青海省阿达滩沟脑矿区地质特征及综合成矿预测
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  • 英文篇名:Geological Characteristics and Integrated Metallogenic Prediction of Adatangounao Mining Area in Qinghai Province
  • 作者:张庆华 ; 宋小军 ; 罗洪远
  • 英文作者:Zhang Qinghua;Song Xiaojun;Luo Hongyuan;Geological and Mineral Resource Exploration Institute of Non-ferrous Metals and Nuclear Industry Geological Exploration Bureau of Guizhou;
  • 关键词:铅锌多金属矿 ; 水系沉积物测量 ; 高精度磁测 ; 土壤地球化学测量 ; 成矿规律 ; 找矿靶区
  • 英文关键词:Pb-Zn polymetallic deposit;;Stream sediment survey;;High-precision magnetic measurement;;Soil geochemical measurement;;Metallogenic regularity;;Prospecting target area
  • 中文刊名:JSKS
  • 英文刊名:Metal Mine
  • 机构:贵州省有色金属和核工业地质勘查局地质矿产勘查院;
  • 出版日期:2019-05-15
  • 出版单位:金属矿山
  • 年:2019
  • 期:No.515
  • 基金:青海省地质勘查基金项目(编号:KD2012-06)
  • 语种:中文;
  • 页:JSKS201905018
  • 页数:10
  • CN:05
  • ISSN:34-1055/TD
  • 分类号:112-121
摘要
青海祁漫塔格地区位于东昆仑造山带西段,区内经历了多期次、多阶段的复杂构造—岩浆活动,是青藏高原北部最重要的铁铜铅锌多金属成矿带。阿达滩沟脑位于祁漫塔格铁多金属成矿带上,区内岩浆活动强烈,断层发育,具有良好的找矿潜力。为查明该区成矿条件,选择未经查证的3处1∶50 000水系沉积物Hs_(乙3)~7、Hs_(乙3)~8和Hs_丙~6综合异常和高精度磁测C16号异常开展大比例尺地质测量、高精度磁测及土壤地球化学剖面测量工作,结合地质调查成果对异常高值区布置探槽进行查证,以查明矿致异常源和分布特征,并对成矿规律进行初步总结。研究表明:①土壤样品中Cu、Ni、Co是区内的主成矿元素且相关性好,其中Ni富集成矿的可能性较大,在剖面图上,Cu、Ni、Co、Cr高值异常分布较广,浓集中心相对突出;②高精度磁测在C16异常中心附近的异常强度尤为强烈,异常值与中酸性岩体,辉长、辉绿岩体以及NW向断裂构造吻合较好;③在地表矿化点及异常区地段经探槽工程查证,圈出了5条铅锌铜矿化带,7条矿体(其中5条铅锌矿体,2条铜矿体),圈定了可靠的找矿靶区,并进行了找矿潜力分析。上述分析进一步表明:该类矿体的发现加深了对区内成矿地质条件的认识,在高海拔地区采用地质、物探、化探综合勘查方法,并与成矿规律研究紧密结合,可实现找矿突破。
        Qimantag area of Qinghai Province is located in the western part of East Kunlun Orogenic Belt,which possesses a complicated evolutional history and unique tectonic process.It is the most important polymetallic ore accumulated area in Northern Qinghai-Tibet Plateau.Adatangounao is located in the Qimantage iron-polymetallic metallogenic belt.In this area,the magmatic activity is strong,the faults is well developed and the prospecting potential is good.In order to find out the metallogenic conditions in this area,large-scale geological survey,high-precision magnetic survey and soil profile measurement are carried out on the basis of unconfirmed three 1∶50 000 stream sediment survey Hs_(乙3)~7、Hs_(乙3)~8 and Hs_丙~6 comprehensive anomalies and high-precision magnetic measurement C16 anomaly. The anomalous high concentration is performed by exploratory trenches,combined with geological survey to identify the source and distribution characteristics of the mining area and to summarize the metallogenic regularity.The study results show that:①Cu,Ni and Co are the main metallogenic elements in the soil samples and have good correlation,among them,possibility of enrichment and mineralization of Ni is high,high-value anomalies of Cu,Ni,Co and Cr are widely distributed in the profile,the concentration centers are relatively prominent;②the anomaly intensity of high-precision magnetic measurement is especially strong near C16 anomaly center,the abnormal value is consistent with the intermediate to acidic intrusive rocks,gabbro plutons,diabase dikes and NW trending regional faults;③five lead-zinc-copper mineralization zones and seven orebodies(including five lead-zinc orebodies and two copper orebodies)have been delineated by the exploratory trenches in the surface mineralization point and the anomalous area,reliable prospecting target area is delineated,and its prospecting potential is discussed.The above analysis results further indicated that the discovery of the orebodies have deepened the understanding of metallogenic conditions in Adatangounao Mining Area,and prospecting breakthrough can be obtained by using integrated exploration methods of geology,geophysical exploration and geochemical exploration,in close association with metallogenic regularity.
引文
[1]姜春发,王宗起,李锦轶.中央造山带开合构造[M].北京:地质出版社,2000.Jiang Chunfa,Wang Zongqi,Li Jinyi.Opening-closing Tectonics of Central Orogenic Belt[M].Beijing:Geological Publishing House,2000.
    [2]边千韬,赵大升,叶正仁,等.初论秦祁昆缝合系[J].地球学报,2002,23(6):501-508.Bian Qiantao,Zhao Dasheng,Ye Zhengren,et al.A preliminary study of the Kunlun-Qilian-Qinling suture system[J].Acta Geoscientia Sinica,2002,23(6):501-508.
    [3]李荣社,计文化,赵振明,等.昆仑早古生代造山带研究进展[J].地质通报,2007,26(4):373-382.Li Rongshe,Ji Weihua,Zhao Zhenming,et al.Progress in the study of the Early Paleozoic Kunlun orogenic belt[J].Geological Bulletin of China,2007,26(4):373-382.
    [4]刘渭,杨兴科,王守良,等.青海省祁漫塔格矿带虎头崖矿田构造控矿特征[J].中国地质,2014,41(1):222-234.Liu Wei,Yang Xingke,Wang Shouliang,et al.Characteristics of ore-controlling structures of the Hutouya orefield in the Qimantage metallogenic belt,Qinghai Province[J].Geology in China,2014,41(1):222-234.
    [5]黄敏,赖健清,马秀兰,等.青海省肯德可克多金属矿床地球化学特征与成因[J].中国有色金属学报,2013,23(9):2659-2670.Huang Min,Lai Jianqing,Ma Xiulan,et al.Geochemical characteristics and genesis of Kendekeke deposit in Qinghai Province,China[J].The Chinese Journal of Nonferrous Metals,2013,23(9):2659-2670.
    [6]张爱奎,刘光莲,莫宣学,等.青海祁漫塔格晚古生代-早中生代侵入岩构造背景与成矿关系[J].西北地质,2012,45(1):9-19.Zhang Aikui,Liu Guanglian,Mo Xuanxue,et al.Relationship between tectonic settings and metallogenesis of late Paleozoic-Early Mesozoic intrusive rock in Qimantage,Qinghai Province[J].Northwestern Geology,2012,45(1):9-19.
    [7]丰成友,李东生,吴正寿,等.东昆仑祁漫塔格成矿带矿床类型、时空分布及多金属成矿作用[J].西北地质,2010,43(4):10-17.Feng Chengyou,Li Dongsheng,Wu Zhengshou,et al.Major type,time-space distribution and metallogeneses of polymetallic deposits in the Qimantage metallogenic belt,Eastern Kunlun Area[J].Northwestern Geology,2010,43(4):10-17.
    [8]徐文艺,张德全,阎升好,等.东昆仑地区矿产资源大调查进展与前景展望[J].中国地质,2001,28(1):25-29.Xu Wenyi,Zhang Dequan,Yan Shenghao,et al.Progress and foreground expectation of mineral resource survey in the Eastern Kunlun Area[J].Geology in China,2001,28(1):25-29.
    [9]赵一鸣,丰成友,李大新.中国矽卡岩矿床找矿新进展和时空分布规律[J].矿床地质,2017,36(3):519-543.Zhao Yiming,Feng Chengyou,Li Daxin.New progress in prospecting for skarn deposits and spatial-teporal distribution of skarn deposits in China[J].Mineral Deposits,2017,36(3):519-543.
    [10]高鹏,耿涛,冀显坤,等.青海祁漫塔格成矿带地球物理方法找矿有效性试验[J].地质与勘探,2017,53(5):923-934.Gao Peng,Geng Tao,Ji Xiankun,et al.Effectiveness experiments of geophysical methods in the Qimantage metallogenic belt of Qinghai Province[J].Geology and Exploration,2017,53(5):923-934.
    [11]黎存林,代岩,王雪萍,等.青海省格尔木市哈西亚图地区铁多金属矿床的发现及意义[J].西北地质,2012,45(1):222-228.Li Cunlin,Dai Yan,Wang Xueping,et al.Discover and significance of the iron-polymetallic deposits in Haxiyatu Area of Golmud City in Qingha[iJ].Northwestern Geology,2012,45(1):222-228.
    [12]佘宏全,张德全,景向阳,等.青海省乌兰乌珠尔斑岩铜矿床地质特征与成因[J].中国地质,2007,34(2):306-314.She Hongquan,Zhang Dequan,Jing Xiangyang,et al.Geological characteristics and genesis of the Ulan Uzhur porphyry copper deposit in Qingha[iJ].Geology in China,2007,34(2):306-314.
    [13]张晓飞,李智明,贾群子,等.青海祁漫塔格虎头崖多金属矿区花岗斑岩地球化学、年代学特征及其地质意义[J].吉林大学学报:地球科学版,2016,46(3):749-765.Zhang Xiaofei,Li Zhiming,Jia Qunzi,et al.Geochronology,geochemistry and geological significance of granite Porphyry in Hutouya polymetallic deposit,Qimantage Area,Qinghai Province[J].Journal of Jilin University:Earth Science Edition,2016,46(3):749-765.
    [14]舒树兰,何书跃,李彬,等.青海东昆仑鸭子沟多金属矿床地质地球化学特征及找矿前景分析[J].西北地质,2014,47(2):62-72.Shu Shulan,He Shuyue,Li Bin,et al.Geology,geochemical characteristics and prospecting analysis of Yazigou polymetallic deposit,East Kunlun,Qinghai Province[J].Northwestern Geology,2014,47(2):62-72.
    [15]张爱奎,莫宣学,李云平,等.青海西部祁漫塔格成矿带找矿新进展及其意义[J].地质通报,2010,29(7):1062-1074.Zhang Aikui,Mo Xuanxue,Li Yunping,et al.New progress and significance in the Qimantage metallogenic belt prospecting,Western Qinghai,China[J].Geological Bulletin of China,2010,29(7):1062-1074.
    [16]何书跃,舒树兰,刘永乐,等.青海祁漫塔格地区有效找矿方法总结[J].矿床地质,2013,32(1):187-194.He Shuyue,Shu Shulan,Liu Yongle,et al.Summary of effective prospecting methods in Qimantag Area,Qinghai Province[J].Mineral Deposits,2013,32(1):187-194.
    [17]赵一鸣,丰成友,李大新.青海西部祁漫塔格地区主要矽卡岩铁多金属矿床成矿地质背景和矿化蚀变特征[J].矿床地质,2013,32(1):1-19.Zhao Yiming,Feng Chengyou,Li Daxin.Metallogenic setting and mineralization-alteration characteristics of major skarn Fe-polymetallic deposit in Qimantag Area,Western Qinghai Province[J].Mineral Deposits,2013,32(1):1-19.
    [18]何书跃,祁兰英,舒树兰,等.青海祁漫塔格地区斑岩铜矿的成矿条件和远景[J].地质与勘探,2008,44(2):14-22.He Shuyue,Qi Lanying,Shu Shulan,et al.Metallogenic environment and potential in the Qimantage porphyry copper deposit,Qingha[iJ].Geology and Exploration,2008,44(2):14-22.
    [19]马永寿,拜永山,何皎,等.祁漫塔格地区泛非期二长花岗岩的发现及意义[J].青海大学学报:自然科学版,2010,28(5):56-60.Ma Yongshou,Bai Yongshan,He Jiao,et al.Discovery of erchang granite in Qimantage Region in Pan-African period and its significance[J].Journal of Qinghai University:Natural Science,2010,28(5):56-60.
    [20]杨兴科,刘渭,何虎军,等.青海祁漫塔格景忍-虎头崖矿田地质与找矿:岩浆热力构造类型与构造岩相填图[J].地学前缘,2015,22(4):104-112.Yang Xingke,Liu Wei,He Hujun,et al.The geology and prospecting of Jingen-Hutouya orefield in Qimantage of Qinghai Province:type of magma-thermodynamic structure and structure-lithofacies geological mapping[J].Earth Science Frontiers,2015,22(4):104-112.
    [21]潘蔚,余长发,田青林,等.青海祁漫塔格中段铀成矿要素分析与远景预测[J].铀矿地质,2016,32(3):146-151.Pan Wei,Yu Zhangfa,Tian Qinglin,et al.Key factors of uranium mineralization and prospect prognosis in the middle of Qimantage,Qingha[iJ].Uranium Geology,2016,32(3):146-151.
    [22]宋忠宝,张雨莲,贾群子,等.青海祁漫塔格地区野马泉花岗闪长岩LA-ICP-MS锆石U-Pb年龄[J].地质通报,2016,35(12):2006-2013.Song Zhongbao,Zhang Yulian,Jia Qunzi,et al.LA-ICP-MS zircon U-Pb age of the Yemaquan granodiorite in the Qimantag Area,Qinghai Province and its geological implications[J].Geological Bulletin of China,2016,35(12):2006-2013.
    [23]保广普,王国良,刘荣.喀雅克登塔格地区两期基性岩墙的岩石化学特征及意义[J].西北地质,2013,46(2):37-43.Bao Guangpu,Wang Guoliang,Liu Rong.Kayakedengtage area two basic dike rocks geochemistry and significance[J].Northwestern Geology,2013,46(2):37-43.
    [24]青海省区调综合地质大队.1∶20万土窑洞幅(J-46-19)、茫崖幅(J-46-20)区域地质调查报告[R].西宁:青海省地质矿产局,1986.Qinghai Regional Geological Survey and Comprehensive Research Team.Regional geological survey report of 1∶200 000 Tujiao(J-46-19)and Mangya(J-46-20)[R].Xining:Bureau of Geology and Mineral Resources of Qinghai Province,1986.
    [25]叶占福,王国良,李五福,等.青海省喀雅克登塔格地区1:5万区域地质调查报告[R].西宁:青海省地质调查院,2010.Ye Zhanfu,Wang Guoliang,Li Wufu,et al.1:50 000 regional geological survey report in the Kayakedengtage area of Qinghai Province[R].Xining:Qinghai Geological Survey Institute,2010.
    [26]黎彤.化学元素的地球丰度[J].地球化学,1976(3):167-174.Li Tong.Chemical element abundances in the earth and its major shells[J].Geochimica,1976(3):167-174.
    [27]许光,刘长征,赵娟,等.青海省矿产资源潜力评价地球化学资料应用成果报告[R].西宁:青海省地质矿产勘查开发局,2011.Xu Guang,Liu Changzheng,Zhao Juan,et al.Report on application results of geochemical data for mineral resources potential evaluation in Qinghai Province[R].Xining:Bureau of Geology and Mineral Exploration and Development of Qinghai Province,2011.
    [28]于俊博,宋云涛,郭志娟,等.R型聚类分析在区域化探元素分组中的作用探讨[J].物探化探计算技术,2014,36(6):771-776.Yu Junbo,Song Yuntao,Guo Zhijuan,et al.Discussion on the affection of the R-cluster analysis applied in grouping elements in regional geochemical exploration[J].Computing Techniques for Geophysical and Geochemical Exploration,2014,36(6):771-776.
    [29]丰成友,李东生,吴正寿,等.东昆仑祁漫塔格成矿带矿床类型、时空分布及多金属成矿作用[J].西北地质,2010,43(4):10-17.Feng Chengyou,Li Dongsheng,Wu Zhengshou,et al.Major types,time-space distribution and metallogeneses of polymetallic deposits in the Qimantage metallogenic belt,Eastern Kunlun Area[J].Northwestern Geology,2010,43(4):10-17.
    [30]温汉捷,肖化云,俞广钧.构造地球化学探矿方法的应用--以山东招远魏家沟金矿床为例[J].地质与勘探,1999,35(3):32-35.Wen Hanjie,Xiao Huayun,Yu Guangjun.Weijiagou Gold Deposit in Shandong:application of tectonic geochemistry to prospecting[J].Geology and Exploration,1999,35(3):32-35.
    [31]吴德海,潘家永,钟福军,等.安徽小紫山地区铜多金属矿土壤地球化学特征及找矿前景[J].金属矿山,2017(1):119-125.Wu Dehai,Pan Jiayong,Zhong Fujun,et al.Soil geochemical characteristics and prospecting potential of Cu-polymetallic deposit in Xiaozishan Area,Anhui Province[J].Metal Mine,2017(1):119-125.

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