The study of fine particle total measurement over the Huaniushan Pb-Zn deposit of Gansu Province was conducted. The authors have revealed that major ore-forming elements Pb and Zn show obvious background-anomaly contrast and strong concentration coefficient; in addition, they have positive correlation with Ag, Sb, As, Au, Hg and Cu. There are Pb-Zn-Ag-Au-Sb-As-Cu-Hg geochemical anomalies delineated by this method and the anomalies are located right over the known orebodies, indicating that the geochemical exploration method can be used to effectively locate reliable prospecting targets in Gobi desert terrain.
刘汉粮, 张必敏, 刘东盛, 王学求, 张振海, 韩志轩. 土壤微细粒全量测量在甘肃花牛山矿区的应用[J]. 物探与化探, 2016, 40(1): 33-39.
LIU Han-Liang, ZHANG Bi-Min, LIU Dong-Sheng, WANG Xue-Qiu, ZHANG Zhen-Hai, HAN Zhi-Xuan. The application of soil geochemical measurement method to the Huaniushan Pb-Zn deposit, Gansu Province. Geophysical and Geochemical Exploration, 2016, 40(1): 33-39.
[1] 杨建国,翟金元,杨宏武,等.甘肃北山地区花牛山铅锌矿区玄武岩锆石LA-ICP-MS U-Pb定年及其地质意义[J].地质通报, 2010, 29(7):1017-1023.[2] 杨建国,闫晔轶,王凯,等.花牛山喷流沉积型银铅锌矿床综合找矿方法[J].矿物学报, 2009(增刊):151-153.[3] 甘肃省地矿局地质科学研究所.花牛山有色金属矿床及其外围找矿方向研究报告[R].甘肃省地矿局地质科学研究所,1983-1984.[4] 王学求.深穿透勘查地球化学[J].物探与化探, 1998, 22(3):166-199.[5] Kristiansson K, Malmqvist L. Evidence for nondiffusive transport of Rn in the ground and a new physical model for the transport[J]. Geophysics, 1982, 47(10):1444-1452.[6] Clark J R, Meier A L, Riddle G. Enzyme leaching of surficial geochemical samples for defecting hydromorphic trace-element anomalies associated with precious-metal mineralized bedrock buried beneath glacial overburden in northern Minnesota[J]. Gold, 1990, 90:189-207.[7] Antropova L V, Goldberg I S, Voroshilov N A, et al. New methods of regional exploration for blind mineralization:Application in the USSR[J]. Journal of Geochemical Exploration, 1992, 43:157-166.[8] Mann A W, Birrell R D, Gay L M, et al. Partial extractions and mobile metal ions[C]//Camuti K S Extended Abstracts of the 17th IGES, 1995:31-34.[9] 谢学锦.用新观念与新技术寻找巨型矿床[J].科学中国人, 1995, 15:14-16.[10] 王学求,程志忠.元素活动态测量技术的发展及其意义[J].国外地质勘探技术, 1996(2):17-22.[11] 王学求,刘占元,叶荣,等.新疆金窝子矿区深穿透地球化学对比研究[J].物探与化探, 2003, 27(4):247-254.[12] 刘汉粮,王学求,张必敏,等.沙泉子隐伏铜镍矿地球化学勘查方法试验[J].物探化探计算技术, 2014, 36(6):763-770.[13] 王学求.荒漠隔壁区超低密度地球化学调查与评价-以东天山为例[J].新疆地质, 2001, 19(3):200-206.[14] 聂风军,江思宏,白大明.北山地区金属矿床成矿规律及找矿方向[M].北京:地质出版社, 2002.[15] 朱江,吕新彪,曹晓峰,等.甘肃花牛山铅锌金矿床地质特征及成矿物质来源[J].矿床地质, 2010, 29(增刊):1033-1034.[16] 何智祖,曹俊,董钦伟.甘肃北山花牛山东金矿床地质特征及找矿思路[J].甘肃冶金, 2012, 34(3):74-78.[17] 代文军.甘肃北山花牛山金银铅锌矿床成因探讨[J].华南地质与矿产, 2010,(3):25-33.[18] 殷勇,殷先明.甘肃北山重要金属矿床类型与找矿预测[J].甘肃地质, 2008, 17(2):9-18.[19] 迟清华,鄢明才.应用地球化学元素丰度数据手册[M].北京:地质出版社, 2007.[20] 中国科学院地球化学研究所.高等地球化学[M].北京:科学出版社, 1998.[21] 韩吟文,马振东.地球化学[M].北京:地质出版社, 2003.[22] 刘汉粮,王学求,张必敏,等.岩屑测量和土壤微细粒测量在沙泉子铜镍矿的应用[J].物探与化探, 2015, 39(2):228-233.[23] 张必敏.我国西部特殊景观区化探方法研究进展[J].物探与化探, 2008, 32(5):473-476.[24] 叶荣,王学求,赵伦山,等.戈壁覆盖区金窝子矿带深穿透地球化学方法研究[J].地质与勘探,2004,40(6):65-70.[25] 王学求.深穿透地球化学迁移模型[J].地质通报, 2005, 24(10/11):892-896.[26] 刘汉粮,迟清华,王玮,等.内蒙古中东部残山丘陵草原覆盖区化探方法研究[J].物探与化探, 2013, 37(3):382-388.[27] 张必敏,迟清华,张永勤.干旱荒漠覆盖区隐伏金矿上方覆盖层三维地球化学分布模式[J].地学前缘,2012,19(3):130-137.