Role of water/rock interaction in the formation of ore-bearing solutions and deposition of hydrothermal ore, Sadon Mining  District, North Caucasus Mountains

Авторы: Borisov M., Bychkov D., Volkova M., Shvarov Yu
Сборник: 16th International Symposium on Water-Rock Interaction (WRI-16) and 13th International Symposium on Applied Isotope Geochemistry (1st IAGC International Conference) E3S Web Conf. Volume 98
Том: 98
Год издания: 2019
Издательство: EDP Sciences
Местоположение издательства: France
Первая страница: 1
Последняя страница: 5
DOI: 10.1051/e3sconf/20199805003
Аннотация: REE distribution patterns of the ores and host rocks of the Dzhimidon vein lead-zinc deposit (North Caucasus, Ossetia, Sadon mining district, Russia) have been analyzed to elucidate the source(s) of hydrothermal ore deposits. Two types of prevailing rocks are involved in ore formation - Paleozoic granites (the main ore-hosting rocks at the majority of deposits) and Precambrian schists (specific only the for host rocks of the Dzhimidon deposit). The source of ore components tends to be complex and includes host rocks in variable proportions that could be characterized by REE distribution in ores. Interaction of water with combined sources was thermodynamically modeled. Critical differences were found in the ore-forming models, with variable sequence and rock proportions during interaction with barren fluid.
Добавил в систему: Борисов Михаил Васильевич

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