Abstract
Based on the sulfur isotopic composition of sulfide minerals, gold deposits in terrigenous successions were systematized and grouped by variation ranges, intervals of modal values, and distribution of δ34S. It was concluded that the evolution of the sulfur isotopic composition of deposits depends on the character of changes in sulfur isotopes in the host rocks of the continental crust.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: 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.