Polygonal fault systems (PFS) are widely developed along many continental margin basins
and some interior cratonic and foreland basins. They are networks of small normal faults that …

Geological structure changes, including deformations and ruptures, developed in shallow
marine sediments are well recognized but were not systematically reviewed in previous …

We used scaled physical models to investigate how buried, dormant diapirs are rejuvenated
by lateral squeezing. In Stage 1, regional shortening increased the pressure of the source …

We present new evidence for the existence of a large pockmark field on the continental
slope of the Santos Basin, offshore southeast Brazil. A recent high-resolution multibeam …

This contribution describes the influence of diapirism and compressional tectonics in the
sedimentary record of the Estopanyà and Boix synclines (salt-walled basins) in the South …

We model the evolution of a salt diapir during sedimentation and study how deposition and
salt movement affect stresses close to the diapir. We model the salt as a solid visco-plastic …

Here, we document a suite of radial faults associated with hydrothermal vent complexes in
the Vøring Basin, offshore Norway. These complexes have pyramid-shaped, cylindrical-and …

Elastic full-waveform inversion (FWI) can provide accurate and high-resolution subsurface
parameters. However, its high computational cost prevents the application of this method to …

The largest condensate field of the Ordovician reef-shoal reservoirs, in China, was
discovered along the N° 1 fault zone in the Tarim Basin. However, current drilling activities …

We use a multiscale study to investigate the strain record in the continental sandstones-filled
minibasins of the Sivas Basin. Located on the central Anatolian Plateau, the Sivas basin is a …