山东莱州曲家金矿黄铁矿微量元素对成矿过程的指示*
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山东省地质科学研究院

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国家重点研发计划“蚀变岩型金矿立体地球化学探测试验示范”(2016YFC0600606)


Trace Element Characteristics of Pyrite in Qujia gold Deposit ,Laizhou,Shandong Province and Its Implication on Metallogenic Process
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Shandong Institute of Geological Sciences,Key Laboratory of Gold Mineralization Processes and Resource Utilization of Ministry of Natural Resources,Key Laboratory of Metallogenic Geological Processes and Resource Utilization in Shandong Province,Jinan

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    摘要:

    摘 要: 曲家金矿位于我国重要的蚀变岩型金矿矿集区之焦家金矿带的中段,矿床赋存标高为-726m~-1334m。为研究黄铁矿的演化及其对金成矿过程的指示,运用LA-ICP-MS分析黄铁矿原位微量元素含量,结合岩相学观察和点群分析对黄铁矿进行了分类。发现黄铁矿中Co、Ni、As等微量元素主要以类质同像形式赋存,而Au、Ag、Cu、Zn、Pb、Bi等元素主要以纳米级、微米级矿物包裹体形式赋存。黄铁矿主要分为5种类型,富Co型Py1,富Ni型Py2,富Au、As型Py3和富Au、Ag、Pb、Bi型Py4及“干净”型Py5。黄铁矿微量元素特征 指示成矿物质可能主要来源于前寒武纪变质基底岩石和中生代岩浆岩,少量来源于地幔,成矿热液可能属变质热液、岩浆热液、浅部大气降水的混合成因。不同类型黄铁矿反映成矿热液由富Co、Ni经富As、Au向富Pb、Bi、Au、Ag演化。Py1和Py2形成后受构造活动影响发生强烈破碎,裂隙表面对热液中金络合物增强的吸附作用,促使金在裂隙中沉淀,对金的富集成矿可能起重要作用。 Co、Ni含量较低,同时Au、Ag、As、Pb、Bi等元素含量较高的黄铁矿与成矿作用有密切关系。另外,黄铁矿中Co、Ni含量较高,但破碎强烈,成矿相关元素含量较高为黄铁矿在早期形成并被后期成矿作用改造的特征。

    Abstract:

    Abstract: Qujia gold deposit is located in the middle of Jiaojia gold deposit belt, which is an important altered rock type gold ore concentration area in China. and the elevation of the deposit is -726 m ~ -1334 m. In order to study the evolution of pyrite and its indication of the gold mineralization process, LA-ICP-MS was used to analyze the in-situ trace element content of pyrite, and, and the pyrite was classified by petrographic observation and cluster analysis.It is found that the trace elements such as Co, Ni and As in pyrite are mainly in the form of isomorphism, while elements such as Au, Ag, Cu, Zn, Pb and Bi are mainly in the form of nano-scale and micro-scale mineral inclusions. Pyrite is mainly divided into five types, Co-rich Py1, Ni-rich Py2, Au and As-rich Py3, Au, Ag, Pb, Bi-rich Py4 and 'clean 'Py5. The characteristics of trace elements of pyrite indicate that the ore-forming material may be mainly derived from the Precambrian metamorphic basement rocks and Mesozoic magmatic rocks, and a small amount from the mantle. The ore-forming hydrothermal solution may be a mixed genesis of metamorphic hydrothermal solution, magmatic hydrothermal solution and shallow atmospheric precipitation. Different types of pyrite reflect the evolution of ore-forming hydrothermal fluid from rich Co and Ni to rich As and Au to rich Pb, Bi, Au and Ag. After the formation of Py1 and Py2, they were strongly broken by tectonic activities, the enhanced adsorption of gold complexes in hydrothermal fluid on the fracture surface promotes the precipitation of gold in fractures, which may play an important role in the enrichment and mineralization of gold. The low content of Co and Ni in pyrite and the high content of Au, Ag, As, Pb and Bi in pyrite are closely related to mineralization. In addition, the content of Co and Ni in pyrite is high, but the crushing is strong, and the content of ore-forming related elements is high, which are the characteristics of pyrite formed in the early stage and transformed by the later mineralization.

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  • 收稿日期:2023-06-14
  • 最后修改日期:2023-10-06
  • 录用日期:2023-10-31
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