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- ...[[Siberia]] both rose as the edge of Kazakhstania dove under the European plate. This event was the last stage in the assembly of [[Pangaea]].{{citation ne {{tectonics-stub}}2 KB (267 words) - 15:43, 27 April 2025
- ...s of the western continental margin zones of the Siberian craton ([[Angara Plate]]) on the north and the [[Kazakhstania|Kazakhstan craton]] on the south. ...ngara Plate, accreting some of the basalts and ultramafics onto the Angara Plate. [[Sial]]ic sediments were metamorphosed, melted and intruded into the rock7 KB (974 words) - 15:43, 27 April 2025
- ...lt]], which was formed by the collision of the Indian and Eurasian [[Plate tectonics|plates]] in the [[Cenozoic]] era. They are one of the longest mountain rang * [[Tectonics of the Tian Shan]]19 KB (2,743 words) - 15:43, 27 April 2025
- ...Ocean]], but became landlocked about 5.5 million years ago due to [[plate tectonics]].<ref name="irngaz"/> The [[Volga River]] (about 80% of the inflow) and th47 KB (6,905 words) - 15:44, 27 April 2025