Genesis of fahlore in the Tianbaoshan lead–zinc deposit, Sichuan Province, China: a scanning electro

• 作者: Yusi Hu Lin Ye Zhenli Li Zhilong Huang Jiawei Zhang
• 学科: 地球科学
• 关键词: Fahlore Tianbaoshan Pb–Zn deposit SEM– EDS MVT deposit
• 年，卷（期）: 2022,（6）
• 页码范围: 842-853
• 页数: 11页
• 语种: 英文
• DOI: 10.1007/s11631-018-0280-9

摘要

The Tianbaoshan deposit, located in the southwestern part of the Yangtze Block, is a representative Pb–Zn deposit in the Sichuan–Yunnan–Guizhou Pb–Zn metallogenic province. The Pb–Zn orebodies are hosted in the upper Sinian Dengying Formation dolostone. The predominant minerals are sphalerite, galena, pyrite, chalcopyrite, quartz, and calcite with minor arsenopyrite, fahlore, and dolomite. The deposit is characterized by relatively strong Cu mineralization. However, the relationship between Pb–Zn and Cu mineralization is unknown. We analyzed the mineralogy and composition of fahlore, chalcopyrite, arsenopyrite, sphalerite, and galena using scanning electron microscopy–energy dispersive spectroscopy, with the aim of providing new evidence for the genesis of the Pb–Zn–(Cu) ore. The results show that the Cu ore in the deposit is dominated by chalcopyrite and fahlore, both of which formed before or during the Pb–Zn ore-forming stage. The fahlore showed dramatic compositional variation and was characterized by negative correlations between Ag and Cu, and between As and Sb, suggesting substitution of Ag for Cu, and that As and Sb substitute in the same site in the fahlore lattice. Based on backscattered electron images and composition, the fahlore was divided into two types. Type Ⅰ fahlore crystallized early and is characterized by enrichment of Cu and depletion in Ag and Sb. Type Ⅱ fahlore formed after Type Ⅰ, and is rich in Ag and poor in Cu and As. Moreover, galena and fahlore are the host minerals of Ag. The variation of valence state with As host mineral—from fahlore to arsenopyrite—indicates the metallogenic environment changed from relatively oxidizing to reducing with a high pH. In the light of Gibbs energies of reciprocal reactions and isotherms for cation exchange, the composition of the fahlore implies its ore-forming temperature was lower than 220℃, corresponding with typical Mississippi Valley-type (MVT) deposits. Based on the geologic character and geochemi