Abstract
The localization conditions for the large Sovinoe gold-quartz deposit were clarified based on results of the geological exploration. It has been ascertained that the vein- and stockwork-type ore bodies are confined to gentle ttectonic nappe zones in sites where they are crossed by steeply dipping faults. Ore deposition occurred under conditions of long-term tectonic movements, with participation of gold-bearing fluids enriched in methane and carbon dioxide, coming from deep-seated magmatic chambers at the stage of the orogen activation. The fluid flow was confined to deep-seated faults and represented the main factor for the transformation of tectonized terrigenous-sedimentary rocks into carbonaceous shales and for the formation of quartz-veined gold mineralization.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
