青海三岔河北金多金属矿地球化学异常特征及找矿潜力分析

谈艳, 张鑫利, 王泰山, 保善斌, 赵伟. 2019. 青海三岔河北金多金属矿地球化学异常特征及找矿潜力分析. 西北地质, 52(4): 170-181.
引用本文: 谈艳, 张鑫利, 王泰山, 保善斌, 赵伟. 2019. 青海三岔河北金多金属矿地球化学异常特征及找矿潜力分析. 西北地质, 52(4): 170-181.
TAN Yan, ZHANG Xingli, WANG Taishan, BAO Shanbin, ZHAO Wei. 2019. Geochemical Anomaly Characteristics and Prospecting Potential of Gold Polymetallic Deposits in Sanchahebei Area, Qinghai Province. Northwestern Geology, 52(4): 170-181.
Citation: TAN Yan, ZHANG Xingli, WANG Taishan, BAO Shanbin, ZHAO Wei. 2019. Geochemical Anomaly Characteristics and Prospecting Potential of Gold Polymetallic Deposits in Sanchahebei Area, Qinghai Province. Northwestern Geology, 52(4): 170-181.

青海三岔河北金多金属矿地球化学异常特征及找矿潜力分析

  • 基金项目:

    青海省地质勘查基金项目“青海省格尔木市三岔河北金多金属矿预查”(2016020046kc008)

详细信息
    作者简介: 谈艳(1990-),女,青海西宁人,工程师,硕士,主要从事矿产项目管理工作。E-mail:jltyandk@163.com
  • 中图分类号: P592

Geochemical Anomaly Characteristics and Prospecting Potential of Gold Polymetallic Deposits in Sanchahebei Area, Qinghai Province

  • 三岔河北金-多金属矿位于东昆仑多金属成矿带中段,区内矿化主要赋存于青办食宿站组与沙松乌拉组之间的接触带,矿化富集受北西西向断裂构造控制的特征明显,围绕北西西向断裂构造带是寻找金矿化最直接的标志。区内金矿化的主要含矿岩性为构造蚀变岩,铜多金属矿化的主要含矿岩性为千枚状板岩、大理岩。通过在三岔河北地区3处以Au、Sn、Mo为主的1:5万水系沉积物异常靶区(HS乙316、HS乙324、HS乙239)内实施1:1万土壤测量、槽探、钻探工程,圈定出破碎蚀变带4条(Sb1、Sb2、Sb3、Sb4)、2条金矿化体(MⅠ-1、MⅢ)、5条多金属矿(化)体(MⅠ-2、MⅡ、MⅣ、MⅤ、MⅥ)。通过1:20万水系沉积物测量-1:5万水系沉积物地球化学测量-1:1万土壤地球化学测量-地质及工程验证的化探综合找矿方法,不断缩小找矿靶区,取得了较好的找矿效果。其中,Sb1、Sb3破碎蚀变带为构造蚀变岩型金矿,Sb2、Sb4破碎蚀变带为与黑色岩系有关的钒钼矿及伴生铂族矿。通过进一步的工作,有望寻找出一定规模的与黑色岩系有关的钒钼矿及伴生铂族矿床和构造蚀变岩型金矿床。综上所述,本区具有优越的成矿地质条件,化探异常发育,且已发现了较好的银多金属矿找矿信息,充分展示出本区具较大的找矿潜力,通过进一步工作,有望取得较好的找矿成果。
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出版历程
收稿日期:  2019-01-09
修回日期:  2019-04-12

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