Extraction of remote sensing ore-indicating information and block optimization in middle-northern segment of Zhongtiao Mountain, Shanxi Province
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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。
Abstract:Objective Ore block optimization of is an important task in the new round of strategic prospecting breakthrough actions, and a key initiative to respond to the Ministry of Natural Resources in further improving the efficiency of prospecting, developing new-quality productive forces, and enhancing the support capacity of mineral resources. As one of China's key national strategic resource concentration areas for gold, copper, iron, and other critical minerals, the Zhongtiao Mountain in Shanxi Province is abundant in mineral resources. However, to date, there is relatively limited research on the large-scale remote sensing geological interpretation and prospecting applications based on remote sensing satellite images in this region, which is of great significance for prospecting prediction.
Methods The middle-northern segment of the Zhongtiao Mountain in Shanxi Province was selected as the study area. Based on human-computer interactive interpretation of ore-controlling structural and ore-controlling ring features from Spot-6 remote sensing images, the regional structural distribution of the study area was summarized from a macro perspective. Principal component analysis (PCA) was employed to preliminarily extract mineralization alteration anomaly information via Aster data. Additionally, with field spectral curves of typical rocks and minerals collected by an ASD spectrometer as training samples, the spectral angle mapping (SAM) method was applied to extract the distribution of ore-bearing strata. The distribution results were then used to screen the PCA extraction results to identify three major types of mineralization alterations, including iron staining, hydroxyl, and carbonate. The spatial correlation between alteration anomalies and ore-controlling factors (such as regional structures, ore-bearing strata, and rock mass distribution) was further analyzed.
Results The results indicated that: (1) The linear and ring structures were well-developed in the study area, with 84 newly interpreted faults and 136 ring structures, which helped refine and supplement the shortcomings of previous geological survey findings. (2) The mineralization and alteration information obtained by PCA and rock-ore spectral inversion could effectively indicate mineralization anomalies, highlighting the important role of regional structures in ore formation. (3) A comprehensive anomaly isodensity map was obtained through combined analysis of field verification and existing regional geological data to delineate three optimal mineralization areas.
Conclusion The research findings provide a basis and guidance for subsequent evaluation of mineral resource potential, prospecting prediction, and strategic actions of deep prospecting. The findings also promote the application of remote sensing-based geological prospecting in the Zhongtiao Mountain, and provide insights into future remote sensing-based geological prospecting efforts in other regions of Shanxi Province.
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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
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 2015/12/16 3150 全色分辨率为1.5 m
多光谱分辨率为6 m2014/12/12 2013/12/31 Aster数据 2005/03/23 3150 Band1~3分辨率为15 m
Band4~9分辨率为30 m
Band10~14分辨率为90 m2005/03/30 2006/03/24 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 NNDiffuse 0.60863 0.04475 5.24934 0.02162 Gram-Schmidt 0.50261 0.00749 2.85081 0.00492 PC 0.51384 0.00478 2.26483 0.00285 Brovey 0.50100 0.00027 0.00122 0.00019 注:参数值为各波段参数的平均值 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 云 (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 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+)Band1 0.265456 0.441699 − 0.434136 − 0.751158 Band2 0.342133 0.514535 − 0.354134 0.654396 Band3 0.515148 0.328932 0.741541 − 0.048923 Band4 0.747815 − 0.631286 − 0.214641 0.005133 Al-OH基团 Band1 0.289626 0.572485 0.745240 − 0.237267 Band3 0.445364 0.648204 − 0.554224 0.226745 Band4 0.644482 − 0.302524 − 0.154528 − 0.666426 Band8 0.582397 − 0.354568 0.350533 0.669486 Mg-OH基团 Band1 0.237826 0.515545 0.454256 0.684865 Band4 0.434612 0.699602 − 0.294525 − 0.485568 Band6 0.649462 − 0.358542 − 0.540554 0.395426 Band7 0.542688 − 0.344264 0.642136 − 0.365452 CO32-基团 Band1 − 0.236845 0.565217 0.391453 0.605438 Band3 − 0.440441 0.646354 − 0.134504 − 0.645021 Band4 − 0.644187 − 0.250453 − 0.634035 0.342878 Band5 − 0.574503 − 0.447450 0.651055 − 0.203504 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 -
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