Abstract The Late Paleozoic Ice Age (LPIA) was the penultimate major glaciation of the
Phanerozoic. Published compilations indicate it occurred in two main phases, one centered …

Late to post-Variscan molassic basins of Late Pennsylvanian-Permian age are exposed in
Sardinia (Italy). Here, the compositional and stratigraphic evolution of the Mulargia …

Abstract The Variscan Bohemian Massif reveals evidence for two oceans. The Saxo-
Thuringian basin separated the microcontinents Franconia-Thuringia (N-Armorica) and …

Volcanic particles have particular geodynamic significance. Despite abundant datasets on
volcanic-derived sand (stone), the distinction between spatial and temporal distribution of …

Abstract In the northern Iberian Peninsula, the Pyrenean-Cantabrian orogenic belt extends
EW for ca. 1000 km between the Atlantic Ocean and Mediterranean Sea. This orogen …

Abstract In Europe, North Africa and Asia Minor, the remains of Pennsylvanian sedimentary
basins bearing continental deposits either intimately mixed with shallow-marine strata or …

A long and detailed pole path has been defined from ignimbritic successions across the
Tamworth Belt forearc basin of a Carboniferous continental arc in the southern New England …

The evolution of eruptive vents related to calderas is not fully understood. We focus on a
structural, rock-magnetic and geochemical investigation of a 314 Ma rhyolite dyke swarm …

We present new zircon U–Pb chemical abrasion–isotope dilution–thermal ionization mass
spectrometry (CA–ID–TIMS) ages of two Late Carboniferous–early Permian continental …

Palaeo-loess and silty aeolian-marine strata are well recognized across the Carboniferous–
Permian of equatorial Pangaea. Aeolian-transported dust and loess appear in the Late …