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物探与化探  2025, Vol. 49 Issue (6): 1281-1290    DOI: 10.11720/wtyht.2025.0123
  地质调查资源勘查 本期目录 | 过刊浏览 | 高级检索 |
青海松树南沟金矿区土壤地球化学特征及异常评价
陈庚户1(), 郎兴海2(), 王兆帅3, 董维财1, 王登科1, 向佐朋2, 李壮4, 叶紫枫2, 吴昌益2, 王旭辉2, 吴天文1, 罗超1
1.四川鑫顺矿业股份有限公司, 四川 成都 610041
2.成都理工大学 地球与行星科学学院, 四川 成都 610059
3.山东省地矿工程集团有限公司, 山东 济南 250013
4.内江师范学院 地理与资源科学学院, 四川 内江 641100
Geochemical characteristics and anomaly assessments of soils in the Songshunangou gold mining area, Qinghai Province
CHEN Geng-Hu1(), LANG Xing-Hai2(), WANG Zhao-Shuai3, DONG Wei-Cai1, WANG Deng-Ke1, XIANG Zuo-Peng2, LI Zhuang4, YE Zi-Feng2, WU Chang-Yi2, WANG Xu-Hui2, WU Tian-Wen1, LUO Chao1
1. Sichuan Xinshun Mining Co., Ltd., Chengdu 610041, China
2. College of Earth and Planetary Sciences, Chengdu University of Technology, Chengdu 610059, China
3. Shandong Geology and Mineral Resources Engineering Group Co., Ltd., Jinan 250013, China
4. College of Greography and Resources Science, Neijiang Normal University, Neijiang 641100, China
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摘要 

松树南沟金矿区位于北祁连成矿带中部,目前发现有东、西两个矿床,累计探获Au资源量超34 t,已达大型金矿规模,矿区找矿潜力巨大,亟须开展找矿方向研究,为找矿勘查工作部署提供支撑。为此,本文通过1∶10 000土壤地球化学异常分析,利用两窗口移动平均法查明了该区Au、As、Sb、Hg、Cu、Pb、Zn、Ag、W、Mo共10种元素的异常分布特征及富集规律;基于元素地球化学异常数据解析,综合研究区成矿地质条件,采用平均衬度法圈定综合异常区,并进行异常评价。研究结果表明:Au是矿区的主要成矿元素,呈现强富集、强变异特征,具有较大的成矿潜力;矿区内共圈定土壤地球化学综合异常区7个,其中HP-1、HP-2和HP-5综合异常找矿潜力最大。经工程验证,HP-2异常新发现矿(化)体见矿厚度达1.5 m,金品位达到0.57 g/t;HP-5综合异常新发现矿(化)体见矿厚度达1.42 m,品位达到1.67 g/t。本研究为松树南沟金矿区的找矿方向提供了地球化学依据,为矿区下一步的矿产勘查工作部署提供了参考。

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陈庚户
郎兴海
王兆帅
董维财
王登科
向佐朋
李壮
叶紫枫
吴昌益
王旭辉
吴天文
罗超
关键词 松树南沟金矿土壤地球化学特征综合异常成矿预测北祁连造山带    
Abstract

The Songshunangou gold mining area in Qinghai Province is situated in the central part of the North Qilian metallogenic/orogenic belt. Two deposits have been identified in its eastern and western portions, with cumulative proven Au resources exceeding 34 t, establishing them as large-scale deposits. Moreover, the area holds significant potential for ore prospecting, necessitating an urgent need for research into prospecting orientations to support mineral exploration efforts. Hence, based on the anomaly analysis of 1∶10 000 soil geochemical survey data and employing the two-window moving average method, this study identified the anomaly distributions and enrichment patterns of 10 elements (i.e., Au, As, Sb, Hg, Cu, Pb, Zn, Ag, W, and Mo) in the area. By analyzing elemental geochemical anomaly data and integrating the geological conditions for mineralization, this study delineated composite anomaly zones in the area using the average contrast method, followed by anomaly assessments. The results indicate that Au is the primary ore-forming element in the area, characterized by strong enrichment and significant variability, suggesting high mineralization potential. Seven composite soil geochemical anomaly zones were delineated in the area, with zones HP-1, HP-2, and HP-5 demonstrating the greatest potential for mineral exploration. Engineering validation confirms the presence of two ore/mineralized bodies, with one exhibiting an ore thickness of 1.5 m and a gold grade of 0.57 g/t in zone HP-2 and the other featuring an ore thickness of 1.42 m and a gold grade of 1.67 g/t in zone HP-5. Overall, this study provides geochemical evidence for determining prospecting orientations in the Songshunangou gold mining area while offering a reference for the deployment of subsequent mineral exploration work in the area.

Key wordsSongshunangou gold mining area    soil geochemical characteristics    composite anomaly    metallogenic prediction    North Qilian orogenic belt
收稿日期: 2025-04-07      修回日期: 2025-08-29      出版日期: 2025-12-20
ZTFLH:  P632.1  
基金资助:国家自然科学基金项目(42572103);国家重点研发计划项目(2022YFC2905000);自然资源部新一轮找矿突破战略行动科技支撑项目(ZKKJ202405);自然资源部新一轮找矿突破战略行动科技支撑项目(ZKKJ202427);西藏自治区科技计划项目(XZ202401YD0066);四川省自然科学基金项目(2024NSFSC1954);四川省自然科学基金项目(2025ZNSFSC1196);科学技术部深地国家科技重大专项(SQ2024AAA060124-6);威海市能源资源调查评价重点实验室开放课题(LDKF-2023WH-04);成都理工大学珠峰科学研究计划项目(2020ZF11407)
通讯作者: 郎兴海
引用本文:   
陈庚户, 郎兴海, 王兆帅, 董维财, 王登科, 向佐朋, 李壮, 叶紫枫, 吴昌益, 王旭辉, 吴天文, 罗超. 青海松树南沟金矿区土壤地球化学特征及异常评价[J]. 物探与化探, 2025, 49(6): 1281-1290.
CHEN Geng-Hu, LANG Xing-Hai, WANG Zhao-Shuai, DONG Wei-Cai, WANG Deng-Ke, XIANG Zuo-Peng, LI Zhuang, YE Zi-Feng, WU Chang-Yi, WANG Xu-Hui, WU Tian-Wen, LUO Chao. Geochemical characteristics and anomaly assessments of soils in the Songshunangou gold mining area, Qinghai Province. Geophysical and Geochemical Exploration, 2025, 49(6): 1281-1290.
链接本文:  
https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2025.0123      或      https://www.wutanyuhuatan.com/CN/Y2025/V49/I6/1281
Fig.1  松树南沟金矿区大地构造位置(a)及地质简图(b)
Fig.2  松树南沟矿区土壤地球化学测量采样范围(地质简图见图1)
参数 Au Ag As Sb Hg Cu Zn Mo W Pb
最小值 0.18 0.71 2.52 0.28 3.6 1 1.13 0.21 0.2 4.2
中位数 1.39 72 17.9 1.15 29 29.9 90.4 1.05 2.06 2.06
最大值 720 3700 1281 139 1140 290 870 6.58 41.4 886
平均值 2.44 76 23.99 1.42 32.22 33.93 93.43 1.06 2.11 27.9
标准离差 9.47 49.05 27.95 1.78 24.25 14.12 23.67 0.26 0.69 21.65
变异系数 3.89 0.65 1.17 1.25 0.75 0.42 0.25 0.25 0.33 0.78
克拉克值 1.35 66.1 12.4 0.82 24.7 19.5 55.5 0.66 1.66 20.2
浓度克拉克值 1.81 1.15 1.93 1.73 1.3 1.74 1.68 1.61 1.27 1.38
Table 1  松树南沟矿区土壤地球化学参数
Fig.3  松树南沟矿区土壤地球化学元素相关矩阵
Fig.4  松树南沟矿区土壤地球化学元素R型聚类分析谱系
元素 F1 F2 F3
Au 0.576 -0.026 0.048
Ag 0.291 0.331 0.245
As 0.877 0.066 0.203
Sb 0.878 0.063 0.001
Hg 0.102 0.490 -0.524
Cu -0.005 -0.209 0.119
Zn 0.069 0.083 0.849
Mo 0.067 0.734 0.075
W -0.037 0.711 0.143
Pb 0.280 0.402 0.672
特征值 2.054 1.616 1.591
累积方差贡献率/% 20.542 36.698 52.608
Table 2  松树南沟矿区因子分析结果
参数 Au As Sb Hg Cu Pb Zn Ag W Mo
背景值 0.11 0.43 0.03 0.57 0.64 0.40 0.26 1.04 0.01 0.01
异常下限 0.92 5 0.3 9 8 6 12 14 0.4 0.2
Table 3  松树南沟矿区因子分析结果
Fig.5  松树南沟矿区土壤元素异常分布
Fig.6  松树南沟矿区土壤元素综合异常分布
模型要素 要素特征 分类
控矿因素 构造 受NW—SE向构造控制 重要
地层 主要赋矿地层为上奥陶统扣门子
组,主要赋矿岩性为玄武安山岩、
晶屑凝灰岩及流纹质凝灰岩
必要
岩浆岩 与成矿有关的岩体为晚奥陶世石
英闪长斑岩
必要
找矿标志 地球化学 Au为松树南沟矿区的主要成矿
元素,As、Sb为前缘元素,Ag、Pb、
Zn为近矿元素
必要
围岩蚀变 斑岩型矿化赋矿蚀变为钾化、青
磐岩化以及绢云母—绿泥石化,
其中钾化蚀变是矿体中心的指示
标志;浅成低温热液型矿化赋矿
蚀变为绢云母—绿泥石化以及
局部的绢英岩化蚀变
必要
Table 4  松树南沟矿区找矿模型
[1] Lang X H, Xiang Z P, Wang X H, et al. Unveiling an Early Paleozoic porphyry-epithermal gold system in Songshunangou district,North Qilian,northwest China:Geological and geochronological constraints[J]. Ore Geology Reviews, 2024, 164:105816.
[2] 隆昊. 门源县松树南沟金矿床地质构造特征[J]. 中国西部科技, 2014, 13(9):15-17.
[2] Long H. The features of geological structure in Songshunangou gold deposit of Menyuan County,Qinghai Province[J]. Science and Technology of West China, 2014, 13(9):15-17.
[3] 王檬. 青海门源县松树南沟金矿床地质特征及成因探讨[D]. 长春: 吉林大学, 2017.
[3] Wang M. Study on the geological characteristics and genesis of songshunangou Au deposit in Menyuan county,Qinghai Province[D]. Changchun: Jilin University, 2017.
[4] 徐镇华, 马玉见, 曹纪虎, 等. 青海巴拉哈图—白土沟地区成矿地质特征及找矿潜力分析[J]. 矿产勘查, 2019, 10(9):2180-2186.
[4] Xu Z H, Ma Y J, Cao J H, et al. Analysis on metallogenic geological characteristics and prospecting potential of the Balahatu-Baitougou area,Qinghai[J]. Mineral Exploration, 2019, 10(9):2180-2186.
[5] Xiang Z P, Lang X H, Wang X H, et al. Origin and tectonic setting of the ore-related late Ordovician porphyry in the songshunangou district,north Qilian,northwest China:Whole-rock geochemical,Sr-Nd-Pb isotopes and zircon Hf isotopes constraints[J]. Journal of Earth Science, 2025, 36(3):1051-1068.
[6] 张涛, 伊有昌, 肖小强, 等. 青海松树南沟金矿床控矿因素及找矿方向研究[J]. 矿产勘查, 2011, 2(1):49-53.
[6] Zhang T, Yi Y C, Xiao X Q, et al. The ore-controlling factors and prospecting guide analysis of Songshu Nangou Gold Deposit,Qinghai Province[J]. Mineral Exploration, 2011, 2(1):49-53.
[7] 刘强, 王冠, 王登科. 北祁连金矿区花岗闪长斑岩年代学及地质意义[J]. 四川地质学报, 2019, 39(1):15-21.
[7] Liu Q, Wang G, Wang D K. Geochronology and its geological significance for granodiorite porphyry in the songshunangou Au deposit,north Qilian Mountains[J]. Acta Geologica Sichuan, 2019, 39(1):15-21.
[8] 王冠, 肖晓林, 刘强, 等. 松树南沟金矿区玄武安山岩锆石U-Pb年代学地球化学及其动力学意义[J]. 四川地质学报, 2017, 37(3):375-382.
[8] Wang G, Xiao X L, Liu Q, et al. Zircon U-Pb age and geochemistry of basaltic andesite from the Songshunangou Au deposit and their geodynamic implication[J]. Sichuan Journal of geology, 2017, 37(3):375-382.
[9] 肖晓林. 青海松树南沟金矿矿床成因成矿预测及选矿关键技术研究[D]. 成都: 成都理工大学, 2013.
[9] Xiao X L. Research on metallogenic prediction and key technology of mineral dressing of south Songshunangou gold deposit in Qinghai[D]. Chengdu: Chengdu University of Technology, 2013.
[10] 白云. 北祁连造山带松树南沟金矿床成因与成矿预测[D]. 成都: 成都理工大学, 2019.
[10] Bai Y. Genesis and metallogenic prediction for songshunangou gold deposit in the northern Qilian orogenic belt[D]. Chengdu: Chengdu University of Technology, 2019.
[11] Wang X H, Wu W Z, Lang X H, et al. Apatite and zircon compositions as petrogenetic and metallogenic indicators for late Ordovician porphyries in the Songshunangou gold district,North Qilian orogenic belt (China)[J]. Ore Geology Reviews, 2025, 179:106502.
[12] 肖晓林, 陈岑. 青海松树南沟金矿矿床地质特征[J]. 地质与勘探, 2010, 46(2):191-197.
[12] Xiao X L, Chen C. Geological characteristics of the songshunangou gold deposit in Qinghai Province[J]. Geology and Exploration, 2010, 46(2):191-197.
[13] 王兆帅, 郎兴海, 向佐朋, 等. 基于三维地质建模的青海松树南沟金矿区找矿预测研究[J]. 物探化探计算技术, 2025, 47(4):545-556.
[13] Wang Z S, Lang X H, Xiang Z P, et al. Research on prospecting prediction of Songshunangou gold district in Qinghai Province based on Three-dimensional geological modeling[J]. Computing Techniques for Geophysical and Geochemical Exploration, 2025, 47(4):545-556.
[14] 李光明. 西藏冈底斯成矿带及邻区铜铁多金属矿成矿规律与成矿预测[M]. 北京: 地质出版社, 2011.
[14] Li G M. Metallogenic regularity and prognosis of copper-iron polymetallic deposits in Gangdise metallogenic belt and its adjacent areas in Xizang[M]. Beijing: Geological Publishing House, 2011.
[15] 韩鹏, 郎兴海, 邓煜霖, 等. 西藏谢通门县雄村矿区外围土壤地球化学特征及异常评价[J]. 物探化探计算技术, 2018, 40(6):812-819.
[15] Han P, Lang X H, Deng Y L, et al. Soil geochemical characteristics and abnormal evaluation of Xiongxcun district peripheral areas,Xietongmen county,Tibet[J]. Computing Techniques for Geophysical and Geochemical Exploration, 2018, 40(6):812-819.
[16] 裴韬, 鲍征宇. 地球化学数据去噪方法研究[J]. 地质地球化学, 1998, 26(4):86-90.
[16] Pei T, Bao Z Y. Research on noise erasing methods with geochemical data[J]. Geology-Geochemistry, 1998, 26(4):86-90.
[17] 师磊. 区域地球化学勘查数据处理方法研究[D]. 长春: 吉林大学, 2009.
[17] Shi L. Study of data processing method in regional geochemical exploration[D]. Changchun: Jilin University, 2009.
[18] 田绍海. 西藏革吉县江玛地区1∶5万水系沉积物地球化学特征及找矿预测[D]. 成都: 成都理工大学, 2019.
[18] Tian S H. Geochemical characteristics and prospecting predictions of 1∶50,000 stream sediments in Jiangma area,Geji County,Tibet[D]. Chengdu: Chengdu University of Technology, 2019.
[19] 赵荣军. 不同方法在栾川北部化探数据处理中的应用[J]. 地质与勘探, 2006, 42(3):67-71.
[19] Zhao R J. Application of different data processing method in geochemical exploration in the north Luanchuan[J]. Geology and Prospecting, 2006, 42(3):67-71.
[20] 李欢, 徐国志, 孙璐, 等. 化探综合异常图定量编制方法及应用[J]. 地质通报, 2019, 38(6):1062-1070.
[20] Li H, Xu G Z, Sun L, et al. A quantitative method for integrated anomaly map of geochemical prospecting and application[J]. Geological Bulletin of China, 2019, 38(6):1062-1070.
[21] 写熹, 魏国辉, 郭泳杰, 等. 化探综合异常的圈定——以安徽绩溪青罗山地区1∶1万土壤地球化学测量为例[J]. 矿产与地质, 2021, 35(4):763-769.
[21] Xie X, Wei G H, Guo Y J, et al. Delineation of comprehensive geochemical anomaly:An example of 1∶10,000 soil geochemical survey in Qingluoshan area,Jixi County,Anhui[J]. Mineral Resources and Geology, 2021, 35(4):763-769.
[22] 黄加忠, 杨明龙, 王晓龙, 等. 四川省瓦岗地区水系沉积物地球化学特征及找矿方向[J]. 华东地质, 2024, 45(3):332-344.
[22] Huang J Z, Yang M L, Wang X L, et al. Geochemical characteristics of stream sediments and prospecting directions in Wagang area of Sichuan Province[J]. East China Geology, 2024, 45(3):332-344.
[23] 翁望飞, 罗家元, 许振宇. 皖南外桐坑金矿床地质、地球化学特征及找矿模型[J]. 华东地质, 2023, 44(1):13-27.
[23] Weng W F, Luo J Y, Xu Z Y. Geological and geochemical characteristics and prospecting model of the Waitongkeng gold deposit in southern Anhui Province[J]. East China Geology, 2023, 44(1):13-27.
[24] 汪等 李佑国, 赵伟, 等. 异常下限衬值滤波法在然乌幅化探数据处理中的应用[J]. 物探与化探, 2013, 37(2):344-349.
[24] Wang D, Li Y G, Zhao W, et al. The application of the anomaly threshold contrast filtering method to the geochemical data processing of the ranwu sheet[J]. Geophysical and Geochemical Exploration, 2013, 37(2):344-349.
[25] 杨笑笑, 罗先熔, 郑超杰, 等. 衡阳盆地北缘国庆矿区土壤地球化学特征及找矿方向[J]. 地质与勘探, 2018, 54(4):762-771.
[25] Yang X X, Luo X R, Zheng C J, et al. Geochemical characteristics of soil and prospecting direction in the guoqing area,northern margin of the Hengyang Basin[J]. Geology and Exploration, 2018, 54(4):762-771.
[26] 杨用彪, 黄顺生, 王丽娟, 等. 溧阳盆地金山地区土壤地球化学特征及找矿效果[J]. 地质与勘探, 2023, 59(4):791-802.
[26] Yang Y B, Huang S S, Wang L J, et al. Geochemical characteristics of soil and their prospecting effect in the Jinshan area of Liyang Basin[J]. Geology and Exploration, 2023, 59(4):791-802.
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