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胶东蓬莱黑岚沟金矿床黄铁矿微区地球化学特征及对成矿流体的启示
引用本文:李秀章, 王勇军, 李衣鑫, 付乐兵, 张铭, 吴兴宇, 赵岩岩, 黄鑫, 徐昌, 孔凡顺. 胶东蓬莱黑岚沟金矿床黄铁矿微区地球化学特征及对成矿流体的启示[J]. 地质通报, 2022, 41(6): 1023-1038. doi: 10.12097/j.issn.1671-2552.2022.06.010
作者姓名:李秀章  王勇军  李衣鑫  付乐兵  张铭  吴兴宇  赵岩岩  黄鑫  徐昌  孔凡顺
作者单位:1.山东省地质调查院, 山东 济南 250013; 2.中国地质大学资源学院, 湖北 武汉 430074; 3.山东省煤田地质规划勘察研究院, 山东 济南 250104; 4.桂林理工大学地球科学学院, 广西 桂林 541004; 5.山东省煤田地质局物探测量队, 山东 济南 250104
基金项目:山东省地勘基金项目《莱州—招远地区构造岩相体系演化与成矿规律研究》(编号: 鲁勘字(2012)04号)、山东省自然科学基金项目《胶东栖霞-蓬莱成矿带典型金矿床成矿机制: 矿物微区地球化学制约》(编号: ZR2020MD031)、山东省地勘基金项目《山东省栖霞-蓬莱成矿带黑岚沟-大柳行金矿田深部成矿预测》(编号: 鲁勘字(2018)15号)、中国地质调查局项目《山东1∶5万大辛店幅、岗嵛幅、臧家庄幅、高疃幅矿产地质调查》(编号: DD20160044-1)和山东省自然科学基金项目《沂沭断裂带全新世断层活动特征及其构造意义》(编号: ZR2020MD039)
摘    要:胶东地区是中国最大的金矿集区, 金矿成因类型一直存在较大争议。黑岚沟金矿床是胶东蓬莱地区最大的金矿床, 曾以产出"明金"而闻名胶东。采用LA-ICP-MS方法分析黑岚沟金矿各成矿阶段黄铁矿中微量元素的组成、变化趋势及相关性, 探讨了Au的富集沉淀过程。通过野外地质调查, 结合矿相学和背散射图像观察, 将主成矿阶段(S1~S3)的黄铁矿(Py1~Py3)进一步划分为6个亚类; 通过微量元素分析发现, 研究区黄铁矿As含量高, 为富砷黄铁矿, 从早到晚, 黄铁矿中Cu、As、Ag、Au、Zn、Co、Ni、Pb、Sb、Bi等微量元素变化趋势不一致, As与Au在各阶段均呈现极强的正相关性, Cu-Zn、Ag-Sb等多对元素具有高的正相关性, Pb与Bi在Py1-1、Py2-1和Py2-2三个黄铁矿亚类中也具有较高的正相关性, 大部分黄铁矿亚类中Co与Ni存在正相关关系, Co/Ni元素含量比值为1.1~3.3, 说明黄铁矿主要为岩浆热液成因。黑岚沟金矿成矿流体是富Au-As流体, S1阶段与S3阶段微量元素相对富集, 说明成矿流体活动持续时间较长, 具有脉动式活动的特点, 金由多次活动的富Au-As流体多次沉淀成矿。

关 键 词:富砷黄铁矿   LA-ICP-MS   微量元素   地球化学   黑岚沟金矿床   胶东
收稿时间:2021-02-08
修稿时间:2021-06-11

Micro-geochemical characteristic of pyrites in the Heilangou gold deposit of penglai area and its implications for ore-forming fluid,Jiaodong gold province
LI Xiuzhang, WANG Yongjun, LI Yixin, FU Lebing, ZHANG Ming, WU Xingyu, ZHAO Yanyan, HUANG Xin, XU Chang, KONG Fanshun. Micro-geochemical characteristic of pyrites in the Heilangou gold deposit of penglai area and its implications for ore-forming fluid, Jiaodong gold province[J]. Geological Bulletin of China, 2022, 41(6): 1023-1038. doi: 10.12097/j.issn.1671-2552.2022.06.010
Authors:LI Xiuzhang  WANG Yongjun  LI Yixin  FU Lebing  ZHANG Ming  WU Xingyu  ZHAO Yanyan  HUANG Xin  XU Chang  KONG Fanshun
Affiliation:1.Shandong Institute of Geological Survey, Ji'nan 250013, Shandong, China; 2.Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, Hubei, China; 3.Shandong Coalfield Geological Planning Investigation Institute, Ji'nan 250104, Shandong, China; 4.College of Earth Sciences, Guilin University of Technology, Guilin 541004, Guangxi, China; 5.Geophysical Prospecting and Surveying Team of Shandong Bureau of Coal Geology, Ji'nan 250104, Shandong, China
Abstract:In China, the largest gold concentration area is Jiaodong, in which the genetic type of gold deposits has always been controversial.Heilangou gold deposit is the largest one in Penglai area of Jiaodong and was well-known for producing gold nugget.In this paper, LA-ICP-MS was used to analyze the composition, variation trend and correlation of trace elements in pyrite of Heilangou gold deposit, and to discuss the formation of Au.Through field investigation, combined with mineralogy and backscatter electron image(BSE), the pyrite(Py1~Py3)in the main metallogenic stage(S1~S3)is divided into six subtypes.Through trace element analysis, it is found that the change trends of Cu, As, Ag, Au, Zn, Co, Ni, Pb, Sb and Bi are inconsistent from early to later stage.As and Au show strong positive correlation in every pyrite subtype, Cu-Zn, Ag-Sb and several other element pairs have high correlation, Pb-Bi has an upper correlation especially in three subtypes of Py1-1, Py2-1 and Py2-2, and also Co-Ni in most pyrite subtypes.The Co/Ni ratio is mainly in the range of 1.1 ~ 3.3, which indicates that the pyrite is mainly of magmatic hydrothermal origin.The ore-forming fluid of Heilangou gold deposit is rich in Au-As, and the trace elements are relatively enriched in S1 and S3 stages, which indicates that the ore-forming fluid activity lasts for a relatively long time and has the pulsating characteristics.Gold is precipitated by the fluid rich in Au-As for multiple activities and several times.
Keywords:As-rich pyrite  LA-ICP-MS  trace element     Heilangou gold deposit  Jiaodong
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