In the Carboniferous, terrestrial vegetation became widespread, diverse and abundant. The
resulting fossil record has proved to be an effective biostratigraphic tool for intra-and …

Wetland forests, known as coal forests, extended over large areas of the palaeotropics
during the Late Carboniferous and the Permian Periods. They were initiated during the …

Abstract Five U-Pb CA-ID-TIMS high-precision ages were obtained from single zircon
crystals separated from tuffs or ignimbrites embedded in Pennsylvanian to Asselian …

The Žacléř coalfield in the western part of the Intra-Sudetic Basin is an example of coal
accumulation in an alluvial valley deposited under a long-term (~ 3 my) stable tectonic …

Old and new, well and poorly known lithofacies data of Moscovian and Artinskian age in the
area limited by the Arctic Sea and central Africa, the Atlantic Ocean and the Ural Mountains …

A synthesis of the upper Moscovian sedimentological and palaeontological record of
terrestrial habitats across the Variscan foreland and adjacent intramontane basins (an area …

The Polish part of the Central European Variscan foreland includes several regional units
that differ in crustal structure and are characterized by distinct Devonian to Carboniferous …

Gaseous emissions from seven self-heating coal waste dumps in two large coal mining
basins, Upper and Lower Silesia (Poland), were investigated by gas chromatography (GC …

Abstract The Serpukhovian (Namurian A) stratigraphy of the Ostrava Formation, Upper
Silesian Coal Basin, Czech Republic, consists of coal-bearing paralic sediments underlain …

Abstract The Intra-Sudetic Basin is essentially a post-orogenic (Variscan) continental basin
with a depositional history that ranges from the late Viséan to the Triassic. The fossil record …