Zonality and ore occurrence of exocontact hydrothermal-metasomatic formations of the Kolomeitsev granite massif (Central Taymyr)
Abstract
Since the 70's in the north of the Central Taymir, considerable attention has been paid to quartz and carbonate-quartz veins with polysulfide mineralization, which is due to the isolation in the Taymir quartz (sulfide)-gold ore formation.
Область исследования:
(Archived) Without section
References
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