Orogenic belts at oblique convergent subduction margins accommodate deformation in several trench parallel domains, one of which is the magmatic arc, commonly regarded as taking up the margin-parallel, strike-slip component. ...

margin, commonly driven by a transpressive regime of stress. They are often developed as a conjugate pair of master faults. Transverse structures, usually Riedel-like, connect both master faults, thus forming a structure ...

Transcurrent fault systems are structures that accomodates the obliquity of convergence throughout a subduction margin, commonly driven by a strike-slip to transpressive regime of stress. They are often developed as a ...

Fault development models are crucial to predict geometry and distribution of fractures at all scales. We present here structures related to the development of the Bolfin Fault in the Atacama Fault System (AFS), covering a ...

Orogenic belts at oblique convergent subduction margins accommodate deformation in several trench-parallel domains, one of which is the magmatic arc, commonly regarded as taking up the margin-parallel, strike-slip component. ...