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Randell Stephenson

Researcher at University of Aberdeen

Publications -  198
Citations -  7130

Randell Stephenson is an academic researcher from University of Aberdeen. The author has contributed to research in topics: Rift & Sedimentary basin. The author has an hindex of 48, co-authored 196 publications receiving 6538 citations. Previous affiliations of Randell Stephenson include University of Amsterdam & Geological Survey of Canada.

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Late Precambrian to Triassic history of the East European Craton: dynamics of sedimentary basin evolution

TL;DR: The East European Craton was affected by rift phases during Early, Middle and Late Riphean, early Vendian, early Palaeozoic, Early Devonian and Middle-Late Devonian times and again at the transition from the Carboniferous to the Permian and the permian to the Triassic as discussed by the authors.
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European Lithosphere Dynamics

TL;DR: The European Litosphere Dynamics (ELEOPROBE) project as mentioned in this paper was a field laboratory for studying lithospheric processes through time, for tracing tectonic evolution of crust and mantle from the present far back into the early Precambrian.
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On the origin of the southern Permian Basin, Central Europe.

TL;DR: In this article, a detailed study of the structural and stratigraphic evolution of the Southern Permian Basin during Carboniferous to Early Jurassic times, supported by quantitative subsidence analyses and forward basin modelling for 25 wells, leads to modify the conventional model for the Rotliegend-Zechstein development of this basin.
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Late Vendian–Early Palæozoic tectonic evolution of the Baltic Basin: regional tectonic implications from subsidence analysis

TL;DR: Subsidence analysis was performed on 43 boreholes penetrating the Upper Vendian-Lower Palaeozoic sedimentary succession of the Baltic Basin this paper, and the results were related to lithofacial and structural data to elucidate subsidence mechanisms and the regional tectonic setting of basin development.
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Tectonic evolution of the mid-polish trough : modelling implications and significance for central european geology

TL;DR: In this paper, the depocentral axis of the Polish Basin, the mid-Polish Trough (MPT), is superimposed on the boundary between the west European Phanerozoic and east European Proterozoic crustal domains, within the Trans-European Suture Zone.