Volume 40 Issue 2
Mar.  2021
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Luan Yan, Sun Xiaohui, Liu Minwu. Indication of elements geochemical characteristics of stream sediment to evaluation of regional denudation degree: A case study of the Dachang gold ore field in east Kunlun, Qinghai Province[J]. Bulletin of Geological Science and Technology, 2021, 40(2): 176-185, 210. doi: 10.19509/j.cnki.dzkq.2021.0216
Citation: Luan Yan, Sun Xiaohui, Liu Minwu. Indication of elements geochemical characteristics of stream sediment to evaluation of regional denudation degree: A case study of the Dachang gold ore field in east Kunlun, Qinghai Province[J]. Bulletin of Geological Science and Technology, 2021, 40(2): 176-185, 210. doi: 10.19509/j.cnki.dzkq.2021.0216

Indication of elements geochemical characteristics of stream sediment to evaluation of regional denudation degree: A case study of the Dachang gold ore field in east Kunlun, Qinghai Province

doi: 10.19509/j.cnki.dzkq.2021.0216
  • Received Date: 17 Jun 2020
  • Using the elements geochemical characteristics in stream sediments survey, have the advantages of yofast, effective and low cost in different scale evaluation of denudation degree in Dachang gold ore field in east Kunlun, Qinghai Province.It also provides strong support for evaluating the regional metallogenic potential.We take a case study of the data of 1∶50 000 stream sediments survey in the Dachang gold ore field for processing and analysis, which is based on the theory of hydrothermal percolation halo banding, and the spatial zoning of the primary halo and the structural similarity with secondary anomalies of gold deposits in the area.Besides, we build the element association and elemental banding sequence with common features between the common mineralization element dispersed train and the primary halo.Three methods, including the elemental ratio method, the triangular graphic method and the elemental banding sequence method are used to set up the evaluation parameters of regional denudation degree.Finally, combined with the characteristics of the geology and mineral resources in the field, the denudation degree of 7 anomalous areas in the Dachang gold ore field and surrounding areas is evaluated, and it is believed that the denudation degree of Zalayibei, Geyonggongma, Dongda Hariwula, and Zhaodaebei areas is higher; the degree of denudation in the Dexiran area is medium; the degree of denudation in the Zarayi-Dachang and Zhaodaenan areas is lower.Meanwhile, it is believed that the use of the elemental geochemical characteristics of stream sediments and the combined use of multiple evaluation indicators can effectively and quickly carry out a moderate evaluation of the degree of regional denudation, provide support for the evaluation of mineralization potential, and have very important indications for prospecting and exploration.

     

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  • [1]
    袁万明, 莫宣学, 王世成, 等. 东昆仑金成矿作用与区域构造演化的关系[J]. 地质与勘探, 2003, 39(3): 5-8. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKT200303001.htm
    [2]
    翟玉林, 魏俊浩, 李艳军, 等. 青海大场金矿床地质地球化学找矿模型[J]. 地质科技情报, 2015, 34(6): 100-107. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201506014.htm
    [3]
    庄玉军, 曹新志, 黄良伟, 等. 矿床剥蚀程度研究现状综述[J]. 地质科技情报, 2014, 33(1): 171-177. doi: 10.3969/j.issn.1009-6248.2014.01.015
    [4]
    徐伯骏, 费小丽, 曹新志, 等. 新疆伊犁阿希金矿床成矿深度和剥蚀程度分析[J]. 地质科技情报, 2014, 33(3): 154-162. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201403022.htm
    [5]
    魏俊浩. 初论成矿场与矿产勘查意义[J]. 地质科技通报, 2020, 39(1): 114-129 http://dzkjqb.cug.edu.cn/CN/abstract/abstract9932.shtml
    [6]
    Cheng Q M. Mapping singularities with stream sediment geochemical data for prediction of undiscovered mineral deposits inGejiu, Yunnan Province, China[J]. Ore Geology Reviews, 2007, 32(1/2): 314-324. http://www.sciencedirect.com/science/article/pii/S0169136806001119
    [7]
    Cheng Q M, Zhao P D. Singularity theories and methods for characterizing mineralization processes and mapping geo-anomalies for mineral deposit prediction[J]. Geoscience Frontiers, 2011, 2(1): 67-79. doi: 10.1016/j.gsf.2010.12.003
    [8]
    Cheng Q M. Singularity theory and methods for mapping geochemical anomalies caused by buried sources and for predicting undiscovered mineral deposits in covered areas[J]. Journal of Geochemical Exploration, 2012, 122: 55-70. doi: 10.1016/j.gexplo.2012.07.007
    [9]
    Zuo R G, Carranza E J M, Wang J. Spatial analysis and visualization of exploration geochemical data[J]. Earth-Science Reviews, 2016, 158: 9-18. doi: 10.1016/j.earscirev.2016.04.006
    [10]
    于家明, 张辉, 陆学普, 等. 区域化探异常元素分带与找矿远景分析[J]. 吉林地质, 2007, 26(2): 37-46, 62. doi: 10.3969/j.issn.1001-2427.2007.02.008
    [11]
    耿国帅. 安徽绩溪东部化探工作区剥蚀程度及主攻矿种浅析[J]. 矿床地质, 2010, 29(增刊2): 173-180. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ2010S2028.htm
    [12]
    黄文斌, 罗先熔, 刘攀峰, 等. 青海省石灰沟地区水系沉积物测量地球化学特征及找矿预测[J]. 地质科技通报, 2020, 39(3): 150-159. http://dzkjqb.cug.edu.cn/CN/abstract/abstract10032.shtml
    [13]
    贾琳, 石文杰, 魏俊浩, 等. 水平总梯度法在化探异常圈定中的应用: 以青海省某地区1∶5万水系沉积物地球化学测量为例[J]. 地质科技情报, 2019, 38(5): 71-80 https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201905007.htm
    [14]
    李胜荣, 侯增谦. 西藏冈底斯带区域性断裂与金矿床剥蚀程度: Ag/Au比值的启示[J]. 中国科学: 地球科学, 2001, 31(B12): 104-108. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK2001S1015.htm
    [15]
    姜启明, 鲁挑建. 甘肃金山金矿床伴生元素特征及矿床剥蚀程度研究[J]. 黄金, 2011, 32(10): 10-16. https://www.cnki.com.cn/Article/CJFDTOTAL-HJZZ201110005.htm
    [16]
    康太翰, 于洪顺. 利用异常元素水平分带序列评价矿床剥蚀程度: 以兰家、八台岭、官马金矿为例[J]. 吉林地质, 1997, 16(1): 57-62. https://www.cnki.com.cn/Article/CJFDTOTAL-JLDZ701.007.htm
    [17]
    金献革. 矿床原生晕元素空间分带序列计算方法研究[J]. 科技与企业, 2012(20): 274-275. https://www.cnki.com.cn/Article/CJFDTOTAL-KJYQ201220257.htm
    [18]
    Singer D A, Kouda R. Some simple guides to finding useful information in exploration geochemical data[J]. Natural Resources Research, 2001, 10(2): 137-147. doi: 10.1023/A:1011552810482
    [19]
    Ding Q F, Jiang S Y, Sun F Y, et al. Origin of the Dachang gold deposit, NW China: Constraints from H, O, S, and Pb isotope data[J]. International Geology Review, 2013, 55(15): 1885-1901. doi: 10.1080/00206814.2013.804687
    [20]
    夏锐, 邓军, 卿敏, 等. 青海大场金矿田矿床成因: 流体包裹体地球化学及H-O同位素的约束[J]. 岩石学报, 2013, 29(4): 1358-1376. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201304021.htm
    [21]
    王发明, 翟玉林, 李艳军, 等. 青海大场金矿田北缘灭格滩矿区土壤地球化学异常信息提取及找矿预测[J]. 地质科技情报, 2015, 34(5): 127-133. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201505020.htm
    [22]
    Ding Q F, Wang G, Sun F Y. Ore-forming fluid evolution of Dachang gold deposit in Qumalai County, Qinghai Province: Evidence from fluid inclusion study and arsenopyrite geothermometer[J]. Acta Petrologica Sinica, 2010, 26(12): 3709-3719. http://www.researchgate.net/publication/305534009_Ore-forming_fluid_evolution_of_Dachang_gold_deposit_in_Qumalai_County_Qinghai_Province_Evidence_from_fluid_inclusion_study_and_arsenopyrite_geothennometer
    [23]
    赵财胜, 孙丰月, 毛景文, 等. 青海大场金矿床流体包裹体特征及其地质意义[J]. 矿床地质, 2005, 24(3): 305-316. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ200503009.htm
    [24]
    李琳业, 俞长捷, 戴梅芳, 等. 青海省大场金矿床地质特征及找矿远景分析[J]. 青海大学学报: 自然科学版, 2009, 27(1): 11-19. https://www.cnki.com.cn/Article/CJFDTOTAL-QHXZ200901003.htm
    [25]
    Wang S L, Qu C X, Liu W. Geophysical-geochemical anomaly characteristics and prospecting marks of Dachang gold deposit in Qinghai[J]. Applied Mechanics and Materials, 2013, 448/453: 3792-3796.
    [26]
    李惠, 张文华, 刘宝林, 等. 中国主要类型金矿床的原生晕轴向分带序列研究及其应用准则[J]. 地质与勘探, 1999, 35(1): 3-5. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKT901.008.htm
    [27]
    蒋敬业, 程建萍, 祁士华, 等. 应用地球化学[M]. 武汉: 中国地质大学出版社, 2006: 68.
    [28]
    Vilà M, Martínez-Lladó X. Approaching earth surface geochemical variability from representative samples of geological units: The Congost River Basin case study[J]. Journal of Geochemical Exploration, 2015, 148: 79-95. http://www.sciencedirect.com/science/article/pii/S0375674214003008
    [29]
    骆地伟, 姚书振, 王成相, 等. 黔西南卡林型金矿剥蚀程度评价[J]. 地球科学: 中国地质大学学报, 2016, 41(2): 199-217. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201602003.htm
    [30]
    向运川. 化探资料应用技术要求[M]. 北京: 地质出版社, 2010.
    [31]
    陈静. 青海省大场金矿矿床地质特征及其成因意义[D]. 西安: 西北大学, 2012.
    [32]
    Xie S Y, Cheng Q M, Xing X T, et al. Geochemical multifractal distribution patterns in sediments from ordered streams[J]. Geoderma, 2010, 160(1): 36-46. http://www.sciencedirect.com/science/article/pii/S0016706110000352
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