A systematical investigation of primary and secondary geochemical anomaliesaround the gold deposits in Shaoxing-Longquan uplifted zone, Zhejiang Provinceindicates that Au, Ag, Cu, Co, Hg, Pb, Zn, As, Te, Sb are main indicator elementsin the primary anomalies while Au, Ag, As, Hg, Te are indicator elements insecondary anomalies. It has been discovered that the distribution regularity,assemblage as well as vertical and horizontal zonation of these elements are con-trolled by their geochemical properties and by anomaly-forming conditions. Sixcomposite indicators are considered to be of practical significance in prospectingfor gold deposits in this area.
刘英俊, 孙承辕, 沙鹏. 浙江绍兴——龙泉隆起带中金矿床的原生及次生地球化学异常研究[J]. 物探与化探, 1986, 10(3): 171-182.
Liu Yingjun, Sun Chengyuan, Sha Peng . A STUDY OF PRIMARY AND SECONDARY GEOCHEMICALANOMALIES AROUND GOLD DEPOSITS IN SHAOXING-LONGQUAN UPLIFTED ZONE, ZHEJIANG PROVINCE. Geophysical and Geochemical Exploration, 1986, 10(3): 171-182.
［1］ 刘英俊,孙承辕,沙鹏:1984,浙江某地金银矿床的原生地球化学异常特征,第二届勘查地球化学学术讨论文选编,中国地质学会勘查地球化学专业委员会印,P 13-220。
［2］ Boyle R. W.: 1979, The Geochemistry of Gold and its Deposits, Canada Geological Survey Bulletin。
［3］ 沙鹏,顾鹰:1983,对《氟异常定量计算的初步研究》一文的商榷,地质与勘探,第10期,P55-57。
［4］ G. J. S. Govett et.:1976, Experimental Aqueous Dispersion of Element around Sulfides, Econ. Geol., 71,P 925-940。
［5］ 戴安邦:1978,酸碱的软硬度的势标度及其相亲强度和络合物的稳定度,化学通报,第1期,P 26-31。
［6］ 王学仁:1981,地质数据的多元统计分析,科学出版社。
［7］ Barnes H. L.:1979, Solubility of Ore Minerals, Geochemistry of Hydrothermal Ore Deposits, 2nd., by H. L. Barnes, ed., John Wiley & Son.,New York。
