首页|黑龙江椭坡垴地区水系沉积物地球化学特征与找矿前景

黑龙江椭坡垴地区水系沉积物地球化学特征与找矿前景

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椭坡垴地区为大兴安岭森林植被浅覆盖区,是实施水系沉积物测量找矿的有利区域,针对该区热液成矿作用的特点,对该区开展了Au、Ag、Cu、Pb、Zn、As、Sb、Bi、W、Mo、Sn、Hg等12种元素的1∶5万水系沉积物测量,通过对4个地质子区的元素地球化学特征进行的对比与分析,查明了区域元素富集贫化规律,采用因子分析方法对特征值大于1的塔木兰沟组火山岩(J3t)子区和侵入岩(ηγ∈3-O1和γπ∈3-O1)子区的因子主成分进行了系统研究,结果表明火山岩子区中宝14Hs-30异常由金铅锌矿化引起,在该子区发现金铅锌矿点一处;侵入岩子区中宝14Hs-4异常由锡矿化引起.在此基础上总结了区内金矿和铅锌矿的找矿标志,并在该区域内圈定锡成矿远景区1处.
Geochemical characteristics and prospecting prospects of stream sediments in the Tuoponao area,Heilongjiang
Twelve elements such as Au,Ag,Cu,Pb,Zn,As,Sb,Bi,W,Mo,Sn,Hg are analyzed for 2776 sedimentary samples of 1∶50 000 stream system in Tuoponao area of 630.29 km2.The geochemical charac-teristics of the four geoproton areas are compared and analyzed,and the rrgularity of regional element enrich-ment and depletion is found out.The factor analysis method is adopted to systematically study the factor principal components of sub-area(J3t)of volcanic rock and intrusive rock(ηγ∈3O1,γπ ∈ 3 O1)of Tamu-langou Formation with characteristic values greater than 1.The study result indicates that the Bao14Hs-30 a-nomaly in the volcanic rock sub-area is caused by gold-lead-zinc mineralization,and a gold lead zinc mineral spot has been discovered in this sub-area.The Bao-14Hs-4 anomaly in the intrusive rock zone is caused by tin mineralization.On this basis,the prospecting indicator for gold and lead-zinc mineralization in the region is summarized,and one tin mineralization prospect area is delineated within the region.

stream sedimentary surveyelement anomaly characteristicsfactor analysisprospecting predic-tionTuoponao area in Heilongjiang

李冰、王晓鹏、苏仁奎

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黑龙江省第七地质勘查院,黑龙江绥化 152000

水系沉积物测量 元素异常特征 因子分析 找矿预测 黑龙江椭坡垴地区

黑龙江省财政项目黑龙江省塔河县508高地金多金属矿普查

HLJKD2014-11KCZX-SDKC-2017026

2024

矿产与地质
桂林矿产地质研究院

矿产与地质

CSTPCD
影响因子:0.42
ISSN:1001-5663
年,卷(期):2024.38(1)
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