Peculiarities of the Kinematics of the South Uralian Suture Zones as a Cause of the Formation of the Convergent Structure of the East Uralian Megazoneстатья
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Дата последнего поиска статьи во внешних источниках: 28 мая 2015 г.
Аннотация:This article deals with structure of suture zones, bordering the East-Ural megazone of the South Urals. Analysis of mesoscale structures allowed to prove the strike-slip nature of suture zones. Their kinematics was changed from left-sided in the Early Carboniferous to the right-sided in the Mesozoic. The age of these dislocations is determined by the age of synkinematical intrusions. The suture zones are of divergent structure, so the East-Ural megazone located between has the opposite, convergent structure.