Lopian orogeny

Archean orogeny

The Lopian orogeny (also known as the Rebolian orogeny) was a mountain building event that affected the Baltic Shield during the Archean, between 2.9 and 2.6 billion years ago. The Kola-Belomorian gneiss and Karelian granitoid-greenstone terrane both formed during this time.^[1]^[2]

References

^ Gaal, G. & Gorbatschev, R. (1987). "An Outline of the precambrian evolution of the baltic shield". Precambrian Research. 35: 15–52. Bibcode:1987PreR...35...15G. doi:10.1016/0301-9268(87)90044-1.{{cite journal}}: CS1 maint: multiple names: authors list (link)
^ Goodwin, A. (1991). Precambrian Geology: The Dynamic Evolution of the Continental Crust. Academic Press. p. 582. ISBN 9781483288550.

Geology of Europe

Countries

Albania
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Geologic regions

Orogens	Acadian Alpine Belomorian Cadomian Caledonian Carpathian Dalslandian Gothian Grampian Hallandian-Danopolonian Hellenic Laxfordian Lopian Saamian Scandian Scourian Timanide Svecofennian Sveconorwegian Uralian Variscan
Mountain ranges	Alps Apennines Caucasus Dinaric Alps Harz Massif Central Ore Mountains Pyrenees Scandinavian Mountains Sudetes Urals Western Carpathians
Oceanic basins	Atlantic Ocean Arctic Ocean Bay of Biscay Black Sea Mediterranean Sea Norwegian Sea
Intracontinental basins and grabens	Aquitaine Basin Barents Basin Baltic Sea Basin Central Lowlands Dnieper–Donets Rift Ebro Basin European Cenozoic Rift System Hellenic Trench Limagne Graben Mezen Basin Molasse Basin Moscow Basin North Sea Basin Oslo Rift Pannonian Basin Paris Basin Peri-Caspian Depression Timan-Pechora Basin White Sea Rift System
Tectonic plates and microcontinents	Adriatic Plate Aegean Sea Plate Anatolian Plate Eurasian Plate Iberian Plate Jan Mayen Microcontinent Moesian Plate Pelso Plate Tisza Plate
Terranes	Armorican terrane Avalonia Baltica Cimmeria East European Craton Fennoscandian Craton Sarmatian Craton Volgo–Uralia