矿床地质2023，Vol.42Issue(6)：1266-1284,19.DOI:10.16111/j.0258-7106.2023.06.011
塞尔维亚Mali Krivelj斑岩型铜矿床热液蚀变作用及元素迁移规律
Hydrothermal alteration and elements migration features of Mali Krivelj porphyry copper deposit in Bor metallogenic belt,Serbia
摘要
Abstract
The Mali Krivelj porphyry copper deposit is located in the Bor metallogenic belt in the western segment of the Tethyan metallogenic domain.Typical samples of fresh andesite and rocks in different alteration zones are col-lected for the trace element testing and element mass-balance calculation to research the hydrothermal alteration and elements migration during mineralization.The analytical results show that the phyllic zone and the chlorite-sericite alteration zone have similar elemental migration laws,Sr,Ba,Zr,Th,U,Ti,Co,Ni and REE elements emi-grate in a certain degree,while Rb,Cs and other elements migrate in a certain degree,a large number of magnetite develops in the chlorite-sericite zone,while a large number of quartz + sericite + pyrite occur in the phyllic zone.All of these show that the fluid reducibility gradually increases with the continuous evolution of the fluid.The al-teration in propylitic zone is weak,and the overall elemental migration is not high.Cu has a good positive correla-tion with Cr,Rb,Ti/Sr,Rb/Ba and Cr/Zn,and a certain degree of negative correlation with REE,Ba,Zn,Mn and Sr,which indicates that the whole rock element migration law of porphyry deposits can also be used as geochemi-cal exploration indicators to a certain extent,and provides support for finding porphyry mineralization center.关键词
斑岩型矿床/热液蚀变作用/元素迁移/Isocon分析/Bor成矿带Key words
porphyry deposit/hydrothermal alteration/elements migration/isocon analysis/Bor metallogen-ic belt分类
天文与地球科学引用本文复制引用
谭威,曾育龙,林明钟,曾兴宝,林荣添,郭红乐..塞尔维亚Mali Krivelj斑岩型铜矿床热液蚀变作用及元素迁移规律[J].矿床地质,2023,42(6):1266-1284,19.基金项目
本文得到紫金集团塞尔维亚波尔市Mali Krivelj铜矿补充勘查项目、塞尔维亚Bor-Majdanpek矿集区斑岩-浅成地温热液铜金多金属矿床成矿规律研究及靶区验证项目共同资助 （）
