In-situ trace elements and S isotopes of pyrite from the Twangiza and Misisi gold deposits, Kivu region, D.R. Congo: Implications for the evolution of the Kibaran Metallogenic System
Key Points
The analysis shows that trace elements in pyrite provide insights into the metallogenic system.
Key evidence includes the identification of specific sulfur isotopes, which enriches the understanding of mineral deposits.
Observational analysis across the Twangiza and Misisi deposits highlights variations in pyrite chemistry.
These findings suggest significant geological implications for understanding gold deposit formation.
In-situ trace elements and S isotopes of pyrite from the Twangiza and Misisi gold deposits, Kivu region, D.R. Congo: Implications for the evolution of the Kibaran Metallogenic System | Synapse