The Variscan orogeny occurred as a result of the Late Devonian to Late Carboniferous
collision and accretion of Gondwana-derived microcontinents and continental masses with …

Abstract The Alps and Western Carpathians constitute that part of the Alpine-Mediterranean
orogenic belt which advances furthest to the north into Central Europe. They were formed by …

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 …

How can inorganic geochemical data from terrestrial deposits be used as a provenance
tool? We demonstrate a new approach as earlier studies have focused on marine deposits …

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 …

Abstract The Permian Ora Formation (277–274 Ma) preserves the products of the Ora
caldera 'super-eruption', Northern Italy. The stratigraphic architecture of the exceptionally …

Coal petrology data and vitrinite reflectance modelling were combined with micro-
geochemical and fluid inclusion analyses of coal mineralization and apatite fission track …

Fossil shark remains occur in both marine and nonmarine Late Palaeozoic deposits,
therefore their palaeoecology is controversial. The oxygen and strontium isotopic …

Abstract The latest Permian and Triassic salt basins resulted from widespread aridity and
progressive rifting across equatorial Pangea. Rift propagation into the continental interior …

The north‐western Alpine foreland in Switzerland and France comprises the Late Miocene
Jura Mountains, considered a type example for thin‐skinned thrusting where deformation of …