The Osning Thrust is one of the major fault systems in Central Europe, with a length of
approximately 115 km. It underwent a polyphase tectonic evolution in the Mesozoic that …

The deformation and uplifting history of the Qinghai–Tibet Plateau is a controversial issue,
and so far there has been insufficient evidence for interpretation. Investigations of the …

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 …

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 …

Geologists agree that the collision of the Indian and Asian plates caused uplift of the Tibet
Plateau. However, controversy still exists regarding the modes and mechanisms of the …

Several selected seismic lines are used to show and compare the modes of Late-
Cretaceous–Early Tertiary inversion within the North German and Polish basins. These …

Abstract Subsequent to the Variscan Orogeny, the lithosphere of Central Europe was
subjected to a series of tectonic events in the Latest Palaeozoic and Mesozoic which were …

Lower Cretaceous early syn‐rift facies along the eastern flank of the Eastern Cordillera of
Colombia, their provenance, and structural context, reveal the complex interactions between …