Abstract
The author suggests a hypothesis of multistage evolution of the mobile crust zones of the Earth, taking into consideration the type of crustal columnar section (oceanic, intermediate, continental, and orogenic), the history of tectonic and magmatic epochs (Caledonian, Hercynian, Kimmeridgian, and Alpine), and the factor of lineament type mobile zones existing during long periods of geological history and contributing to the activation of magmaticprocesses. --E.A. Alexandrov.
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