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黄金科学技术 ›› 2018, Vol. 26 ›› Issue (3): 279-288.doi: 10.11872/j.issn.1005-2518.2018.03.279

• 矿产勘查与资源评价 • 上一篇    下一篇

山东牟平阎家疃金矿床地质特征及成因探讨

张琪彬,张朋,徐忠华,刘向东,张亮亮,王斌,王珊珊   

  1. 山东省第六地质矿产勘查院,山东 威海 264209
  • 收稿日期:2017-11-21 修回日期:2018-01-08 出版日期:2018-06-30 发布日期:2018-07-28
  • 作者简介:张琪彬(1987-),男,山东东平人,硕士研究生,从事金矿勘查和相关研究工作。zqb11758@163.com
  • 基金资助:
    山东省重大科技创新工程“深部金矿资源评价理论、方法与预测”(编号:2017CXGC1604)和山东省泰山学者建设工程专项经费“胶东型金矿的构造岩浆背景和深部找矿关键技术”(编号:ts201511076)联合资助

Geological Characteristics and Genesis of Yanjiatuan Gold Deposit in Muping,Shandong Province

ZHANG Qibin,ZHANG Peng,XU Zhonghua,LIU Xiangdong,ZHANG Liangliang,WANG Bin,WANG Shanshan   

  1. Shandong 6th Geology&Mineral Resources Survey Institute,Weihai 264209,Shandong,China
  • Received:2017-11-21 Revised:2018-01-08 Online:2018-06-30 Published:2018-07-28

摘要: 阎家疃金矿床位于胶东三大金成矿带中的牟平—乳山金成矿带,是鹊山岩体中受小规模SN、NNE向断裂控制的破碎带蚀变岩型和硫化物石英脉型复合型金矿床。通过矿相学和电子探针分析,对阎家疃金矿床矿石金属矿物特征和金矿物赋存状态进行研究,确定了金属矿物的共生组合及其生成顺序。发现金矿物大部分为粒径<0.074 mm的中细粒金,赋存状态以粒间金为主,包裹金次之。金矿物的成色高于牟平—乳山金成矿带内的其他金矿床,且富含Bi,认为阎家疃金矿床成矿深度为中深部。在总结区域成矿地质背景和矿床地质特征的基础上,通过类比区内金矿床成矿年龄来探讨矿床成因,初步认为早白垩世胶东地区岩石圈大规模拆沉、壳幔强烈相互作用,俯冲板片变质脱水形成大量成矿流体,活化前寒武纪变质基底岩石中的金等成矿物质,含金流体沿金牛山断裂运移,在NNE和SN向断裂交会处,破碎程度高、孔隙度大的位置沉淀成矿。

关键词: 牟平, 鹊山岩体, 地质特征, 金属矿物, 共生组合, 成矿阶段, 矿床成因, 阎家疃金矿床

Abstract: Yanjiatuan gold deposit is located in the Muping-Rushan metallogenic belt,one of the three major gold mineralization belts in the Jiaodong district.It is the altered rock type and sulfide quartz vein type complex gold deposit,controlled by small scale SN and NNE-trending faults is Queshan rock mass.Through mine-ralogical and electron probe analysis,the ore mineral characteristics and occurrence state of gold minerals in Yanjiatuan gold deposit are studied,and symbiotic assemblage and formation sequence of metal minerls are determined.Gold generally occurs as medium-fine size grains,including mainly intergranular gold and minor inclusion gold.The higher fineness and the enrichment of Bi indicates that gold was formed under the condition of medium depth.On the basis of summarizing regional metallogenic background and geological characteristics of the deposit,the genesis is discussed by analogy with mineralization ages of gold deposit in the area,we concluded that extensive delamination and crust-mantle interaction occurred in the Jiaodong lithosphere in the early Cretaceous,and that large amount of fluid derived from metamorphic dehydration of the subduction slab activated the gold in the Precambrian meta-basement,which migrated along  Jinniushan faults.The gold formed the large scale mineralization in the joint of the SN and NNE-trending where the crushing and the porosities are development.

Key words: Muping, Queshan granite, geological characteristics, metallic mineral, paragenetic association, mineralization stage, genesis, Yanjiatuan gold deposit

中图分类号: 

  • P618.51
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