Ореольні води ртутних рудних полів Донбасу як результат еволюції гідротермальних систем
DOI :
https://doi.org/10.15587/2313-8416.2018.143613Mots-clés :
ореольні води, флюїди, гідротермальна система, рудне поле, рудна мінералізація, гідрогеохімічні асоціаціїRésumé
Розглянуто фактори та процеси формування ореольних вод гідротермальних рудних полів Донбасу як результат еволюції гідротемальних систем на постгідротермальному етапі їхнього розвитку.
Встановлено, що ці води утворюються на ділянках активного тепломасоперенесення по зонах розломів. Визначено, що у формуванні ореольних вод гідротермальних родовищ приймають участь інфільтраційні води зони вільного водообміну, напірні води глибоких горизонтів та ендогенні флюїди
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