地质通报2024，Vol.43Issue(2)：246-257,12.DOI:10.12097/gbc.2022.04.048
桂西北箭猪坡铅-锌-锑多金属矿床成因:来自闪锌矿微量、稀土元素及氢氧同位素的证据
The genesis of the Jianzhupo Pb-Zn-Sb polymetallic deposit in northwestern Guangxi:Evidence from the characteristics of trace elements,rare earth elements,and hydrogen and oxygen isotopes of sphalerite
摘要
Abstract
The Danchi metallogenic belt,located in the northeast of the Youjiang basin,is an important non-ferrous metal ore concentration area in southern China,and the Jianzhupo deposit,the largest and most representative large-scale Pb-Zn-Sb polymetallic deposit in the Wuxu ore field in the southern section of the deposit,consisting of vein Pb-Zn-Sb orebody and newly discovered stratified Sn polymetallic orebody.In this paper,through the analysis of trace elements,rare earth elements,and H-O isotopes of sphalerite,the differences in metallogenic characteristics of the two types of ore bodies are compared and studied,and the source of ore-forming fluids and the genesis of deposits are further discussed.The results show that sphalerite in different types of ore bodies in the Jianzhupo deposit is relatively enriched in Fe,Cu,Pb,Sn and Sb,and depleted in Ga,Ge,Co and Ni,which is similar to typical magmatic hydrothermal deposits.Meanwhile,the total amount of rare earth in the stratified ore body(ΣREE=12.80×10-6～44.31×10-6)is higher than that in the vein ore body(ΣREE=3.34×10-6),with obvious LREE and HREE fractionation and Eu depletion.The results of H-O isotope analysis of sphalerite show that δD=-81.8‰～-69.2‰,δ18O=2.1‰～5.2‰(vein orebody);δD=-109.4‰～-75.2‰,δ18O=-4.0‰～4.0‰(stratified orebody),indicating that the ore-forming fluids of the two types of ore bodies are mixed fluids with different proportions of magmatic hydrothermal and atmospheric precipitation.The above characteristics show that the Jianzhupo deposit belongs to magmatic hydrothermal Pb-Zn deposit,and the ore-forming materials(fluids)of vein ore bodies and stratified ore bodies are mainly derived from magmatic hydrothermal fluid.关键词
箭猪坡矿床/闪锌矿/微量元素/稀土元素/氢-氧同位素/矿床成因/广西Key words
Jianzhupo deposit/sphalerite/trace elements/rare earth elements/hydrogen and oxygen isotopes/genesis of deposit/Guangxi分类
天文与地球科学引用本文复制引用
何光武,蔡明海,胡鹏飞,肖俊杰,甘能俭,朱敏杰,吕堂安..桂西北箭猪坡铅-锌-锑多金属矿床成因:来自闪锌矿微量、稀土元素及氢氧同位素的证据[J].地质通报,2024,43(2):246-257,12.基金项目
广西自然科学基金项目《广西大厂锡多金属矿成矿物质来源及成因研究》(编号:桂科计字[2020]159号) （编号:桂科计字[2020]159号）
