Genesis and mineral exploration of the Daqishan Lead-Zinc Deposit, Beishan orogenic Belt, NW China: Constraints from In-Situ trace element compositions of Sphalerite, Pyrite, and Chalcopyrite | Synapse
March 3, 2026
Genesis and mineral exploration of the Daqishan Lead-Zinc Deposit, Beishan orogenic Belt, NW China: Constraints from In-Situ trace element compositions of Sphalerite, Pyrite, and Chalcopyrite
Key Points
The in-situ analysis of trace elements reveals critical mineral compositions at the Daqishan site, highlighting their role in deposit formation.
Sphalerite, pyrite, and chalcopyrite demonstrate distinct trace element signatures, which offer insights into the deposit's genesis in the Beishan region.
Using advanced techniques to analyze mineral samples enhances understanding of mineralization processes in orogenic belts.
These findings highlight the importance of trace element compositions for mineral exploration and understanding ore formation.