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邛莫金矿床中块硫锑铜矿含硒性及其特征
引用本文:刘家军,刘建明,卢文全,刘显凡,凌洪飞.邛莫金矿床中块硫锑铜矿含硒性及其特征[J].高校地质学报,2000,6(2):210-214.
作者姓名:刘家军  刘建明  卢文全  刘显凡  凌洪飞
作者单位:1. 中国科学院 地球化学研究所 矿床地球化学开放研究实验室,贵州 贵阳 550002;2. 南京大学 内生金属矿床成矿机制研究国家重点实验室,江苏 南京 210093;3. 中国科学院 矿物资源探查研究中心,北京 100101;4. 地质矿产部 矿产综合利用研究所,四川 成都 610041
基金项目:中国科学院资助项目,中国科学院"百人计划",国家重点实验室基金,49773197,,,,,
摘    要:硒的块硫锑铜矿产于西秦岭邛莫金矿床中,与其伴生的矿物有硒汞矿、硒铅矿、硒锑矿、斜方硒镍矿、硒铜镍矿、硒质辉锑矿、自然金以及石英、重晶石等。 含硒的块硫锑铜矿平均显微硬度VHN50=247.5kg/mm2,相当于摩氏硬度4.2。电子探 针分析结果(w,%)为:Sb 25.79,Cu 38.20,S 21.12,Se 1 2.76,Hg 0.0 0~1.49(平均0.58),Ag 0.00~0.33(平均0.09),As 0.00~2.01(平均0.76)。根据成分中S e/(S+Se)比值(原子比)<0.2抑≥0.2,可将所测矿物划分为含硒质块硫锑铜矿与硒质块硫锑 铜矿。它们的化学分子式分别为: (Cu2.84Hg0.01)2.85(Sb1.00A s0.07)1.07(S3.54Se0.46) 4.00和(Cu3.05Hg0.03)3.08(Sb1.07As0.03) 1.10(S2.77Se1.23)4.00。代表性的反射率(%): (470nm) Rγ'=22.84~22.50, Rα'= 27.92~27.99; (550 nm) Rγ'= 22.63~22.76, Rα'=2 7. 79~28.11; (590nm) Rγ'=22.92~22.08, R α'=28.27~28. 72; (650nm) Rγ'=23.08~23.76, Rα'=28.79~29.13。

关 键 词:块硫锑铜矿  含硒性  金矿床  西秦岭
收稿时间:2000-06-20
修稿时间:1999-10-10

Selenium Concentration and Characteristics of Famatinite from Qiongmo Gold Deposit, Western Qinling Mountains
LIU Jia-jun,LIU Jian-ming,LU Wen-quan,LIU Xian-fan,LING Hong-fei.Selenium Concentration and Characteristics of Famatinite from Qiongmo Gold Deposit, Western Qinling Mountains[J].Geological Journal of China Universities,2000,6(2):210-214.
Authors:LIU Jia-jun  LIU Jian-ming  LU Wen-quan  LIU Xian-fan  LING Hong-fei
Institution:1. Open Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002; 2. Key State Laboratory for Mineral Deposits Research, Nanjing University, Nanjing 210093; 3. The Research Center of Mineral Resources Exploration CAS, Beijing, 10010l4;4.Institute of Complex Utilization of Mineral Resources, Ministry of Geology and Mineral Resources, Chengdu, 610041
Abstract:The Qiongmo gold deposit occurs in the Cambrian silicalite and slate in the sou th subzone of western Qinling Mountains. The Se-bearing and selenium famatinite are found in quartz-barite veins in the form of dissemination or veinlets. The associated minerals include tiemannite, clasthalite, antimonselite, kullerudi te, penroseite, selenium stibnite, native gold, barite and quartz. The mineral is lead-gray in colour, brashy, with metallic luster, and 0.01~0.1mm in size. The average microhardness is 247.5kg/mm2 (for 50g load) corresponing to Moh s' hardness=4.2. The reflectance values (SiC standard) are given in 10nm steps. The representative R values are: (470nm), Rγ'=22.84~22.50, Rα'= 27.92~27 .99; (550nm), Rγ'= 22.63~22.76, Rα'=27.79~28.11; (590nm), Rγ'=22. 92~ 22.08, Rα'=28.27~28.72; (650nm), Rγ'=23.08~23.76, Rα'=28.79~29.13. E lectron microprobe analyses of eleven points on famatinite gave the results as f ollows (wt%): Sb, 24.42~28.12 (25.79 in average ); Cu, 36.60~39.94 (38.2 0 in average);S, 14.49~25.74 (21.12 in average);Se, 6.11~23.89 (12.76 in average ). Based on Se/(S+Se) ratios of microprobe analyses the mineral is classified as Se-bearing famatinite and selenium famatinite, corresponding to the formula (C u2.84Hg0.01)2.85(Sb1.00As0.07)1.07(S3.54 Se0.46)4.00 and (Cu3.05Hg0.03)3.08(Sb1.07A s0.03)1.10(S2.77Se1.23)4.00 respectively.
Keywords:famatinite  selenium concentration  gold deposit  Qiongmo  western Qinling Mountains
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