The relationship between maximum displacement (dmax) and fault length (L) has been
studied extensively, mainly in attempts to understand how fault geometry varies over …

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 …

With the explosive growth in seismic data acquisition and the successful application of deep
convolutional neural networks (DCNN) to various image processing tasks within …

During early extension, cold continental lithosphere thins and subsides, creating rift basins.
If extension continues to final break-up, the split and greatly thinned plates subside deep …

Offset of each syn-fault horizon across a synsedimentary (ie growth) fault records the throw
subsequent to its deposition, allowing successive growth stages of a fault to be determined …

Abstract The Corinth Rift, central Greece, enables analysis of early rift development as it is
young (< 5 Ma) and highly active and its full history is recorded at high resolution by …

As a young (< 5 Myr old) active rift with high resolution spatial and temporal constraints, the
Corinth Rift is a natural laboratory for testing models of rift and fault network development in …

Synrift stratigraphy and the distribution of breakup‐related erosional unconformities vary
vastly between passive margins and cannot be explained by classical rifting models. Here …

Thrust faulting is a fundamental mode of crustal deformation, yet many of the key
geometrical attributes of thrust faults and the controls on fault rupture, growth, and linkage …

The formation of the Taranaki Basin, an active volcanic back‐arc rift situated in the
continental Australian Plate, is related to subduction of the Pacific Plate along the Hikurangi …