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Gold Science and Technology >

2019 , Vol. 27 >Issue 6: 816 - 825

DOI: https://doi.org/10.11872/j.issn.1005-2518.2019.06.816

Mineral Exploration and Resource Evaluation

Characteristics of Soil Geochemical Anomalies and Prospecting Potential of Tanbeixuefeng Area in Qinghai Province

  • Baokai YANG , 1 ,
  • Meijun XU 1 ,
  • Rui CAO 1 ,
  • Yang YU 1 ,
  • Yongjian XIE 1 ,
  • Anquan HE 2
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  • 1. Qingdao Geological Engineering Investigation Institute，Qingdao 266100，Shandong，China
  • 2. The Third Institution of Qinghai Geological Prospecting，Xining 810029，Qinghai，China

Received date: 2019-03-19

  Revised date: 2019-06-24

  Online published: 2019-12-24

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Highlights

Qimantage metallogenic belt is located in the western part of the East Kunlun Mountains.It is an important metallogenic belt in the western part of China.Superior metallogenic geological conditions have resulted in abundant mineral resources in this region.In recent years，a large number of mineral deposits related to intermediate-acid magmatic activities have been discovered in the Qimantage metallogenic belt.The genetic types of the deposits are mainly skarn，porphyry，high temperature hydrothermal，sedimentary metamorphic，sedimentary，hot water sedimentary-reformed and volcanic rock type.The minerals include copper，iron，lead，zinc and other metals.Tanbeixuefeng is a newly discovered tectonic altered type gold deposit in the region, which is located in the Qimantage back-arc rift basin，and the metallogenic geological conditions are very favorable.In this study，through 1∶10 000 soil geochemical survey in Tanbeixuefeng area，the results shows that Au is an important enriched element with a large coefficient of variation，indicating that there is superimposition of late stage mineralization.Moreover,R-type cluster analysis shows that Au and Bi are significantly positively correlated，indicating that Au mineralization may be related to mesothermal and low-temperature hydrothermal activities.Further analysis of geochemical characteristics of elements，combined with geological background，13 comprehensive soil anomalies dominated by gold have been delineated， trench prospecting has been carried out in AP7 and AP9 anomalous areas.A gold mineralization alteration zone has also been found，and three gold orebodies have been delineated in the zone.The gold orebodies are developed in the NW-trending structural fracture zone，as well as joint structure.The ore-hosting lithology is silicified altered rock and strong limonization.Several gold mineralization clues have been found on the surface，such as silicification，sericitization，and pyritization.Furthermore,based on the analysis of metallogenic geological conditions，the prospecting criteria of geology，geochemistry and structure are preliminarily established.Moreover，the genesis of the deposit is discussed and analyzed.Therefore，this study point out the prospecting direction in the Tanbeixuefeng area as follows：（1） The Au is already found in the No.1 mineralized alteration zone，thus the drilling should be carried out；（2） Compared the No.1 mineralized alteration zone，the prospecting should be focussed on the NWW fault；（3） Other unidentified Au high-value points in soil anomalies；（4） Other unchecked Au high-value points in soil anomalies，and Au and As combination anomalies should be strengthen prospecting work.It is a favorable area of prospecting for structural altered type gold deposits.Surface tracing and deep verification work in this area are expected to make breakthrough prospecting progress.

Cite this article

Baokai YANG , Meijun XU , Rui CAO , Yang YU , Yongjian XIE , Anquan HE . Characteristics of Soil Geochemical Anomalies and Prospecting Potential of Tanbeixuefeng Area in Qinghai Province[J]. Gold Science and Technology, 2019 , 27(6) : 816 -825 . DOI: 10.11872/j.issn.1005-2518.2019.06.816

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References

Publishing order | Descend order by publishing year | Descend order by cited within
1
杨生德，王彦，任家骐，等.青海省第三轮成矿远景区划研究及找矿靶区预测[R].西宁：青海省地质矿产勘查开发局，2013.

Yang Shengde， Wang Yan， Ren Jiaqi，et al.The third round metallogenic prospective zoning and prospecting target prediction in Qinghai Province[R].Xining：Qinghai Bureau of Geology and Mineral Resources，2013.

2
丰成友，李东生，吴正寿，等.东昆仑祁漫塔格成矿带矿床类型、时空分布及多金属矿成矿作用[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.

3
张雨莲，贾群子，宋忠宝，等.青海省卡尔却卡铜多金属矿床A区斑岩型和B区矽卡岩型成矿岩体特征对比[J].西北地质，2014，47（4）：114-122.

Zhang Yulian， Jia Qunzi， Song Zhongbao，et al.Contrastive study on features of ore-forming rock mass between area A porphyry type and area B skarn type in Ka’erqueka copper molybdenum deposit in Qinghai Province[J].Northwestern Geology，2014，47（4）：114-122.

4
于淼，丰成友，保广英，等.青海尕林格铁矿床矽卡岩矿物学及蚀变分带[J].矿床地质，2013，32（1）：55-76.

Yu Miao， Feng Chengyou， Bao Guangying，et al.Characteristics and zonation of skarn in Galinge iron deposit，Qinghai Province[J].Mineral Deposit，2013，32（1）：55-76.

5
李侃，高永宝，钱兵，等.东昆仑祁漫塔格虎头崖铅锌多金属矿区花岗岩年代学、地球化学及Hf同位素特征[J].中国地质，2015，42（3）：630-645.

Li Kan， Gao Yongbao， Qian Bing，et al.Geochronology，geochemical characteristics and Hf isotopic compositions of granite in the Hutouya deposit，Qimantag，East Kunlun[J].Geology in China，2015，42（3）：630-645.

6
张爱奎，刘光莲，丰成友，等.青海省虎头崖多金属矿床地球化学特征及成矿—控矿因素研究[J].矿床地质，2013，21（1）：94-108.

Zhang Aikui， Liu Guanglian， Feng Chengyou，et al.Geochemical characteristics and ore-controlling factors of Hutouya polymetallic deposit，Qinghai Province[J].Mineral Deposits，2013，21（1）：94-108.

7
宋忠宝，贾群子，张占玉，等.东昆仑祁漫塔格地区野马泉铁铜矿床地质特征及成因探讨[J].西北地质，2010，43（4）：209-217.

Song Zhongbao， Jia Qunzi， Zhang Zhanyu，et al.Study on geological feature and origin of Yemaquan Fe-Cu deposit in Qimantage area，Eastern Kunlun[J].Northwestern Geology，2010，43（4）：209-217.

8
Zhang A K， Mo X X， Yuan W M，et al.Petrogensis and tectonic setting of the Yemaquan granite from the iron polymetall ore area of Qimantage，Eastern Kunlun Mountains，Qinghai-Tibet Plateau[J].Island Arc，2017（1）：e12190.

9
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.

10
苏旭亮，赵永亮，赵闯，等.东昆仑祁漫塔格克停哈尔斑岩型铜钼矿找矿思路突破及找矿模型[J].中国地质，2013，41（6）：2048-2062.

Su Xuliang， Zhao Yongliang， Zhao Chuang，et al.Prospecting thinking and model for the Ketinghaer porphyry copper molybdenum deposit in the East Kunlun Mountains[J].Geology in China，2014，41（6）：2048-2062.

11
杨宝凯，何安全，苏旭亮，等.青海省茫崖行委滩北雪峰地区多金属矿调查评价报告[R].西宁：青海省第三地质矿产勘查院，2016.

Yang Baokai， He Anquan， Su Xuliang，et al.Report of investigation and evaluation in Tanbeixuefeng in Mangya Xingwei，Qinghai Province[R].Xining：The Third Institution of Qinghai Geological Mineral Prospecting，2015.

12
杨生德，吴正寿，赵呈祥，等.青海省矿产资源潜力评价成果报告[R].西宁：青海省地质矿产勘查开发局，2013.

Yang Shengde， Wu Zhengshou， Zhao Chengxiang，et al.The potential of mineral resources in Qinghai Province evaluation report[R].Xining：Qinghai Bureau of Geology and Mineral Resources，2013.

13
李荣社，计文化，杨永成.昆仑山及邻区地质[M].北京：地质出版社，2008.

Li Rongshe， Ji Wenhua， Yang Yongcheng.Geology of Kunlun Mountains and Adjacent Areas[M].Beijing：Geological Publishing House，2008.

14
臧金生，王东晓，赵瑞强.化探异常定量评价[J].物探与化探，2014，38（6）：1114-1118.

Zang Jinsheng， Wang Dongxiao， Zhao Ruiqiang.Quantitative evaluation of geochemical anomalies［J］.Geophysical and Geochemical Exploration，2014，38（6）：1114-1118.

15
黎彤，袁怀雨.大洋岩石圈和大陆岩石圈的元素丰度[J].地球化学，2011，40（1）：1-5.

Li Tong， Yuan Huaiyu.Element abundance in the oceanic and the continental lithospheres[J].Geochimica，2011，40（1）：1-5.

16
阳正熙.地学数据分析教程[M].北京：科学出版社，2008.

Yang Zhengxi.Geological Data Analysis Tutorial[M].Beijing：Science Press，2008.

17
刘珊，陈亮，段先哲，等.土壤地球化学在黔东八瓢达冲金矿勘查中的应用与找矿效果[J].物探与化探，2016，40（1）：27-32.

Liu Shan， Chen Liang， Duan Xianzhe，et al.The application of soil geochemistry survey to prospecting in the Bapiao Dachong gold ore district of eastern Guizhou Province and its effect［J］.Geophysical and Geochemical Exploration，2016，40（1）：27-32.

18
刘洪微.云南省景谷帕断山矿区土壤地球化学测量效果及找矿前景[J].物探与化探，2017，41（4）：619-626.

Liu Hongwei.The applying effect of geochemical soil survey at the Paduanshan mining area in Jinggu County，Yunnan Province，and prospecting potential［J］.Geophysical and Geochemical Exploration，2017，41（4）：619-626.

19
王福德，李云平，贾妍慧.青海金矿成矿规律及找矿方向[J].地球科学与环境学报，2018，40（2）：162-175.

Wang Fude， Li Yunping， Jia Yanhui.Metallogenic regularity and prospecting direction of gold deposits in Qinghai，China[J].Journal of Earth Sciences and Environment，2018，40（2）：162-175.

20
Deng J， Wang Q F.Gold mineralization in China：Metal-logenic Province，deposit types and tectonic framework[J].Gondwana Research，2016，36：219-274

21
Yuan W M， Mo X X， Zhang A K，et al.Fission track thermochronology evidence for multiple periods of mineralization in the Wulonggou gold deposits，Eastern Kunlun Mountains，Qinghai Province[J].Journal of Earth Science，2013，24（4）：471-478.

22
潘彤，王福德.初论青海省金矿成矿系列[J].黄金科学技术，2018，26（4）：423-430.

Pan Tong， Wang Fude.Preliminary discusion on minerogentic series of gold deposits in Qinghai Province[J].Gold Science and Technology，2018，26（4）：423-430.

23
管波，苏胜年，杨青云，等.青海苦海地区金矿找矿远景浅析[J].黄金科学技术，2012，20（3）：35-39.

Guan Bo， Su Shengnian， Yang Qingyun.Analsis on gold prospecting potential of Kuhai Area in Qinghai Province[J].Gold Science and Technology，2012，20（3）：35-39.

24
陈超，牛树银，赵夫旺.太行山中段丑泥口金矿找矿前景分析[J].黄金科学技术，2016，24（5）：32-39.

Chen Chao， Niu Shuyin， Zhao Fuwang.Study on prospecting potential of Chounikou gold deposit in the middle of Taihang Mounttains[J].Gold Science and Technology，2016，24（5）：32-39．

25
鞠培姣.山西灵丘县梨园金矿地质特征及控矿因素分析[J].黄金科学技术，2018，26（6）：706-717．

Ju Peijiao.Geological characteristics and ore-controlling factors of Liyuan gold deposit，Shanxi Province[J].Gold Science and Technology，2018，26（6）：706-717.

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