Hydrogen is expected to play a key role in the future as a clean energy source that can
mitigate global warming. It can also contribute significantly to reducing the imbalance …

Salt tectonics at passive margins is currently interpreted as a gravity-driven process but
according to two different types of models: i) pure spreading only driven by differential …

Salt flows downslope, irrespective of overburden. In salt basins on passive margins, the salt
will tilt and flow towards the ocean immediately after continental rifting has ended due to …

Evidence of salt movement prior to the main Zagros folding event lead us to question: 1. The
role of pre-existing salt structures on the Zagros fold and thrust belt development; 2. The …

The Central North Sea lies within the North Permian evaporite Basin, which was largely
flexural but with locally significant basement faults. While the main evaporite basin fill is …

Abstract The North Sea Basin contains a widespread Permian salt layer that reached a
depositional thickness of c. 1 km in the basin centre. This layer profoundly affected structural …

Existing models for the initiation of salt withdrawal minibasins focus on the role of triggers
that exist within the minibasin, either stratigraphic (eg differential deposition) or tectonic …

Abstract The Guadalquivir Basin is the Neogene foreland basin of the central and western
Betic thrust belt in southern Spain. At the boundary between the basin and the outcrops of …

The Levantine Basin in the South-eastern Mediterranean Sea is a world class site for
studying the initial stages of salt tectonics driven by differential sediment load, because the …

New regional (two-dimensional) seismic reflection data, published Deep-Sea Drilling Project–
Ocean Drilling Program reports, and unpublished shallow-offshore well information …