1. 新疆大学地质与矿业学院
2. 新疆维吾尔自治区有色地质勘查局703队
3. 新疆西部黄金股份有限公司
纸质出版:2014
移动端阅览
[1]郑子军,马海杰,汪立今,等.新疆加曼特金矿的显微矿物学及黄铁矿研究[J].新疆大学学报(自然科学版),2014,31(04):487-491.
郑子军, 马海杰, 汪立今, et al. 新疆加曼特金矿的显微矿物学及黄铁矿研究[J]. Journal of Xinjiang University (Natural Science Edition in Chinese and English), 2014, 31(4): 487-491.
新疆加曼特金矿床赋存于下石炭统大哈拉军山组上亚组中酸性火山岩及火山碎屑岩中[1].黄铁矿是金的主要载体矿物之一
因此
通过对黄铁矿的显微特征和成分标型的细致研究
既可以了解金的赋存状态
又能获取金矿床的成因及相关成矿条件的信息.本文通过对加曼特金矿床中黄铁矿的矿物学初探
发现黄铁矿中赋含金
有可能其赋存状态是晶格金.同时发现金矿中黄铁矿的Co/Ni的比值为2.765(Co/Ni>1)
Au/Ag比值为5.889(Au/Ag>0.5)
通过投图、计算
发现加曼特金矿为中—低温热液成因
这与吴艳爽等通过流体包裹体研究所得出的结论一致.
Jia Mante gold deposite in Xinjiang
which Occurrence at the mountain subgroup acidic volcanic rocks and pyroclastic rocks Carboniferous large army Sahara. Pyrite is one of the main carriers of gold minerals
Through carefully study of the pyrite with microscopic characteristics and compositional type
not only can understand the mode of occurrence of gold
but also access to the causes of gold deposits
and information related to mineralization conditions. Based on the gold deposits in pyrite with Mineralogical Study
which is located in Jia Mante
we have found that pyrite may contain gold
and its hosting state maybe lattice Gold. what else
pyrite in Goldmine
we have understanded that the ratio between Co and Ni
the value is 2.765(Co/Ni>1).The ratio between Au and Ag is 5.889(Au/Ag>0.5). By administering figures and calculating
there is a conclusion
the cause of formation in Jia Mante gold deposite in mid-low temperature hydrothermal. So
the conclusions
what we have calculated were in complete agreement with Wu Yanshuang
who has a verdict studied by fluid inclusion.
白建科,李智佩,徐学义,等.新疆西天山吐拉苏-也里莫墩火山岩带年代学:对加曼特金矿成矿时代的约束[J].地球学报,2011,32(3):322-330.
李锦轶,肖序常,汤耀庆,等.新疆北部金属矿产与板块构造[J].新疆地质,1992(2):138-146.
董连慧,田昌烈.西天山吐拉苏-也里莫墩金成矿带简述[J].地质与资源,2001(2):85-90+101.
沙德铭,董连慧,鲍庆中,等.西天山地区金矿床主要成因类型及找矿方向[J].新疆地质,2003(4):419-425.
韩刚.新疆尼勒克县加曼特金矿床地质特征及成因浅析[J].新疆有色金属,2010,33(2):34-37.
卢静文,彭晓蕾.金属矿物显微镜鉴定手册[M].北京:地质出版社,2010.
魏明秀.黄铁矿晶胞参数计算及某些杂质含量分布特征[J].矿物学报,1986(3):245-251.
宫丽,马光.黄铁矿的成分标型特征及其在金属矿床中的指示意义[J].地质找矿论丛,2011,26(2):162-166.
刘英俊,马东升.金的地球化学[M].北京:科学出版社,1991.
吴艳爽,汪立今,马海杰,等.新疆加曼特金矿矿床地质特征及流体包裹体初探[J].矿物学报,2011,31(S1):513.
Bajwah Z,Seccombe P,Offler R.Trace element distribution,Co:Ni ratios and genesis of the Big Cadia iron-copper deposit,New South Wales,Australia[J].Mineralium Deposita,1987,22(4):292-300.
Brill B.Trace-element contents and partitioning of elements in ore minerals from the CSA Cu–Pb–Zn deposit,Australia[J].Can Mineral,1989,27:263-74.
李红兵,曾凡治.金矿中的黄铁矿标型特征[J].地质找矿论丛,2005(3):199-203.
0
浏览量
97
下载量
0
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621
