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新疆白杨河铀矿床钻孔岩芯蚀变分带特征及地质意义

侯腱膨, 徐清俊, 叶发旺, 张川, 孟树. 2018. 新疆白杨河铀矿床钻孔岩芯蚀变分带特征及地质意义[J]. 中国地质, 45(4): 839-850. doi: 10.12029/gc20180413
引用本文: 侯腱膨, 徐清俊, 叶发旺, 张川, 孟树. 2018. 新疆白杨河铀矿床钻孔岩芯蚀变分带特征及地质意义[J]. 中国地质, 45(4): 839-850. doi: 10.12029/gc20180413
HOU Jianpeng, XU Qingjun, YE Fawang, ZHANG Chuan, MENG Shu. 2018. Alteration zonation of drilling cores in the Baiyanghe uranium deposit of Xinjiang and its geological implications[J]. Geology in China, 45(4): 839-850. doi: 10.12029/gc20180413
Citation: HOU Jianpeng, XU Qingjun, YE Fawang, ZHANG Chuan, MENG Shu. 2018. Alteration zonation of drilling cores in the Baiyanghe uranium deposit of Xinjiang and its geological implications[J]. Geology in China, 45(4): 839-850. doi: 10.12029/gc20180413

新疆白杨河铀矿床钻孔岩芯蚀变分带特征及地质意义

  • 基金项目:
    核工业地质局项目“铀及多金属矿产勘查高光谱遥感综合应用示范研究”(YLTY1604)资助
详细信息
    作者简介: 侯腱膨, 1984年生, 男, 工程师, 地质资源与地质工程专业; E-mail:xiatonghai@163.com
    通讯作者: 徐清俊, 1987年生, 男, 博士生, 构造地质学专业; E-mail:15210964889@163.com
  • 中图分类号: P627

Alteration zonation of drilling cores in the Baiyanghe uranium deposit of Xinjiang and its geological implications

  • Fund Project: Supported by Comprehensive application study of hyperspectral remote sensing for uranium and multi-metal ore exploration (No. YLTY1604)
More Information
    Author Bio: HOU Jianpeng, male, born in 1985, engineer, majors in geological resources and geological engineering; ;E-mail:xiatonghai@163.com .
    Corresponding author: XU Qingjun, male, born in 1987, doctor candidate, majors in structural geology; E-mail:15210964889@163.com
  • 钻孔岩芯高光谱技术是获取岩芯地学信息与研究的新方向。新疆白杨河铀矿床钻孔岩芯蚀变发育,对其开展蚀变研究有助于对白杨河矿床深部铀矿勘探提出更好的找矿认识。本次研究利用FieldSpec4可见光-短波红外地面非成像光谱仪对新疆白杨河铀矿床8个钻孔进行光谱测试与分析,研究发现钻孔岩芯热液蚀变矿物组合垂向上具有明显的"上低下高中过渡"的三分带特征:即上部为低铝绢云母+少量赤铁矿与少量褐铁矿+少量蒙脱石,中部为中铝绢云母+低铝绢云母+少量蒙脱石+少量碳酸盐、赤铁矿与褐铁矿,下部为高铝绢云母+绿泥石+碳酸盐;绢云母Al-OH吸收峰位置变化规律反映出矿床的热液活动具有深部相对高温、高压、偏酸性,浅部相对低温、低压、偏碱性的特征。蚀变三分带特征以及热液活动特征表明白杨河铀矿床具有明显的热液成矿背景,同时,铀矿化总体处于3分带特征中的中部以中铝绢云母为主的蚀变带与下部以高铝绢云母为主的蚀变带之间的过渡带中,该过渡带是铀成矿的有利部位,同时也是可能的热液/矿化中心;过渡带中发育赤铁矿,中铝绢云母和高铝绢云母,此3种蚀变矿物可能与铀成矿关系密切。这些可以为白杨河铀矿床深部铀矿勘探提供借鉴与参考。

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  • 图 1  雪米斯坦东缘白杨河矿床位置图

    Figure 1. 

    图 2  白杨河铀矿床地质简图(据张鑫等修改, 2013

    Figure 2. 

    图 3  白杨河铀矿床矿体平面分布图(a)及矿体垂向剖面上分布图(b)(据核工业216队)

    Figure 3. 

    图 4  钻孔岩芯光谱数据处理流程图

    Figure 4. 

    图 5  8种蚀变矿物光谱曲线图

    Figure 5. 

    图 6  钻孔ZK5630-1碳酸盐脉照片(a)和ZK5630-1矿化段岩芯(b)照片

    Figure 6. 

    图 7  钻孔ZK5630-1综合编录图

    Figure 7. 

    图 8  8个钻孔蚀变矿物编录图

    Figure 8. 

    图 9  绢云母Al-OH吸收峰位变化图

    Figure 9. 

    表 1  8种蚀变矿物特征吸收峰位

    Table 1.  The absorption features of eight kinds of altered minerals

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出版历程
收稿日期:  2016-09-19
修回日期:  2017-07-18
刊出日期:  2018-08-25

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