首页|内蒙古喀喇沁旗安家营子金矿床热液蚀变过程中元素迁移特征及其地质意义

内蒙古喀喇沁旗安家营子金矿床热液蚀变过程中元素迁移特征及其地质意义

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安家营子金矿床在成矿过程中发生了广泛的热液蚀变作用,蚀变类型从早到晚依次为钠长石化、绢云母化、硅化、黄铁绢英岩化、绿泥石化等.通过对各类蚀变岩样品及其原岩的主量元素、微量元素进行测试分析,详细研究了热液蚀变过程中元素迁移特征.结果表明:①主量元素SiO2、CaO、MgO、Fe2O3、TiO2 呈现逐渐降低特征;②微量元素中大离子亲石元素K、Rb、Th显示出增加趋势,而Sr呈现减少趋势,Bi在所有蚀变中都表现出明显升高特征;③稀土元素总量呈现升高趋势;④成矿元素Bi、Cu、Zn在黄铁绢英岩化和硅化阶段具有较高的含量.结合岩相学特征,进一步揭示了成矿元素卸载从绢英岩化阶段开始,大量集中在硅化阶段,为矿体定位及圈定提供依据.
Characteristics of element migration during hydrothermal alteration in Anjiayingzi Gold Deposit,Harqin Banner,Inner Mongolia,and its geological significance
Extensive hydrothermal alteration occurred to Anjiayingzi Gold Deposit during mineralization.The sequence of alteration types from early to late is albitization,sericitization,silicification,pyrite sericitization,chloritiza-tion.Through the analysis of major and micro elements in various altered rock samples and their original rocks,this paper studied the characteristics of element migration during hydrothermal alteration in detail.The results show that①the main elements SiO2,CaO,MgO,Fe2O3 and TiO2 show a gradual decreasing feature;②the large ion lithophile elements K,Rb,Th in the micro elements show an increasing trend,while Sr shows a decreasing trend,and Bi shows an obvious increas-ing feature in all alterations;③the abundance of rare earth shows an increasing trend;④the ore-forming elements Bi,Cu and Zn have high contents in the pyrite sericitization and silicification stages.Combining with the petrographic character-istics,it is further revealed that the unloading of ore-forming elements starts from the stage of pyritization,and is concen-trated in the silicification stage,providing a basis for the positioning and delineation of ore bodies.

hydrothermal alterationelement migrationAnjiayingzi Gold DepositHarqin Bannermajor elementmicro element

茹朋、李晓芳、王亚珂

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河南省地质研究院

河南省金属矿产成矿地质过程与资源利用重点实验室

河南省地质科学研究所有限公司

热液蚀变 元素迁移 安家营子金矿床 喀喇沁旗 主量元素 微量元素

中国地调局项目中国地调局项目中国地调局项目

DD20221695DD20190379DD20160346

2024

黄金
长春黄金研究院

黄金

CSTPCD
影响因子:0.446
ISSN:1001-1277
年,卷(期):2024.45(5)
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