胶东半岛乳山邓格庄金矿带成矿期次探析
Analysis of Metallogenic Phases in the Denggezhuang Gold Belt, Rushan, Jiaodong Peninsula
DOI: 10.12677/ag.2025.155081, PDF,   
作者: 周进伟*, 兰占军, 计 煊:河北工程大学地球科学与工程学院,河北 邯郸
关键词: 邓格庄金矿带石英脉型金矿成矿期次Denggezhuang Gold Belt Quartz-Vein-Type Gold Deposit Metallogenic Stages
摘要: 邓格庄金矿带是胶东地区牟平–乳山一带的典型的石英脉型金矿带,其具有较高的金品位与储量,是研究胶东石英脉型金矿十分理想的场所。本研究将以邓格庄金矿带的成矿期次为研究方向,通过野外考察、镜下观察、能谱与电子探针数据分析等方法探究区域的多阶段成矿机制,同时为理解邓格庄金矿带的成矿机理以及找矿勘探提供必要的证据。研究表明,邓格庄金矿带成矿期次按时间先后划分为:(I)黄铁矿–石英阶段;(II)石英–黄铁矿阶段;(III)多金属硫化物阶段;(IV)石英–碳酸岩阶段。其中,黄铁矿是主要载金矿物,石英-黄铁矿阶段与多金属硫化物阶段是主要的金富集阶段。
Abstract: The Denggezhuang Gold Belt in the Muping-Rushan area of Jiaodong Peninsula represents a typical quartz-vein-type gold deposit system characterized by high gold grades and substantial reserves, making it an ideal subject for studying quartz-vein-type gold deposits in this region. This study investigates the metallogenic stages of the Denggezhuang Gold Belt through field investigations, microscopic observations, energy dispersive spectroscopy, and electron probe microanalysis to elucidate the multi-stage mineralization mechanisms and provide critical evidence for understanding ore-forming processes and exploration guidance. The results reveal four distinct metallogenic stages in chronological order: (I) pyrite-quartz stage, (II) quartz-pyrite stage, (III) polymetallic sulfide stage, and (IV) quartz-carbonate stage, with pyrite as the primary gold-bearing mineral and stages II-III representing the main gold enrichment phases.
文章引用:周进伟, 兰占军, 计煊. 胶东半岛乳山邓格庄金矿带成矿期次探析[J]. 地球科学前沿, 2025, 15(5): 848-857. https://doi.org/10.12677/ag.2025.155081

参考文献

[1] 刘俊来, 季雷, 倪金龙, 等. 早白垩世华北克拉通岩石圈减薄与破坏动力学: 兼论古太平洋型活动大陆边缘[J]. 地质学报, 2022, 96(10): 3360-3380.
[2] 宋明春, 宋英昕, 丁正江, 等. 胶东金矿床: 基本特征和主要争议[J]. 黄金科学技术, 2018, 26(4): 406-422.
[3] 杨立强, 邓军, 王中亮, 等. 胶东中生代金成矿系统[J]. 岩石学报, 2014, 30(9): 2447-2467.
[4] 胡芳芳, 范宏瑞, 沈昆, 等. 胶东乳山脉状金矿床成矿流体性质与演化[J]. 岩石学报, 2005, 21(5): 1329-1338.
[5] 梁辉, 韩作振, 王立功, 等. 胶东辽上金矿床的流体包裹体、氢-氧-碳-硫-铅同位素特征及矿床成因[J]. 地质通报, 2022, 41(6): 1053-1067.
[6] 林博磊. 吉林东部闹枝金矿成矿构造背景及矿床成因研究[D]: [硕士学位论文]. 长春: 吉林大学, 2013.
[7] Chai, P., Zhang, H., Dong, L. and Zhang, Z. (2019) Geology and Ore-Forming Fluids of the Dayingezhuang Gold Deposit, Jiaodong Peninsula, Eastern China: Implications for Mineral Exploration. Journal of Geochemical Exploration, 204, 224-239. [Google Scholar] [CrossRef
[8] Ma, W., Fan, H., Liu, X., Pirajno, F., Hu, F., Yang, K., et al. (2017) Geochronological Framework of the Xiadian Gold Deposit in the Jiaodong Province, China: Implications for the Timing of Gold Mineralization. Ore Geology Reviews, 86, 196-211. [Google Scholar] [CrossRef
[9] Li, Y., Li, S., Santosh, M., Liu, S., Zhang, L., Li, W., et al. (2015) Zircon Geochronology, Geochemistry and Stable Isotopes of the Wang’ershan Gold Deposit, Jiaodong Peninsula, China. Journal of Asian Earth Sciences, 113, 695-710. [Google Scholar] [CrossRef
[10] 江胜国. 山东胶东地区郭家岭花岗岩岩石地球化学特征及其意义[D]: [硕士学位论文]. 青岛: 山东科技大学, 2011.
[11] 王斌, 宋明春, 霍光, 等. 胶东晚中生代花岗岩的源区性质与构造环境演化及其对金成矿的启示[J]. 岩石矿物学杂志, 2021, 40(2): 288-320.
[12] 王立功, 祝德成, 郭瑞朋, 等. 胶西北仓上、三山岛岩体二长花岗岩地球化学、锆石U-Pb年龄及Lu-Hf同位素研究[J]. 地质学报, 2018, 92(10): 2081-2095.
[13] 罗贤冬, 杨晓勇, 段留安, 等. 胶北地块与金成矿有关的郭家岭岩体和上庄岩体年代学及地球化学研究[J]. 地质学报, 2014, 88(10): 1874-1888.
[14] 杨喜安, 赵国春, 宋玉波, 等. 胶东牟平-乳山成矿带拆离断层控矿特征及找矿方向[J]. 大地构造与成矿学, 2011, 35(3): 339-347.
[15] Sai, S., Deng, J., Qiu, K., Miggins, D.P. and Zhang, L. (2020) Textures of Auriferous Quartz-Sulfide Veins and 40ar/39ar Geochronology of the Rushan Gold Deposit: Implications for Processes of Ore-Fluid Infiltration in the Eastern Jiaodong Gold Province, China. Ore Geology Reviews, 117, Article ID: 103254. [Google Scholar] [CrossRef
[16] Deng, J., Liu, X., Wang, Q. and Pan, R. (2015) Origin of the Jiaodong-Type Xinli Gold Deposit, Jiaodong Peninsula, China: Constraints from Fluid Inclusion and C-D-O-S-Sr Isotope Compositions. Ore Geology Reviews, 65, 674-686. [Google Scholar] [CrossRef