К проблеме рудоносности черных сланцев Вишерско-Кутимского антиклинория (Северный Урал)

G. A. Petrov, V. A. Aleksandrov, A. I. Zubkov, A. V. Maslov, Yu. L. Ronkin

Аннотация


В пределах Вишерско-Кутимского антиклинория известны рудопроявления золота, пространственно сопряженные с россыпными месторождениями. Исследование рудных минералов показало наличие большого разнообразия сульфидов, сульфоарсенидов, теллуридов и самородных элементов (в том числе благородных металлов), кристаллизовавшихся в несколько стадий. Выделены две перспективные площади в ранге прогнозируемых золоторудных узлов – Мартайский узел и Верхневагранская зона, расположенные над погребенными гранитными массивами, предполагаемыми по геофизическим данным. Изучение особенностей локализации и состава золоторудной минерализации позволяет предположить возможность присутствия здесь золоторудных месторождений сухоложского типа.

Ключевые слова


Северный Урал; Вишерско-Кутимский антиклинорий; черные сланцы; золото

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Литература


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DOI: http://dx.doi.org/10.17072/psu.geol.29.32

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