Paleoproterozoic Kimberlites of the Lake Kimozero Area, Karelian Craton: Ore Mineralization in Kimberlites and Fault Zones


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Syngenetic and epigenetic ore mineralization was studied in Paleoproterozoic metakimberlites in the area of Kimozero Lake. In the Kimozero structure, redeposited ore mineralization is constrained to fracture and shear zones and consists of Fe-vaesite, Fe–Co-polydymite, millerite, Ni-pyrrhotite, pentlandite, chalcopyrite, Zn-bearing copper, galena, and Ni-pyrite. The composition of this mineralization is analogous to that of syngenetic mineralization in pyroclastic and coherent kimberlite, and its likely source was the kimberlite itself.

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O. Bogatikov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: alexandre-dokuchayev@yandex.ru
俄罗斯联邦, Moscow, 119017

A. Dokuchaev

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

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Email: alexandre-dokuchayev@yandex.ru
俄罗斯联邦, Moscow, 119017

A. Kargin

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: alexandre-dokuchayev@yandex.ru
俄罗斯联邦, Moscow, 119017

E. Yutkina

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: alexandre-dokuchayev@yandex.ru
俄罗斯联邦, Moscow, 119017

I. Kondrashov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: alexandre-dokuchayev@yandex.ru
俄罗斯联邦, Moscow, 119017

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