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小兴安岭伊东林场金多金属矿床地质特征及找矿标志

  • 作者:
  • 梁杉杉|孙博|周佳峥|赵忠海|王兴|李成禄
  • 作者单位:
  • 辽宁工程技术大学矿业学院|辽宁省冶金地质勘查研究院有限责任公司|辽宁工程技术大学矿业学院|辽宁工程技术大学矿业学院|黑龙江省自然资源调查院|黑龙江省自然资源调查院
  • 基金项目:

  • 国家重点研发计划项目(2017YFC0601306);辽宁省自然科学基金项目(2020-BS-258);辽宁省教育厅科学研究经费项目(LJ2020JCL010);黑龙江省重点研发计划项目(GA21A204);辽宁工程技术大学学科创新团队资助项目(LNTU20TD-14);辽宁工程技术大学研究生创新实践竞赛培育项目(LNTU2022A023)
  • 详细信息:

  • 作者简介:
  • 梁杉杉(1997—),女,硕士研究生,研究方向为矿床地球化学;E-mail:ssl133@yeah.net
  • 通讯作者:
  • 赵忠海(1984—),男,副教授,博士,从事区域地质调查及矿床学研究工作;E-mail:zhaozhonghai@lntu.edu.cn
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Geological characteristics and ore-prospecting indicators in Yidonglinchang Gold Polymetallic Deposit,the Lesser Khingan Range

  • English Author:
  • College of Mining,Liaoning Technical University|Liaoning Metallurgical Geological Exploration Research Institute Co.,Ltd.|College of Mining,Liaoning Technical University|College of Mining,Liaoning Technical University|Natural Resources Survey Institute of Heilongjiang Province|Natural Resources Survey Institute of Heilongjiang Province
  • Unit:
  • 摘要
  • 在线预览
  • 参考文献

摘要:

伊东林场金多金属矿床赋存于宁远村组中酸性火山-次火山岩中,矿石类型主要为碳酸盐石英脉型和硅化角砾岩型,成矿地质体为闪长玢岩和英安玢岩。矿石中的金属矿物有银金矿、辉银矿、自然银、黄铁矿、黄铜矿、闪锌矿、方铅矿等,含金、银的矿物主要有银金矿、辉银矿、自然银;脉石矿物主要有石英、方解石、斜长石、绢云母,还含有少量石膏。矿石结构主要有自形—半自形—他形粒状结构、碎裂结构、交代结构和包含结构,矿石构造主要有胶状构造、孔洞状构造、梳状构造、晶簇状构造、稀疏浸染状构造、致密块状构造、角砾状构造、网脉状构造和叶片状构造。围岩蚀变类型有硅化、碳酸盐化、绢云母化、黏土化、绿泥石化和绿帘石化等。以矿体为中心,由内向外发育典型浅成低温热液蚀变带:硅化带、黄铁绢英岩化带、泥化带、青磐岩化带,总体呈环带状。综合典型矿床分析,确定宁远村组中酸性火山-次火山岩,强硅化、碳酸盐化和石英脉,北东东向和近东西向断裂,Au、Ag、As、Sb组合异常,高阻低极化低磁化等条件为伊东林场金多金属矿床的重要找矿标志。

关键词:

矿床地质特征;找矿标志;浅成低温热液;金多金属矿床;伊东林场;小兴安岭

Abstract:

Yidonglinchang Gold Polymetallic Deposit occurs in intermediate acid volcanic-subvolcanic rocks of the Ningyuancun Formation.The ore types are mainly carbonate quartz veins and silicified breccia,and the ore-forming geological body is diorite porphyrite and dacite porphyrite.The metallic minerals in the ore are electrum,argentite,native silver,pyrite,chalcopyrite,sphalerite,galena,and so on.The minerals containing gold and silver are mainly electrum,argentite,and native silver.The gangue minerals mainly include quartz,calcite,plagioclase,sericite,and minor content of gypsum.Major ore textures are euhedral-subhedral-anhedral texture,cataclastic texture,metasomatic texture,and inclusion texture.Major ore structures are colloform structure,cavernous structure,comb structure,crystal cluster structure,sparsely disseminated structure,dense massive structure,breccia structure,stockwork structure,and blade structure.The wall rock alteration includes silicification,carbonation,sericitization,clayization,chloritization,and epidotization.With the ore body as the center,a typical epithermal alteration belt is developed from the inside out:silicification zone,beresitization zone,argillation zone,and propylitization zone,generally taking the form of rings.Based on typical deposit analysis,the study takes the volcano-subvolcanic rocks in the Ningyuancun Formation,strong silicification,carbonation,and quartz veins,NEE and near-EW faults,Au,Ag,As,and Sb combination anomalies,low polarization high resistivity,and negative magnetic anomaly as important prospecting indicators in Yidonglinchang Gold Polymetallic Deposit.

Keywords:

deposit geological characteristics;prospecting indicator;epithermal;gold polymetallic deposit;Yidonglinchang;the Lesser Khingan Range