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Vorobieva S.V. GEOLOGIC-STRUCTURAL POSITION OF COMPLEX SULFIDE ORE BEDS IN THE ZONE OF JOINT OF MAGNITOGORSKY FLEXURE AND EAST-URAL RISE The allocation of ore centres in the indicated region is linear- zoned. Geologic-structural position of ore beds are controlled with deep permeable zones in a framing of granite and gneiss rises. Tectonic zones have a character of main slide-thrust and discharge-displacement zones. Morphologically difficult sulfide beds are localized on the parts of paleovolcanic depressions, formed in a middle palaeozoic. Ore bodies connect with protovolcanic horst-anticlinal structures spatially. Perspective parts are taken place on the slopes of horst-anticlinal rises, permeated with granitoids of Magnitogorsky intrusive complex.
About this article
Author: Vorobyeva S.V.
Year: 2004
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Editor-in-chief |
Sergey Aleksandrovich
MIROSHNIKOV |
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