| UDC 551.24-552.31(571.6) |
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Different-Order Late Mesozoic Structures of Tectonomagmatic Activization in the Verkhoayn-Chukotian Folded Area |
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| © 2006 V. M. Kuznetsov |
| Federal State Unitary Enterprise "Magadangeology", Magadan |
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| Tectonomagmatic processes became active in the territory of the Verkhoyan-Chukotian Folded Area in late Mesozoic. This was due to developing volcanoplutonic belts related to different blocks of the Earth’s crust there. The belt rims have perivolcanic zones with indistinct limits, which display indications of magmatism and mineralizations. There are linear zones of tectonomagmatic activity, which are the typomorphic units and serve as important ore-control structures. |
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| Keywords: tectonomagmatic activity, the Earth’s crust blocks, volcanoplutonic belts, deep faults, granitoid massifs, mineralization. |
| Full text [In Russian] |
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