The descriptions of chondrichthyan microremains collected from several stratigraphic levels of the Devonian and Lower Carboniferous
of Belarus are presented in this paper.
1968, The Lower Carboniferous
of the Intra-Sudetic Basin; sedimentary, petrology and basin analysis.
Oxyprora irregulare (Koninck 1842), from the Lower Carboniferous
of Belgium and from the Lower Carboniferous
of the United Kingdom (Hind 1900), is similar to O.
This in turn can be correlated with the lower part of the Brigantian Stage of the Visean Series of the Mississippian (= Lower Carboniferous
in European terminology).
Devonian and Lower Carboniferous
conodonts of the Eurasia: Assemblages, zonal subdivisions, correlation of different facies sediments (Gladenkov, Yu.
Organic petrology and Rock-Eval analyses of the Lower Carboniferous
Emma Fiord Formation in the Sverdrup Basin, Canadian Arctic Archipelago.
Galmoy lies in the central midlands of Ireland, most of which is underlain by Lower Carboniferous
Limestones which are the host rock for previous major discoveries at Tynagh, Silvermines, and Tara.
Upper Devonian and Lower Carboniferous
bauxite deposits: Shugorskoye, Vostochnoye, Vezhayu-Vorykvinskoye, Timshersko-Puzlinskoye, Kedva-Vapovskoye, and some others are situated in the middle and southern Timan.
The Lower Carboniferous
period, lasting from 360 million to 320 million years ago, saw many important evolutionary changes in reptiles, amphibians and arthropods.
On the characteristics of the Upper Devonian and Lower Carboniferous
The well is located approximately 8 kilometers from Deep Well A5 and was planned to target the same structure as Deep Well A5 in the Middle and Lower Carboniferous
The oldest rocks in the CV are low-grade metamorphic rocks of Upper Devonian age overlied by lower Carboniferous
volcanic rocks with scarce sedimentary layers and upper Carboniferous clastic marine sediments.
Also notably absent as clasts, even in Windsor Group conglomerates, are Lower Carboniferous
gabbroic rocks of the Lennox Passage-St.
Moreover, these waves display dispersion, which is a consequence of the stratified overburden of the Lower Carboniferous
Culm facies sediments, e.