https://youtu.be/fvUjTH_VWvU

This research article from Ore Geology Reviews explores the origin of the Jiapigou gold deposit located in the North China Craton. By studying the composition and texture of pyrite, the authors investigated the mineralizing fluids and the processes involved in gold enrichment. They found evidence for two distinct pyrite types, each characterized by a specific trace element signature, which suggested that gold mineralization occurred in multiple stages. Fluid inclusion analysis revealed that the ore-forming fluids were low to moderate salinity, carbonic-aqueous compositions, and likely underwent boiling. The sulfur isotope data further supported the idea that the mineralizing fluids were derived from a crustal source. This study provides a detailed understanding of the Jiapigou gold deposit, highlighting the importance of fluid-rock interaction and the role of boiling in gold precipitation. P. Geo. Ricardo A Valls, M. Sc. and Geo Gadfly Valls Geoconsultant ORCID ID- https://orcid.org/0000-0002-5421-0914 Scopus Author ID: 7003369619/35335510700 ResearcherID: S-6604-2018 If you like this content, please "buy me a coffee" https://www.buymeacoffee.com/goldendroplets