Gondwanaland lasted from the 650–500 Ma (late Neoproterozoic-Cambrian) amalgamation
of African and South American terranes to Antarctica–Australia–India through 320 Ma (mid …

Dedolomitization converts a dolomite into a calcite, and conventionally is interpreted to form
in an eogenetic or telogenetic diagenetic environment where meteoric water dissolves …

A detailed study of the structural and stratigraphic evolution of the Southern Permian Basin
during latest Carboniferous to Early Jurassic times, supported by quantitative subsidence …

The Permian Chert Event (PCE) was a 30 Ma long episode of unusual chert accumulation
along the northwest margin of Pangea, and possibly worldwide. The onset of the PCE …

The Variscan orogeny, resulting from the collision of Laurussia with Gondwana to form the
supercontinent of Pangaea, was followed by a period of crustal instability and re …

A 3D structural model of the Northeast German Basin was evaluated with special emphasis
on its evolution as an intracontinental depression. The study includes investigations on …

Inversion of sedimentary basins has been the subject of increasing research since the early
1980's. The kinematics of basin inversion, as well as the relationship between the …

The Central European Basin System (CEBS) is composed of a series of subbasins, the
largest of which are (1) the Norwegian–Danish Basin (2), the North German Basin extending …

Sedimentary basins host, among others, most of our energy and fresh-water resources: they
can be regarded as large geo-reactors in which many physical and chemical processes …

The Upper Permian Zechstein Supergroup has the potential to play an important role in the
UK's future energy production and energy transition. However the Supergroup is …