THE PROSPECTING EFFECT OF DEBRIS GEOCHEMICAL SURVEY IN THE XIAOBINGGOU LEAD-ZINC MINING AREA IN SUBEI, GANSU ROVINCE
YE Hong-gang1,2, ZHANG De-hui1, CHENG Zhu-hua2, YE Hong-feng3, WU Hu1,4
1. Faculty of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China; 2. No.4 Geological and Mineral Survey, Bureau of Gansu Geological Survey, Jiuquan 735000, China; 3. No.3 Geological and Mineral Survey, Bureau of Gansu Geological Survey, Lanzhou 730000, China; 4. Hubei Bureau of Coal Geological Exploration, Wuhan 430070, China
Abstract：The Xiaobinggou lead-zinc mining area is located in the Qilian cold landscape zone. With the R-model factor analysis method and parameter statistics based on data of 1：10 000 debris survey, the authors revealed the element assemblages in the study area, and delineated the single element anomalies and the comprehensive anomalies. Through the first-level anomaly inspection in the three sifted comprehensive anomaly areas which consists of geophysical exploration method, 1：10 000 field geological mapping and different degrees of trenching and adit exploration as well as drilling, the authors outlined the ideal ore bodies and achieved breakthrough in prospecting. Debris geochemical survey has been relatively rarely employed in this region, but the success of this method in guiding the prospecting work has proved its high efficiency in the Xiaobinggou lead-zinc mining area. So, debris geochemical survey can provide a reference for ore-prospecting work in the same sort of geochemical landscape areas.
叶红刚, 张德会, 程主华, 叶红锋, 吴胡. 岩屑地球化学测量在小冰沟铅锌矿区的找矿效果[J]. 物探与化探, 2014, 38(2): 295-303.
YE Hong-gang, ZHANG De-hui, CHENG Zhu-hua, YE Hong-feng, WU Hu. THE PROSPECTING EFFECT OF DEBRIS GEOCHEMICAL SURVEY IN THE XIAOBINGGOU LEAD-ZINC MINING AREA IN SUBEI, GANSU ROVINCE. Geophysical and Geochemical Exploration, 2014, 38(2): 295-303.
[1] Robbins D A.Applied geology in the discovery of the Spokane Mountain uranium deposit, Washington[J].1978,73(8):1523-1538. [2] Boyle R W.Geochemical methods for the discovery of blind mineral deposits[J].,1982,65(844):123-142. [3] 刘崇民,李应桂,史长义.不同景观区的岩石地球化学勘查方法研究[J].物探与化探,2002,(01):23-26. [4] 奚小环,李敏.中国区域化探若干基本问题研究:1999~2009[J].中国地质,2012(02):267-282. [5] 赵海如,张跃矩,张导训.甘肃省肃北县小冰沟及掉石沟一带物化探普(详)查工作成果报告[R].甘肃地矿局物探队,1987. [6] 张松林.甘肃省肃北蒙古族自治县小冰沟锡、铅、锌矿点踏勘检查报告[R].甘肃省地矿局酒泉地质矿产调查队,1986. [7] 惠剑宁,王学银.甘肃省肃北蒙古族自治县小冰沟铅锌报告[R].甘肃省地质矿产勘查开发局第四地质矿产勘查院,2010. [8] Wittlinger G,Tapponnier P,Poupinet G,et al.Tomographic evidence for localized lithospheric shear along the Altyn Tagh fault[J].1998,282(5386):74-76. [9] Yin A,Rumelhart P E,Butler R,et al.Tectonic history of the Altyn Tagh fault system in northern Tibet inferred from Cenozoic sedimentation[J].2002,114(10):1257-1295. [10] Wittlinger G,Tapponnier P,Poupinet G,et al.Tomographic evidence for localized lithospheric shear along the Altyn Tagh fault[J].1998,282(5386):74-76. [11] 任收麦,葛肖虹,刘永江.阿尔金断裂带研究进展[J].地球科学进展.2003(03):386-391. [12] 许志琴,杨经绥,张建新,等.阿尔金断裂两侧构造单元的对比及岩石圈剪切机制[J].地质学报.1999(03):193-205. [13] Cowgill E, Yin A, Harrison T M,et al.Reconstruction of the Altyn Tagh fault based on U--Pb geochronology: Role of back thrusts, mantle sutures, and heterogeneous crustal strength in forming the Tibetan Plateau[J].2003,108(B7):2346. [14] 李海兵,杨经绥,许志琴,等.阿尔金断裂带对青藏高原北部生长、隆升的制约[J].地学前缘.2006(04):59-79. [15] Peltzer G, Tapponnier P.Formation and evolution of strike-slip faults, rifts, and basins during the India‐Asia collision: An experimental approach[J].1988,93(B12):15085-15117. [16] Sobel E R, Arnaud N.A possible middle Paleozoic suture in the Altyn Tagh,NW China[J].1999,18(1):64-74. [17] 郑孟林,曹春潮,李明杰,等.阿尔金断裂带东南缘含油气盆地群的形成演化[J].地质论评.2003(03):277-285. [18] 车自成,刘良,刘洪福,等.阿尔金断裂系的组成及相关中新生代含油气盆地的成因特征[J].中国区域地质.1998(04):42-49. [19] 甘肃省地质矿产局.甘肃省区域地质志.北京:地质出版社,1989. [20] 李建锋,张志诚,韩宝福.中祁连西段肃北、石包城地区早古生代花岗岩年代学、地球化学特征及其地质意义[J].岩石学报,2010,26(8):2431-2444. [21] 贾群子,杨忠堂,肖朝阳,等.祁连山铜金钨铅锌矿床成矿规律和成矿预测.北京:地质出版社,2007. [22] 毛景文,张招崇,左国朝.北祁连山西段铜金铁钨多金属矿床成矿系列和找矿评价.北京:地质出版社,2003. [23] 许文进,李长龙,马振武.土达坂铅锌矿地质特征及其找矿标志[J].资源与产业.2009(04):96-98. [24] 王方成,刘伯崇,蔡晓菊.甘肃掉石沟铅锌矿矿床特征及找矿思路[J]地质与勘探.2010(05): 836-843. [25] 甘肃省地质局第二区域地质测量队.1:20万别盖幅区域地质矿产调查报告[R].甘肃省地质矿产局,1973. [26] 冯治汉,徐家乐.甘肃省景观地球化学特征及区域化探工作方法研究[J].地质与勘探.2003(06):2-5. [27] 侯云生,金治鹏,刘建宏,等.甘肃省区域地球化学填图与地球化学景观特征[C]//中国地质学会.第六届世界华人地质科学研讨会和中国地质学会2005年学术年会论文摘要集.北京:中国地质学会,2005:7. [28] 彭梧山.地球化学探矿[M].北京:地质出版社,1986. [29] 赵君,乔树岩,戴慧敏.水系沉积物测量在阿巴通德拉扎卡地区找矿应用[J].物探与化探. 2011(01):24-27. [30] Turekian K K,Wedepohl K H.Distribution of the elements in some major units of the earth's crust[J].1961,72(2):175-192. [31] Pison G,Rousseeuw P J,Filzmoser P,et al.Robust factor analysis[J].2003,84(1):145-172. [32] Rose A W, Hawkes H E, Webb J S.Geochemistry in mineral exploration[M].London: academic press London,1979. [33] 董庆吉,陈建平,唐宇.R型因子分析在矿床成矿预测中的应用——以山东黄埠岭金矿为例[J].地质与勘探,2008,(04):64-68. [34] Shrestha S, Kazama F.Assessment of surface water quality using multivariate statistical techniques: A case study of the Fuji river basin,Japan[J].2007,22(4):464-475. [35] Kaiser H F.An index of factorial simplicity[J].1974,39(1):31-36. [36] Gazzaz N M,Yusoff M K,Ramli M F,et al.Characterization of spatial patterns in river water quality using chemometric pattern recognition techniques[J].2012,64(4):688-698. [37] 杜强,贾丽艳.SPSS统计分析从入门到精通[M].北京:人民邮电出版社,2011. [38] 孟祥金,侯增谦,董光裕,等.江西冷水坑斑岩型铅锌银矿床地质特征、热液蚀变与成矿时限[J].地质学报,2009,(12):1951-1967. [39] 中国选矿技术网.铋的特征及找矿标志[EB/OL].http://www.mining120.com/html/1011/20101116_22019.asp. [40] 张辉善,张杰,史俊波,等.青海格尔木红石山地区水系沉积物测量异常特征及优选找矿靶区[J] .物探与化探,2011,(06):768-772. [41] 任天祥,伍宗华,姜荣生.区域化探异常筛选与查证的方法技术[M].北京:地质出版社,1998. [42] Balasundaram M S.General Report of the Geological Survey of India for the Year 1969-1970[R].Order of the Government of India by the Manager of Publications,1972. [43] 夏祥标,郑来林.普迟亚地区水系沉积物测量地球化学特征及找矿方向[J].物探与化探,2009,35(6):626-629,634. [44] 金旭东,张德会,万天丰.隐伏岩体顶上带与深部成矿预测[J].地质通报,2010,29(2/3):392-400.
