This study investigates how rheology can influence the nucleation and evolution of strike-slip structures and, consequently, the structural architecture. To that end, we carried out a series of analog experiments using materials with different rheological behavior. The materials' properties, such as the angle of internal friction, cohesion, and density, were measured. The Particle Image Velocimetry (PIV) technique was applied to investigate the strain pattern on the surface, the amplitude of damage zones and fault core, the activeness/inactiveness of the structures over the evolution of strike-slip fault, and the earliest nucleation stage of fractures. Two sets of experiments were performed: i) single-layer experiments constituted by rheologically homogeneous material (quartz sand, dry clay, plaster powder, and a mixture of quartz sand and plaster powder), and ii) multilayer experiment using a heterogeneous stratified sequence of materials with different rheology. Except for the plaster powder model, during the first increments of deformation, the strain is widely distributed to give rise to a deforming zone with varying widths, where subsidiary structures nucleate. As deformation evolves, the deformation zone progressively narrows as the maximum strain concentrates along the main fault. Nucleation, development, and relative chronology of structures, such as R, R', P, Y-fractures, pull-apart basins, and positive and negative flower structures, varied according to the material used. The structural architecture of the dry clay and plaster powder models are more similar, with a greater quantity of smaller fractures than the other models. P-shears and pull-apart basins are also present. The quartz sand and mixture models developed a more complex damage zone and a higher topographic relief. The results emphasize that rheology is a controlling factor in the deformation zone architecture. Rheology controls fracture and fault arrangement, structure relative chronology, and the localization of contractional and extensional domains over all the stages of development of strike-slip tectonics.
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