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云南铜厂沟斑岩型铜钼矿矿化蚀变过程中成矿元素迁移特征

陈建航 刘学龙 李振焕 张昌振 罗应 王帅帅

陈建航, 刘学龙, 李振焕, 等, 2019. 云南铜厂沟斑岩型铜钼矿矿化蚀变过程中成矿元素迁移特征. 地质力学学报, 25 (S1): 119-123. DOI: 10.12090/j.issn.1006-6616.2019.25.S1.020
引用本文: 陈建航, 刘学龙, 李振焕, 等, 2019. 云南铜厂沟斑岩型铜钼矿矿化蚀变过程中成矿元素迁移特征. 地质力学学报, 25 (S1): 119-123. DOI: 10.12090/j.issn.1006-6616.2019.25.S1.020
CHEN Jianhang, LIU Xuelong, LI Zhenhuan, et al., 2019. MIGRATION CHARACTERISTICS OF ORE-FORMING ELEMENTS DURING MINERALIZATION AND ALTERATION OF TONGCHANGGOU PORPHYRY COPPER-MOLYBDENUM DEPOSIT, YUNNAN PROVINCE. Journal of Geomechanics, 25 (S1): 119-123. DOI: 10.12090/j.issn.1006-6616.2019.25.S1.020
Citation: CHEN Jianhang, LIU Xuelong, LI Zhenhuan, et al., 2019. MIGRATION CHARACTERISTICS OF ORE-FORMING ELEMENTS DURING MINERALIZATION AND ALTERATION OF TONGCHANGGOU PORPHYRY COPPER-MOLYBDENUM DEPOSIT, YUNNAN PROVINCE. Journal of Geomechanics, 25 (S1): 119-123. DOI: 10.12090/j.issn.1006-6616.2019.25.S1.020

云南铜厂沟斑岩型铜钼矿矿化蚀变过程中成矿元素迁移特征

doi: 10.12090/j.issn.1006-6616.2019.25.S1.020
基金项目: 

云南省科学技术奖"杰出贡献奖项目"专题四 2017001

自然资源部地质信息技术重点实验室开放研究课题 2018432

详细信息
    作者简介:

    陈建航(1995-), 男, 在读硕士, 矿床学专业。E-mail:chenjianhang1995@163.com

    通讯作者:

    刘学龙(1983-), 男, 副教授, 矿床学专业, 从事云南三江地区的地质矿产研究及矿床学教学工作。E-mail:xuelongliu@foxmail.com

  • 中图分类号: P618.2

MIGRATION CHARACTERISTICS OF ORE-FORMING ELEMENTS DURING MINERALIZATION AND ALTERATION OF TONGCHANGGOU PORPHYRY COPPER-MOLYBDENUM DEPOSIT, YUNNAN PROVINCE

  • 摘要: 铜厂沟斑岩型铜钼矿是格咱岛弧燕山晚期Mo多金属成矿作用的典型代表,矿床中与Cu-Mo矿化相关的蚀变作用广泛发育。文章在对该矿床岩相学研究的基础上,选择TiO2作为蚀变过程中惰性组分、运用Gresens方程对元素迁移进行定量分析。主量元素迁移特征显示在钾硅酸盐化蚀变阶段和石英—绢云母化蚀变阶段中Al2O3、K2O、Na2O、P2O5、SiO2持续迁入,青磐岩化阶段Fe2O3、MgO、CaO迁入富集;微量元素在钾硅酸盐化阶段显示为Mo、Ba、W、Ra、Nb、Ta、LREE元素明显迁入,且Ba、W与Mo的富集有明显的相关性,石英—绢云母化蚀变阶段Pb、Zn富集成矿,青磐岩化阶段Cu富集成矿,铜厂沟斑岩型铜钼矿矿化蚀变与成矿元素迁移特征研究对该区深部地球化学勘查指标制定、成矿信息及矿体边界确定等具有重要的参考意义。

     

  • 图  1  格咱岛弧区域地质图(据文献[7]修改)

    1—第四纪全新世堆积层; 2—上三叠统图姆沟组; 3—上三叠统松桂组; 4—上三叠统中窝组; 5—三叠系泥汝组; 6—中三叠统北衙组; 7—下三叠统青天堡组; 8—二叠系冈达概组; 9—二叠系峨眉山组; 10—上二叠统黑泥哨组; 11—下二叠统冰峰组; 12—黑云花岗岩; 13—超基性岩脉; 14—辉长辉绿岩脉; 15—铜钼矿点; 16—金矿点; 17—铅锌矿点; 18—地质界线; 19—断裂; 20—分区断裂; 21—研究区

    Figure  1.  Geological map of the Geza arc (after reference[7])

    图  2  铜厂沟铜钼矿蚀变矿化过程主量元素迁移图

    Figure  2.  Migration diagram of major elements during alteration and mineralization of Cu-Mo ore

    图  3  铜厂沟铜钼矿蚀变矿化过程微量元素迁移图

    Figure  3.  Migration diagram of trace elements during alteration and mineralization of Cu-Mo ore

    图  4  铜厂沟稀土元素球粒陨石标准化图解

    Figure  4.  Standardization diagram of rare earth elements chondrite in Tongchanggou

  • [1] 李文昌, 余海军, 尹光侯, 等.滇西北铜厂沟钼多金属矿床辉钼矿Re-Os同位素年龄及其成矿环境[J].矿床地质, 2012, 31(2):282-292. doi: 10.3969/j.issn.0258-7106.2012.02.009

    LI Wenchang, YU Haijun, YIN Guanghou, et al. Re-Os dating of molybdenite from Tongchanggou Mo-polymetallic deposit in northwest Yunnan and its metallogenic environment[J]. Mineral Deposits, 2012, 31(2):282-292. (in Chinese with English abstract) doi: 10.3969/j.issn.0258-7106.2012.02.009
    [2] 刘学龙, 李文昌, 朱俊, 等.滇西北铜厂沟斑岩型Mo-Cu矿床蚀变分带、脉体系统研究进展[C]//第八届全国成矿理论与找矿方法学术讨论会论文摘要文集.北京: 《矿物学报》编辑部, 2017: 2. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-KWXB201712001198.htm

    LIU Xuelong, LI Wenchang, ZHU Jun, et al. Research progress on the alteration zone and vein body system of Mo-Cu deposit in Tongchang gully in northwest Yunnan[C]. Acta Mineralogica Sinica (in Chinese) http://cpfd.cnki.com.cn/Article/CPFDTOTAL-KWXB201712001198.htm
    [3] 高雪, 孟健寅.滇西北铜厂沟Mo-Cu矿床成矿流体和成矿物质来源:矽卡岩矿物学与稳定同位素证据[J].岩石学报, 2017, 33(7):2161-2174. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201707013

    GAO Xue, MENG Jianyin. The source of ore-forming fluids and materials in the Tongchanggou Mo-Cu deposit, northwestern Yunnan, China:Constrains from skarn mineralogy and stable isotopes[J]. Acta Petrologica Sinica, 2017, 33(7):2161-2174. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/ysxb98201707013
    [4] 余海军, 李文昌, 尹光候, 等.滇西北铜厂沟Mo-Cu矿床岩体年代学、地球化学及其地质意义[J].岩石学报, 2015, 31(11):3217-3233. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201511005

    YU Haijun, LI Wenchang, YIN Guanghou, et al. 2015. Geochronology, geochemistry and geological significance of the intrusion from the Tongchanggou Mo-Cu deposit, northwestern Yunnan[J]. Acta Petrologica Sinica, 2015, 31(11):3217-3233. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/ysxb98201511005
    [5] 刘林, 芮会超.成矿预测的发展现状及趋势[J].地质力学学报, 2016, 22(2):223-231. doi: 10.3969/j.issn.1006-6616.2016.02.004

    LIU Lin, RUI Huichao. Present situation and development tendency of metallogenic prediction[J]. Journal of Geomechanics, 2016, 22(2):223-231. (in Chinese with English abstract) doi: 10.3969/j.issn.1006-6616.2016.02.004
    [6] 张欢欢, 白和, 王和平, 等.构造-蚀变-地球化学综合找矿预测方法研究——以陕西小秦岭金矿田Q173号矿脉为例[J].地质力学学报, 2016, 22(2):269-284. doi: 10.3969/j.issn.1006-6616.2016.02.008

    ZHANG Huanhuan, BAI He, WANG Heping, et al. Study on the Q173 vein in Xiaoqinling gold field with the method of structure-alteration-geochemistry prospecting prediction[J]. Journal of Geomechanics, 2016, 22(2):269-284. (in Chinese with English abstract) doi: 10.3969/j.issn.1006-6616.2016.02.008
    [7] YU H J, LI W C, YIN G H, et al, 2014. Zircon U-Pb ages of the granodioritic porphyry in the Laba molybdenum deposit, Yunnan, SW China and its geological implication[J], Acta Geologica Sinica, 88(4):1183-1194. doi: 10.1111/1755-6724.12282
    [8] GRESENS R L. Composition-volume relationships of metasomatism[J]. Chemical Geology, 1976, 2:47-65. http://cn.bing.com/academic/profile?id=c425712c139db9e7b3d60f97b947746d&encoded=0&v=paper_preview&mkt=zh-cn
    [9] GRANT J A. The isocon diagram; a simple solution to Gresens' equation for metasomatic alteration[J]. Economic Geology, 1986, 81(8):1976-1982. doi: 10.2113/gsecongeo.81.8.1976
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  • 刊出日期:  2019-05-01

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