Although the widths of fault damage zones commonly show a positive correlation with
displacements, these relationships also show a somewhat scattered distribution. We believe …

A review of field observations reveals that faults in the upper crust initiate in one of three
styles: linkage of pre-existing structures, linkage of precursory structures, or by localization of …

Damage zones show very similar geometries across a wide range of scales and fault types,
including strike-slip, normal and thrust faults. We use a geometric classification of damage …

Well-exposed strike-slip faults in limestones in the north-western part of Gozo show damage
zones that can be grouped into three categories based on their location along faults; tip …

The way that faults interact with each other controls fault geometries, displacements and
strains. Faults rarely occur individually but as sets or networks, with the arrangement of …

Epigenetic karstic systems in carbonate rocks commonly result from progressive dissolution
by acidic meteoric waters over thousands to millions of years. The generation of secondary …

Integrated geological-geophysical methods have been used to depict the geometric
characteristics and kinematic evolution of the Shunbei 5 (SB5) and adjacent Shunbei1 (SB1) …

Disjunctive, spaced solution cleavage in carbonate rocks is genetically associated with the
propagation of the left-lateral, strike-slip Mattinata Fault in the Gargano Promontory, Italy …

Small-scale structures along strike-slip fault zones in limestones exposed around the Bristol
Channel, UK, suggest that pressure solution plays a key role during fault nucleation and …

'Tensile Fracturing in Rocks' presents field observations on fracturing of sedimentary rocks
and granite outcrops from various provinces in three continents. It also combines results of …