世界地质    2017 36 (1): 105-117   ISSN: 1004-5589  CN: 22-1111/P  

内蒙古维拉斯托铅锌矿床流体包裹体特征及矿床成因研究
权鸿雁1, 蔡文艳1, 张雪冰1, 付丽娟2, 王可勇1
1. 吉林大学 地球科学学院, 长春 130061;
2. 内蒙古山金地质矿产勘查有限公司, 内蒙古 赤峰 024000
收稿日期 2016-06-24  修回日期 2017-01-03  网络版发布日期 null
参考文献  

[1] 郭利军.内蒙古自治区克什克腾旗维拉斯托矿区银铅锌多金属矿详查报告[R].赤峰:内蒙古地质勘查有限责任公司,2007. GUO Li-jun. Detailed survey report of Weilasituo Ag-Pb-Zn polymetallic deposit, Keshiketeng Region, Inner Mongolia[R].Chifeng:Inner Mongolia Geological Exploration co., Ltd, 2007.
[2] 郑翻身, 蔡红军, 张振法. 内蒙古拜仁达坝维拉斯托超大型银铅锌矿的发现及找矿意义[J]. 物探与化探, 2006, 30(1):13-20. ZHENG Fan-shen, CAI Hong-jun, ZHANG Zhen-fa. The discovery of superlarge silver-lead-zinc deposits in Bairendaba and Weilasituo, Inner Mongolia, and its ore-prospecting significance[J]. Geophysical and Geochemical Exploration,2006, 30(1):13-20.
[3] 江思宏, 聂凤军, 刘翼飞,等. 内蒙古拜仁达坝及维拉斯托银多金属矿床的硫和铅同位素研究[J]. 矿床地质, 2010, 29(1):101-112. JIANG Si-hong, NIE Feng-jun, LIU Yi-fei, et al. Sulfur and lead isotopic compositions of Bairendaba and Weilasituo silver-polymetallic deposits, Inner Mongolia[J]. Mineral Deposits, 2010,29(1):101-112.
[4] 梅微, 吕新彪, 唐然坤,等. 大兴安岭南段西坡拜仁达坝-维拉斯托矿床成矿流体特征及其演化[J]. 地球科学,2015(1):145-162. MEI Wei, LÜ Xin-biao, TANG Ran-kun, et al. Ore-forming fluid and its evolution of Bairendaba-Weilasituo deposits in west slope of Southern Great Xing'an Range[J]. Earth Science, 2015(1):145-162.
[5] 王瑾, 侯青叶, 陈岳龙,等. 内蒙古维拉斯托铜多金属矿床流体包裹体研究[J]. 现代地质, 2010,24(5):847-855. WANG Jin, HOU Qing-ye, CHEN Yue-long, et al. Fluid inclusion study of the Weilasituo Cu polymetal deposit in Inner Mongolia[J]. Geoscience, 2010,24(5):847-855.
[6] 刘翼飞, 樊志勇, 蒋胡灿,等. 内蒙古维拉斯托-拜仁达坝斑岩-热液脉状成矿体系研究[J]. 地质学报, 2014, 88(12):2373-2385. LIU Yi-fei, FAN Zhi-yong, JIANG Hu-can, et al. Genesis of the Weilasituo-Bairendaba porphyry-hydrothermal vein type system in Inner Mongolia, China[J]. Acta Geologica Sinica,2014, 88(12):2373-2385.
[7] Ouyang H G, Mao J W, Santosh M. Anatomy of a large Ag-Pb-Zn deposit in the Great Xing'an Range, northeast China:metallogeny associated with Early Cretaceous magmatism[J]. International Geology Review, 2013, 55(4):411-429.
[8] 欧阳荷根. 大兴安岭南段拜仁达坝-维拉斯托银多金属矿床成矿作用及动力学背景:博士学位论文[D]. 北京:中国地质大学,2013. OUYANG He-gen. Metallogenesis of Barendaba-Weilasituo silver-polymetallic deposit and its geodynamic setting, in the southern segment of Great Xing'an Range, NE China:doctor's degree thesis[D]. Beijing:China University of Geosciences, 2013.
[9] 潘小菲, 郭利军, 王硕,等. 内蒙古维拉斯托铜锌矿床的白云母Ar-Ar年龄探讨[J]. 岩石矿物学杂志, 2009, 28(5):473-479. PAN Xiao-fei, GUO Li-jun, WANG Shuo, et al. Laser microprobe Ar-Ar dating of biotite from the Weilasituo Cu-Zn polymetallic deposit in Inner Mongollia[J]. Acta Petrologica et Mineralogica, 2009, 28(5):473-479.
[10] 邵济安, 牟保磊, 朱慧忠,等. 大兴安岭中南段中生代成矿物质的深部来源与背景[J]. 岩石学报, 2010, 26(3):649-656. SHAO Ji-an, MOU Bao-lei, ZHU Hui-zhong, et al. Material source and tectonic settings of the Mesozoic mineralization of the DaHinggan Mts[J]. Acta Petrologica Sinica, 2010, 26(3):649-656.
[11] 赵一鸣,张德全. 大兴安岭及其邻区铜多金属矿床成矿规律与远景评价[M].北京:地震出版社,1997:131-135. ZHAO Yi-ming, ZHANG De-quan. Metallogeny and prospective evaluation of copper-polymetallic deposits in the Da Hinggan mountains and its adjacent regions[M]. Beijing:Seismological Press, 1997:131-135.
[12] 盛继福, 付先政, 李鹤年. 大兴安岭中段成矿环境与铜多金属矿床地质特征[M]. 北京:地震出版社,1999:90-125. SHENG Ji-fu, FU Xian-zheng, LI He-nian. Metallogenic environment and copper polymetallic ore deposit geological characteristics of middle Greater Hinggan mountains[M]. Beijing:Seismological Press, 1999:90-125.
[13] 李蒙文.天山-兴蒙造山带中段内生金属矿床成矿系列及成矿预测:博士学位论文[D]. 北京:中国地质科院,2006. LI Meng-wen. Research on metallogenic series and metallogenic prognosis of endogenetic metallic deposits in the middle section of Tianshan-Xingmeng Orogen:doctor's degree thesis[D]. Beijing:Chinese Academy of Geological Sciences, 2006.
[14] Clayton R N, O'Neil J R, Mayeda T K.Oxygen isotope exchange between quartz and water[J]. Journal of geophysical research,1972,77(17):3057-3067.
[15] Roedder E. Fluid inclusions[J]. Mineralogical Society of America, 1984, 12:644.
[16] 卢焕章,范宏瑞,倪培,等.流体包裹体[M].北京:科学出版社, 2004:1-450. LU Huan-zhang, FAN Hong-rui, NI Pei, et al. Fluid inclusions[M]. Beijing:Science Press, 2004:1-450.
[17] 范宏瑞, Groves D I, Mikucki E J, 等. 西澳大利亚纳沃日金矿流体混合与金的成矿作用[J]. 矿床地质, 2001, 20(1):37-43. FAN Hong-rui, Groves D I, Mikucki E J, et al. Fluid mixing in the generation of Nevoria Gold mineralisation in the Southern Cross Greenstone Belt, Western Australia[J]. Mineral Deposits, 2001, 20(1):37-43.
[18] Thiery R, Vidal J, Dubessy J. Phase equilibria modelling applied to fluid inclusions:liquid-vapor equilibria and calculation of the molar volume in the CO2 CH4 N2, system[J]. Geochimica Et Cosmochimica Acta, 1994, 58(3):1073-1082.
[19] 王秋玲, 孙洪涛, 丁俊英, 等. 塔里木北缘库鲁克塔格地块大金沟金矿流体包裹体特征:对矿床成因的启示[J]. 世界地质,2016,35(3):771-777. WANG Qiu-ling, SUN Hong-tao, DING Jun-ying, et al. Fluid inclusions for Dajingou gold deposit of Quruqtagh block in northeastern Tarim:implication for ore genesis[J]. Global Geology, 2016, 35(3):771-777.
[20] 魏占浩, 杜生鹏, 王键, 等. 青海青龙沟金矿成矿流体演化特征及矿床成因研究[J]. 世界地质,2015,34(4):951-960. WEI Zhan-hao, DU Sheng-peng, WANG Jian, et al. Evolution characteristics of fluid and genesis of Qinglonggou gold deposit in Qinghai[J]. Global Geology, 2015,34(4):951-960.
[21] 郑永飞. 稳定同位素地球化学[M]. 北京:科学出版社, 2000:1-315. ZHENG Yong-fei. Stable isotope geochemistry[M]. Beijing:Science Press, 2000:1-315.
[22] 张理刚. 稳定同位素在地质科学中的应用[M]. 西安:陕西科学技术出版社,1985:91-94. ZHANG Li-gang. The application of stable isotope to geology[M]. Xi'an:Shanxi Science and Technology Press, 1985:91-94.
[23] 陈永清, 黄静宁, 卢映祥, 等. 中缅毗邻区金腊Pb-Zn-Ag多金属矿田元素, 稳定同位素和流体包裹体地球化学[J]. 地球科学, 2009,34(4):585-594. CHEN Yong-qing, HUANG Jing-ning, LU Ying-xiang, et al. Geochemistry of elements, sulphur-lead isotopes and fluid inclusions from Jinla Pb-Zn-Ag poly-metallic ore field at joint area across China and Myanmar Border[J]. Earth Science, 2009,34(4):585-594.
[24] 陕亮, 郑有业, 许荣科,等. 硫同位素示踪与热液成矿作用研究[J]. 地质与资源, 2009, 18(3):197-203. SHAN Liang, ZHENG You-ye, XU Rong-ke, et al. Review on sulfur isotopic tracing and hydrothermal metallogenesis[J]. Geology and Resources, 2009, 18(3):197-203.
[25] Taylor H P, Jr H P. The application of oxygen and hydrogen isotope studies to problems of hydrothermal alteration and ore deposits[J]. Economic Geology, 1974, 69(6):843-883.
[26] 王春光, 孙丰月, 孙国胜, 等. 内蒙古翁牛特旗荷尔勿苏铅锌矿床成矿流体性质与成因[J]. 世界地质,2016,35(2):450-457,469. WANG Chun-guang, SUN Feng-yue, SUN Guo-sheng, et al. Characteristics and genesis of ore-forming fluid in Heerwusu Pb-Zn deposit of Wengniute banner, Inner Mongolia[J]. Global Geology,2016,35(2):450-457,469.


通讯作者: 王可勇(1965-),男,教授,博士生导师,主要从事矿产勘查与普查和矿床学方面研究.E-mail:wangky@jlu.edu.cn