Abstract
Zhazixi Sb–W deposit, where Sb and W coexist in different orebodies, features a unique metal association between the two minerals. This study aims to analyze the respective sources of Sb and W, through temperature measurement of fluid inclusions, laser-based Raman spectroscopy, as well as isotope test. The ore-forming fluid of Zhazixi Sb-W deposit was found to be a CO2-N2-H2O-NaCl system, which is rich in CO2 and N2. N2-rich inclusions and C, H, O isotopes were observed, indicating that the ore-forming fluid mainly comes from deep magmatic rocks, and secondarily from the metamorphic hydrothermal fluids. The detected S and Pb isotopes suggest that the ore-forming material stems from multiple sources. After comprehensive analysis of the geological features of the deposit and the local region, we believed that the Sb in Zhazixi Sb-W deposit stems from Banxi group, but W comes from the concealed rock body. The results provide a theoretical basis for the metallogenic research and prospecting direction of Xuefengshan metallogenic belt.
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.
