Intraplate strike-slip zones commonly display intricate 3-D geometries, with rapid changes in
structural style along strike and with depth. Strike-slip deformation typically results in …

Experimental modelling applied to the study of orogenic wedge dynamics has been a
subject of fruitful research for more than 30years, although the technique dates back as far …

The Tertiary rift basins of Thailand have been previously interpreted in terms of strike-slip
faulting. However, many of the trends oblique to the N–S orientation of the rift system appear …

Scaled sandbox models were used to investigate the 4D evolution of pull-apart basins
formed above underlapping releasing stepovers in both pure strike-slip and transtensional …

We describe the structures and styles of deformation at the northeastern margin of the Adria
microplate during Miocene to recent times. Throughout the Miocene, deformation induced by …

Movements of tectonic plates often induce oblique deformation at divergent plate
boundaries. This is in striking contrast with traditional conceptual models of rifting and rifted …

Fission-track (FT) thermochronology has been applied to investigate the low-temperature
cooling and denudation history of the Patagonian Andes along the southern part of the intra …

Geometry of basins can indicate their tectonic origin whether they are small or large. The
basins of Bohai Gulf, South China Sea, East China Sea, Japan Sea, Andaman Sea, Okhotsk …

The southern Andes plate boundary zone records a protracted history of bulk
transpressional deformation during the Cenozoic, which has been causally related to either …

The structure of the Cordillera de Domeyko is dominated by a number of elongated N–S-
trending basement ridges. These ridges were uplifted by steep reverse N–S faults that …