Age relations for assembly of Gondwana and Pangea indicate that the timing of collisional
orogenesis between amalgamating continental bodies was synchronous with subduction …

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 …

Дано описание геологии Южного и Среднего Урала, облеченное в концентрированную
форму геодинамического анализа. В книге охарактеризована структура Урала, а также …

Neoproterozoic rocks in the Saxo-Thuringian part of Armorica formed in an active margin
setting and were overprinted during Cadomian orogenic processes at the northern margin of …

Saxo-Thuringia is classified as a tectonostratigraphic terrane belonging to the Armorican
Terrane Collage (Cadomia). As a former part of the Avalonian-Cadomian Orogenic Belt, it …

The Phanerozoic history of the Paleo-Asian, Tethyan, and Pacific oceanic domains is
important for unraveling the tectonic evolution of the Eurasian and Laurentian continents …

The Enganepe ophiolite, Polar Urals was formed at∼ 670 Ma and records a diverse
geochemical association of tholeiite, arc-tholeiite, adakite, and OIB-like lithologies. This …

The southern part of the Eastern European continental landmass consists mainly of a thick
platform of Vendian and younger sediments overlying Precambrian basement, referred to as …

The Paleozoic formations exposed to the West of the Main Uralian fault belonged to a
passive margin of Balica. The margin formed in the Early Paleozoic as a result of break-up of …

A study of U-Pb ages on detrital zircons derived from sedimentary sequences in the western
flank of Urals (para-autochthonous or autochthonous with Baltica) was undertaken in order …