The kinematic evolution of the Pyrenees was largely controlled by structural and thermal
heterogeneities inherited from a precursor rift system, resulting in complex along-strike …

Basin inversion involves the reversal of subsidence in a basin due to compressional tectonic
forces, leading to uplift of the basin's sedimentary infill. A thorough understanding of basin …

Salt tectonics is the study of how and why salt structures evolve and the three-dimensional
forms that result. A fascinating branch of geology in itself, salt tectonics is also vitally …

Defining the structural style of fold–thrust belts and understanding the controlling factors are
necessary steps towards prediction of their long-term and short-term dynamics, including …

Sedimentologic and tectonic records in the Qiangtang Basin, northern Tibet, indicate a
negative basin inversion during the Late Triassic, which reveals Paleo-Tethys closure and …

Common basin models assume that the post‐rift tectonic evolution of most basins is usually
associated with tectonic quiescence. However, tectonic inversion during the post‐rift phase …

Basement inherited structures represent a significant factor affecting thrust propagation
dynamics during the growth of fold-and-thrust belts. In this study inspirited from seismic data …

Inverted structures provide traps for petroleum exploration, typically four-way structural
closures. As to the degree of inversion, based on a large number of worldwide examples …

It is generally accepted that the subduction polarity reversal (SPR) results from the strong
collision of two plates. Yet, the SPR of the Solomon Back‐arc Basin is started in the “soft …

The same sense movement on any given fault plane occurs much more frequently
compared to the cases when the sense reverses. Therefore, positive or negative structural …