PROTEROZOIC TECTONO-MAGMATIC ACTIVISATION AND GOLD MINERALISATION IN WESTERN PART OF KIROVOGRADSK BLOCK (OVRAZHNY ORE MANIFESTATION OF LYPNIZHKA STRUCTURE AS AN EXAMPLE)
Abstract
This article discusses data on common mechanism of ore formation in Lypnyazka structure, that caused by regional processes of tectono-magmatic activization at 2000 ± 100 Ma. Proterozoic activization resulted in bulk mobilisation and migration of ore forming elements from sites of magma generation to the exocontact zones of carbonaceous metamorphic rocks distribution.
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Copyright (c) 2025 О. В. ГРІНЧЕНКО, С. М. БОНДАРЕНКО, Б. М. ІВАНОВ, В. О. СЬОМКА, В. С. РЯБОКІНЬ, І. М. БОНДАРЕНКО

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