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

Aesthetically appealing thrust systems and related large-scale anticlines, in both active and
fossil foreland fold-and-thrust belts, and the economic potential associated with them, have …

A fault zone is produced by the displacement and linkage of component segments, and
hence these are important to the understanding of fault zone-development. A small well …

Relay ramps occur between normal fault segments that overstep in map view. The geometry
and evolution of exposure-scale relay ramps are described from the Somerset coast …

Large fault systems often result from the linkage of smaller faults. This produces an increase
in fault length, but a deviation from the simple displacement pattern observed for individual …

Damage zones are described around small scale normal, strike-slip, and reverse faults
cutting horizontally-bedded carbonates, shales and siltstones in the Bristol Channel basin …

Recent advances are reviewed in the understanding of the geometry and development of
steep, planar normal faults with up to hundreds of meters throw in multilayered sedimentary …

Three-dimensional (3D) seismic data from the continental margin offshore Israel (Eastern
Mediterranean) have been used to analyse the compressional structures within the toe …

We present a methodology to describe fault geometry at different scales and to characterize
the distribution of these scales on the flanks of a salt intrusion in the Colorado Plateau …

We investigate fault growth in Afar, where normal fault systems are known to be currently
growing fast and most are propagating to the northwest. Using digital elevation models, we …