[HTML][HTML] The Mid-Variscan Allochthon: Keys from correlation, partial retrodeformation and plate-tectonic reconstruction to unlock the geometry of a non-cylindrical belt

JRM Catalán, K Schulmann, JF Ghienne - Earth-Science Reviews, 2021‏ - Elsevier
The non-cylindrical character of the Variscan Belt is established via a description of its most
salient geological characteristics and correlations among the main and relatively minor …

Palaeontological evidence bearing on global Ordovician–Silurian continental reconstructions

RA Fortey, LRM Cocks - Earth-Science Reviews, 2003‏ - Elsevier
The discreteness or otherwise of major Ordovician and Silurian terranes can be recognised
by the shallow-water benthic faunas which lived upon them. Their borders are often …

The mid-European segment of the Variscides: tectonostratigraphic units, terrane boundaries and plate tectonic evolution

W Franke - 2000‏ - pubs.geoscienceworld.org
The mid-European segment of the Variscides is a tectonic collage consisting of (from north
to south): Avalonia, a Silurian–early Devonian magmatic arc, members of the Armorican …

The pre-orogenic detrital zircon record of the Peri-Gondwanan crust

T Stephan, UWE Kroner, RL Romer - Geological Magazine, 2019‏ - cambridge.org
We present a statistical approach to data mining and quantitatively evaluating detrital age
spectra for sedimentary provenance analyses and palaeogeographic reconstructions …

Palaeozoic amalgamation of Central Europe: new results from recent geological and geophysical investigations

JA Winchester, Pace TMR Network Team - Tectonophysics, 2002‏ - Elsevier
Multidisciplinary studies of geotransects across the North European Plain and Southern
North Sea, and geological reexamination of the Variscides of the North Bohemian Massif …

The Frasnian/Famennian boundary interval in the South Polish–Moravian shelf basins: integrated event-stratigraphical approach

G Racki, M Racka, H Matyja… - Palaeogeography …, 2002‏ - Elsevier
The Late Devonian mass extinction event near the Frasnian/Famennian (F/F) boundary has
been analysed using conodont biostratigraphy and biofacies, sedimentology, magnetic …

Brunovistulian terrane (Bohemian Massif, Central Europe) from late Proterozoic to late Paleozoic: a review

J Kalvoda, O Bábek, O Fatka, J Leichmann… - International Journal of …, 2008‏ - Springer
The Brunovistulian terrane represents a microcontinent of enigmatic Proterozoic provenance
that was located at the southern margin of Baltica in the early Paleozoic. During the Variscan …

Palaeozoic amalgamation of Central Europe: an introduction and synthesis of new results from recent geological and geophysical investigations

JA Winchester, TC Pharaoh, J Verniers - 2002‏ - pubs.geoscienceworld.org
Multidisciplinary studies undertaken within the EU-funded PACE Network have permitted a
new 3-D reassessment of the relationships between the principal crustal blocks abutting …

Collage tectonics in the northeasternmost part of the Variscan Belt: the Sudetes, Bohemian Massif

P Aleksandrowski, S Mazur - Geological Society, London, Special …, 2002‏ - lyellcollection.org
A synthesis of published and new data is used to interpret the Sudetic segment of the
Variscan belt as having formed by the accretion of four major and two or three minor …

The late Palaeozoic relations between Gondwana and Laurussia

WS McKerrow, C Mac Niocaill, PE Ahlberg, G Clayton… - 2000‏ - pubs.geoscienceworld.org
Reconstructions based on biogeography, palaeomagnetism and facies distributions indicate
that, in later Palaeozoic time, there were no wide oceans separating the major continents …