the lack of local recording stations and noisy teleseismic recordings. This hampers our …

Constraining the controlling factors of fault rupture is fundamentally important. Fluids
influence earthquake locations and magnitudes, although the exact pathways through the …

Surface traces of earthquake faults are complex and segmented on multiple scales. At
seismogenic depth the detailed geometry of faults and earthquake rupture is mainly …

In the last decades, the slow-spreading Red Sea rift has been the objective of several
geophysical investigations to study the extension of the oceanic crust, the thickness of the …