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山西省中条山中北段遥感示矿信息提取与区块优选

刘知 李彦星 杨波 刘小松 张航

刘知,李彦星,杨波,等. 山西省中条山中北段遥感示矿信息提取与区块优选[J]. 地质科技通报,2026,45(2):1-19 doi: 10.19509/j.cnki.dzkq.tb20240617
引用本文: 刘知,李彦星,杨波,等. 山西省中条山中北段遥感示矿信息提取与区块优选[J]. 地质科技通报,2026,45(2):1-19 doi: 10.19509/j.cnki.dzkq.tb20240617
LIU Zhi,LI Yanxing,YANG Bo,et al. Extraction of remote sensing ore-indicating information and block optimization in middle-northern segment of Zhongtiao Mountain, Shanxi Province[J]. Bulletin of Geological Science and Technology,2026,45(2):1-19 doi: 10.19509/j.cnki.dzkq.tb20240617
Citation: LIU Zhi,LI Yanxing,YANG Bo,et al. Extraction of remote sensing ore-indicating information and block optimization in middle-northern segment of Zhongtiao Mountain, Shanxi Province[J]. Bulletin of Geological Science and Technology,2026,45(2):1-19 doi: 10.19509/j.cnki.dzkq.tb20240617

山西省中条山中北段遥感示矿信息提取与区块优选

doi: 10.19509/j.cnki.dzkq.tb20240617
基金项目: 山西省地质勘查基金项目(2018-49;2019-27)
详细信息
    作者简介:

    刘知:E-mail:2454667759@qq.com

    通讯作者:

    E-mail:66369280@qq.com

  • 中图分类号: P627

Extraction of remote sensing ore-indicating information and block optimization in middle-northern segment of Zhongtiao Mountain, Shanxi Province

More Information
  • 摘要:

    区块优选是新一轮找矿突破战略行动一项重要工作,是响应自然资源部进一步提高找矿工作效率、发展新质生产力和提高矿产资源保障能力的重要举措。山西省中条山作为全国金、铜、铁等重要战略资源矿集区之一,矿产资源丰富,目前区内尚无大比例尺基于遥感卫星影像地质解译及找矿应用研究。以山西省中条山中北段为研究区,通过对Spot-6遥感影像进行控矿构造要素、控矿环形要素的人机交互解译,宏观上总结区域构造分布特征,基于Aster数据应用主成分分析法(PCA)初步提取蚀变矿化异常信息,以ASD光谱仪采集的野外典型岩矿光谱曲线作为训练样本,采用光谱角填图法(SAM)反演含矿地层分布,并利用结果用于筛选PCA提取信息,获取铁染、羟基、碳酸盐三大类矿化蚀变,分析蚀变异常与控矿要素(区域构造、赋矿地层、岩体分布等)的空间相关性。结果表明:①研究区线环构造发育,新增解译断裂84条,环形构造136条,解译结果可辅助修正前人地质调查成果的不足;②基于PCA法和岩矿光谱反演得到的矿化蚀变信息可有效指示矿化异常的位置,且研究区构造控矿作用明显;③结合野外实地验证和已有区域地质资料成果叠加分析得到综合异常等密度图,圈定出三大成矿优选区。研究成果为矿产资源潜力评价、找矿预测和深部找矿战略行动提供依据和指导。

     

  • 图 1  研究区地质简图(a)和大地构造位置(b)

    1. 第四系;2. 新近系;3. 古近系;4. 二叠系;5. 石炭系;6. 奥陶系;7. 寒武系;8. 长城系雄耳群;9. 长城系汝阳群;10. 长城系担山石群;11. 上中条亚群;12. 下中条亚群;13. 绛县群铜矿峪亚群;14. 绛县群横岭关亚群;15. 宋家山群;16. 燕山期;17. 晋宁期;18. 中条期;19. 绛县期;20. 宋家山期;21. 涑水期;22. 角砾岩;23. 断裂;24. 研究区范围;25. 三级构造单元;26. 四级构造单元;27. 隆起;28. 坳陷;29. 已知或推断的大断裂及编号;30. 构造单元分级编号;31. 地名;⑦. 涑渭大断裂;⑧. 中条北麓大断裂;⑨. 中条南东侧大断裂;⑩. 太行南麓大断裂;Ⅲ6. 汾渭断陷;Ⅳ2. 稷山台拱;Ⅳ3. 涑渭断凹;Ⅳ4. 黄河断凹;Ⅱ3. 山西中台隆;Ⅱ4. 嵩条断褶区;Ⅲ10. 中黄陷断褶束;Ⅳ8. 中条台穹;Ⅳ9. 黄金山凹断褶束;Ⅳ10. 洛阳台凹;Ⅱ6. 秦岭轴缘坳陷;Ⅲ16. 华露台拱

    Figure 1.  Simplified geological map (a) and tectonic location (b) of the study area

    图 2  不同融合方法结果对比图(以横岭关地区为例)

    a. Brovey融合方法;b. PC融合方法;c. Gram-Schmidt融合方法;d. NNDiffuse融合方法

    Figure 2.  Comparison of results using different fusion methods

    图 3  典型岩石波谱图(a1~j1)及连续统(包络线)去除图(a2~j2)

    a1,a2. 安山岩;b1,b2. 变辉长岩;c1,c2. 片岩;d1,d2. 大理岩;e1,e2. 白云岩;f1,f2. 片麻岩;g1,g2. 千枚岩;h1,h2. 花岗岩;i1,i2. 板岩;j1,j2. 石英岩

    Figure 3.  Typical rock spectra (a1-j1) and continuum removal spectra (a2-j2)

    图 4  蚀变矿物波谱与Aster波段对应关系

    a. Al-OH;b. Mg-OH;c. Fe离子;d. CO32−。彩色柱状为Aster数据的各波段宽度

    Figure 4.  Correation between spectra of alteration minerals and Aster bands

    图 5  研究区线性构造遥感解译标志

    a. 不同地貌单元;b. 断层三角面;c. 色调差异明显;d. 河流汇聚和局部直线;e. 同步错动水系;f. 直角河和同向转弯河系;g. 山脊(规律)错动;h. 正负地形突变;i. 断裂切割地层。淡绿色线为山脊走向或者河流走向;其余线型均为辅助线,起区分和指示作用,无实际含义;下同

    Figure 5.  Remote sensing interpretation signs for linear structures in the study area

    图 6  研究区主要断裂构造解译图(a)和环形构造解译图(b)

    Figure 6.  Interpretation maps of main fault structures (a) and ring structures (b) in the study area

    图 7  研究区环形构造遥感解译标志

    a. 放射状环要素;b. 线环相切型构造;c. 地貌突变型环要素;d. 线环相交型构造;e. 双环相交型构造;f. 火山口型环要素;g. 火山锥型环要素;h. 色调差异明显的双环套合环要素

    Figure 7.  Remote sensing interpretation signs for ring structures in the study area

    图 8  基于光谱反演的蚀变岩性反演图

    Figure 8.  Alteration lithology inversion map based on inversion spectral data

    图 9  遥感异常分布与统计图

    Figure 9.  Remote sensing anomaly distribution and statistics map

    图 10  蚀变异常相关性分析

    a. 蚀变异常面积与重叠区相应异常面积百分比雷达概率图;b. 蚀变异常面积与不同构造运动期岩体面积百分比玫瑰概率图;c. 蚀变异常面积与不同含矿地层面积百分比玫瑰概率图

    Figure 10.  Correlation analysis of alteration anomalies

    图 11  研究区构造野外查证照片

    a,b. 地层错动;c. 断裂擦痕;d,e. 断层破碎带填充;f. 断层破碎带

    Figure 11.  Photos of field structural verification in the study area

    图 12  矿化蚀变野外验证结果

    a. 褐铁矿化与绢英岩化;b. 黄铁矿化;c. 褐铁矿化与孔雀石化;d. 绿泥石化;e. 绿帘石化与碳酸盐化;f. 绿帘石化与硅化;g. 孔雀石化;h. 石英岩化与白云岩化;i. 碳酸盐化

    Figure 12.  Field verification results of mineralization and alteration

    图 13  综合异常等密度图

    Figure 13.  Comprehensive anomaly isodensity map

    表  1  研究区遥感数据基本情况

    Table  1.   Basic information of remote sensing data in the study area

    数据种类成像日期面积/km2空间分辨率
    Spot-6数据2015/12/163150全色分辨率为1.5 m
    多光谱分辨率为6 m
    2014/12/12
    2013/12/31
    Aster数据2005/03/233150Band1~3分辨率为15 m
    Band4~9分辨率为30 m
    Band10~14分辨率为90 m
    2005/03/30
    2006/03/24
    下载: 导出CSV

    表  2  不同融合方法定量评价

    Table  2.   Quantitative evaluation of different fusion methods

    融合方法均值标准差信息熵平均梯度
    NNDiffuse0.608630.044755.249340.02162
    Gram-Schmidt0.502610.007492.850810.00492
    PC0.513840.004782.264830.00285
    Brovey0.501000.000270.001220.00019
      注:参数值为各波段参数的平均值
    下载: 导出CSV

    表  3  各类干扰地物去除方法

    Table  3.   Methods for removing various types of disturbing features

    干扰因素 去除方法
    植被 (Band3−Band2)/(Band3+Band2)或Band3/Band2
    (b1 ge 云的最低亮度值)×0+(b1 lt 云的最低亮度值)×1
    或者Band1高端切割
    盐碱地 Band9/Band1或者Band1高端切割
    水体 Band9/Band1或者(Band1−Band4)/(Band1+Band4)
    阴影 (b1 ge 阴影中的高值)×1+(b1 lt 阴影中的低值)×0
    或者Band9/Band1
    冰雪 Band2或Band3高端切割
      注:b1=Band6/Band1
    下载: 导出CSV

    表  4  4类蚀变的主成分变换特征向量矩阵

    Table  4.   PCA eigenvector matrices of four alteration types

    蚀变类型 波段
    组合
    主成分
    PC1 PC2 PC3 PC4
    铁离子基团
    (Fe3+&Fe2+
    Band10.2654560.4416990.4341360.751158
    Band20.3421330.5145350.3541340.654396
    Band30.5151480.3289320.7415410.048923
    Band40.7478150.6312860.2146410.005133
    Al-OH基团Band10.2896260.5724850.7452400.237267
    Band30.4453640.6482040.5542240.226745
    Band40.6444820.3025240.1545280.666426
    Band80.5823970.3545680.3505330.669486
    Mg-OH基团Band10.2378260.5155450.4542560.684865
    Band40.4346120.6996020.2945250.485568
    Band60.6494620.3585420.5405540.395426
    Band70.5426880.3442640.6421360.365452
    CO32-基团Band10.2368450.5652170.3914530.605438
    Band30.4404410.6463540.1345040.645021
    Band40.6441870.2504530.6340350.342878
    Band50.5745030.4474500.6510550.203504
    下载: 导出CSV

    表  5  新发现矿化点信息统计

    Table  5.   Statistics of newly discovered mineralization occurrence information

    编号 点位坐标/m 出露地层 容矿岩石 Cu Zn Pb Ag Au 所在区位 备注
    wB/% wB/10−6
    KH001 x=3913998
    y=19555231
    Ar2t3 石榴子石绢英片岩 0.5342 0.00254 0.00108 0.214 0.00123 省道335旁 铜矿化点
    KH002 x=3908517
    y=19553831
    Pt1b 绢英片岩 0.5245 0.00296 0.00157 0.111 0.0175 刘庄冶西南 铜矿化点
    KH007 x=3919153
    y=19566379
    Pt1b 碳质板岩夹白云石大理岩 2.0586 0.00307 0.00192 1.866 0.532 前海西南 金、铜矿化点
    KH010 x=3909536
    y=19574976
    Ar2j 石英岩、含碳绢英片岩 3.6783 0.00167 0.00219 0.718 0.878 篱笆沟南 金矿化点、铜矿化线索点
    KH014 x=3876096
    y=19533351
    Pt1b,Pt1yj 碳质板岩、白云石大理岩 0.5345 0.00164 0.00123 0.215 0.024 柳仙洞西 铜矿化点
    KH020 x=3884197
    y=19551670
    Pt1yj,Chm 白云石大理岩、安山岩 0.0494 4.8988 7.9696 4.343 0.0264 上桃沟村 铅、锌矿化点,铜矿化线索点
    KH027 x=3864443
    y=19533227
    Pt1yj 白云石大理岩 0.6476 0.00161 0.0011 0.275 0.0331 西岭梁西北 铜矿化点
    KH029 x=3865560
    y=19533098
    Pt1yj 白云石大理岩 0.565 0.00143 0.000625 1.008 0.476 南白山东 铜矿化点
    KH030 x=3865508
    y=19532389
    Pt1yj 白云石大理岩 1.1206 0.00185 0.00329 3.246 0.0471 小场梁东 铜矿化点
      注:Ar2t3. 横岭关亚群铜凹组三段;Pt1b. 中条群篦子沟组;Ar2j. 宋家山群绛道沟组;Pt1yj. 中条群余家山组;Chm. 熊耳群马家河组
    下载: 导出CSV
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