• 中国出版政府奖提名奖

    中国百强科技报刊

    湖北出版政府奖

    中国高校百佳科技期刊

    中国最美期刊

    Volume 36 Issue 2
    Mar.  2011
    Turn off MathJax
    Article Contents
    ZHANG Shou-ting, ZHAO Peng-da, 2011. Porphyry Ore Deposits: Important Study Subjects of Nontraditional Mineral Resources. Earth Science, 36(2): 247-254. doi: 10.3799/dqkx.2011.025
    Citation: ZHANG Shou-ting, ZHAO Peng-da, 2011. Porphyry Ore Deposits: Important Study Subjects of Nontraditional Mineral Resources. Earth Science, 36(2): 247-254. doi: 10.3799/dqkx.2011.025

    Porphyry Ore Deposits: Important Study Subjects of Nontraditional Mineral Resources

    doi: 10.3799/dqkx.2011.025
    • Received Date: 2010-10-25
    • Publish Date: 2011-03-01
    • For many years, porphyry ore deposits have been regarded as the primary sources of the Cu and Mo in a traditional way. However, the geologic conditions of the diagenesis and metallogenesis of the porphyry ore deposits are complex with various mineralization types. Some of the large-superlarge deposits are multielemental and comprehensive. In addition to the Cu, Mo porphyry ore deposits, the metallogenesis and prospecting on nontraditional resources have great potential, including Au, Ag, Sn, W, Bi, Pb, Zn, Re, U, Co, S, Se, Te, PGE, magnetite, etc; rutile and rare metals, such as Ta, Nb are also worth paying attention to. It is of important theoretical value and practical significance to study the diagenesis and metallogenesis of geological background, geological characteristics, mineralization of distribution and the enrichment of a nontraditional view on the porphyry ore deposits; it is meaningful to summarize the indicator of prognosis and assessment on the nontraditional mineral resources, and to guide the prospecting and resource potential assessment on the porphyry ore deposits.

       

    • loading
    • Armstrong, F.C., 1974. Uranium resources of the future-porphyry uranium depsits, formation of uranium ore deposits. International Atomic Energy Agecy, Vienna, 625-634.
      Babcock, R.C., Ballantyne, G.H., Phillips, C.H., 1995. Summary of the geology of the Bingham district, Utah. In: Pierce, F.W., Bolm, J.G., eds., Porphyry copper deposits of the American Cordillera. Arizona Geological Society Digest, 20: 316-335.
      Clark, G.H., 1990. Panguna copper-gold deposit. In: Hughes, F.E., ed., Geology of the mineral deposits of Australia and Papua New Guinea. Australian Institute of Mining and Metallurgy, Australian, 1807-1816.
      Desborough, G.A., Mihalik, P., 1980. Accessory minerals in the igneous host of molybdenum ore, Henderson Mine, Colorado. US Geological Survey, Open-File Report, 80-661.
      Desbomugh, G.A., Sharp, W.N., 1978. Tantalum, uranium, and scandium in heavy accessory oxides, Climax molybdenum mine, Climax, Colorado. Economic Geology, 73(8): 1749-1751. doi: 10.2113/gsecongeo.73.8.1749
      Du, Q., Zhao, Y.M., Lu, B.G., et al., 1988. Porphyry Cu (Mo) deposits in Duobaoshan. Geological Publishing House, Beijing, 225-247 (in Chinese).
      Halter, W., E., Pettke, T., Heinrich, C.A., 2002. The origin of Cu/Au ratios in porphyry-type ore deposits. Science, 296(5574): 1844-1846. doi: 10.1126/science.1070139
      Hou, Z.Q., 2004. Porphyry Cu-Mo-Au deposits: some new insights and advances. Earth Science Frontiers, 11(1): 131-144 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200401014.htm
      Hou, Z.Q., Ma, H.W., Za, W.K., et al., 2003. The Himalayan Yulong porphyry copper belt: product of large-scale strike-slip faulting in eastern Tibet. Economic Geology, 98: 125-145. http://www.researchgate.net/publication/247864181_The_Himalayan_Yulong_Porphyry_Copper_Belt_Product_of_Large-Scale_Strike-Slip_Faulting_in_Eastern_Tibet
      Huang, C.K., Bai, Y., Zhu, Y.S., et al., 2001. Copper deposits in China (Rudin). Geological Publishing House, Beijing (in Chinese).
      Huang, D.H., Wu, C.Y., Du, A.D., et al., 1994. Re-Os isotope ages of molybdenum deposits in East Qinling and their significance. Mineral Deposits, 12(3): 221-230 (in Chinese with English abstract).
      Jr, A.A., Hedenquist, J.W., Itaya, T., et al., 1995. Contemporaneous formation of adjacent porphyry and epithermal Cu-Au deposits over 300 ka in northern Luzon, Philippines. Geology, 23(4): 337-340. doi:10.1130/0091-7613(1995)?023<0337:CFOAPA>?2.3.CO;2
      Li, J.X., Qin, K.Z., Li, G.M., 2006. Basic characteristics of gold-rich porphyry copper deposits and their ore sources and evolving processes of high oxidation magma and ore-forming fluid. Acta Petrologica Sinica, 22(3): 678-688.
      Li, W.C., Pan, G.T., Hou, Z.Q., et al., 2010. Metallogenic theory and prospecting technology in the polyarc-basin series of "Three-River" region in Southwest China. Geological Publishing House, Beijing (in Chinese).
      Macdonald, G.D., Amold, L.C., 1994. Geological and geochemical zoning of the Grasberg igneous complex, Irian Jaya, Indonesia. Journal of Geochemical Exploration, 50(1-3): 143-178. doi: 10.1016/0375-6742(94)90023-X
      Meldrum, S.J., Aquino, R.S., Gonzales, R.I., et al., 1994. The Batu Hijau porphyry copper-gold deposit, Sumbawa Island, Indonesia. Journal of Geochemical Exploration, 50(1-3): 203-220. doi: 10.1016/0375-6742(94)90025-6
      Qu, X.M., Hou, Z.Q., Huang, W., 2001. Is Gangdese porphyry copper belt the second "Yulong" copper belt?Mineral Deposits, 20(4): 355-366 (in Chinese with English abstract). http://www.researchgate.net/publication/284665935_Is_Gangdese_porphyry_copper_belt_the_second_Yulong_copper_belt
      Richard, J.P., Boyce, A.J., Pringle, M.S., 2001. Geologic evolution of the Escondia area, northern Chile: a model for spatial and temporal localization of porphyry Cu mineralization. Economic Geology, 96(2): 271-305. doi: 10.2113/gsecongeo.96.2.271
      Rui, Z.Y., Huang, C.K., Qi, G.M., et al., 1984. Porphyry Cu(Mo) deposits in China. Geological Publishing House, Beijing, 242-272 (in Chinese).
      Rush, P.M., Seegers, H.J., 1990. Ok Tedi copper-gold deposits. In: Hughes, F.E., ed., Geology of the mineral deposits of Australia and Papua New Guinea. Australian Institute of Mining and Metallurgy, Australian, 1747-1754.
      Sillitoe, R.H., 1983. Unconventional metals in porphyry deposits. In: Shanks, W.C., III, ed., Society of mining engineers. Am. Inst. of Mining, Metallurg. & Petrol. Eng., New York, 207-221.
      Titey, S.R., Beane, R.E., 1981. Porphyry copper deposits, PartⅠ: Geologic settings, petrology, and tectogensis. Economic Geology, 75: 214-235. http://ci.nii.ac.jp/naid/20000481718
      Tooker, E.W., 1990. Gold in the Bingham district, Utah. U.S. Geological Survey Bulletin, 1857 E: 1-16.
      Wang, D.H., Chen, Y.C., Xu, Y., et al., 2005. Cenozoic mineralization in China (Rudin). Geological Publishing House, Beijing (in Chinese).
      Xia, B., Chen, G.W., Wang, H., 2003. Analysis of tectonic settings of global superlarge porphyry copper deposits. Science in China (Series D), 46(Suppl. ): 110-122.
      Zhang, Y.Q., Xie, Y.W., Qiu, H.N., et al., 1998. Shoshonitic series: Sr, Nd, and Pb isotopic compositions of ore bearing porphyry for Yulong copper ore belt in the eastern Xizang (Tibet). Chinese Journal of Geology, 33(3): 359-366 (in Chinese with English abstract).
      Zhao, P.D., 2003. An introduction to nontraditional mineral resources. Geological Publishing House, Beijing (in Chinese).
      Zhao, Y.M., Zhang, D.Q., 1997. Metallogeny and evaluation of copper-polymetallic deposits in the Dahinggan Mountains and its adjacent regions. Geological Publishing House, Beijing (in Chinese).
      Zheng, M.H., et al., 1993. Principle of ore geology. Press of Chengdu University of Science and Technology, Chengdu (in Chinese).
      杜琦, 赵玉明, 卢秉刚, 等, 1988. 多宝山斑岩铜矿床. 北京: 地质出版社, 225-247.
      侯增谦, 2004. 斑岩Cu-Mo-Au矿床: 新认识与新进展. 地学前缘, 11(1): 131-144. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200401014.htm
      黄崇轲, 白冶, 朱裕生, 等, 2001. 中国铜矿床(上册). 北京: 地质出版社.
      黄典豪, 吴澄宇, 杜安道, 等, 1994. 东秦岭地区钼矿床的铼-锇同位素年龄及其意义. 矿床地质, 13(3): 221-230. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ403.003.htm
      李文昌, 潘桂棠, 侯增谦, 等, 2010. 西南"三江"多岛弧盆-碰撞造山成矿理论与勘查技术. 北京: 地质出版社.
      曲晓明, 侯增谦, 黄卫, 2001. 冈底斯斑岩铜矿(化)带: 西藏第二条"玉龙"铜矿带. 矿床地质, 20(4): 355-366. doi: 10.3969/j.issn.0258-7106.2001.04.009
      芮宗瑶, 黄崇轲, 齐国明, 等, 1984. 中国斑岩铜(钼)矿床. 北京: 地质出版社, 242-272.
      王登红, 陈毓川, 徐钰, 等, 2005. 中国新生代成矿作用(上). 北京: 地质出版社.
      夏斌, 陈根文, 王核, 2002. 全球超大型斑岩铜矿床形成的构造背景分析. 中国科学(D辑), 32(增刊): 87-95. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK2002S1009.htm
      张玉泉, 谢应雯, 邱华宁, 等, 1998. 钾玄岩系列: 藏东玉龙铜矿带含矿斑岩Sr、Nd、Pb同位素组成. 地质科学, 33(3): 359-366. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX803.010.htm
      赵鹏大, 2003. 非传统矿产资源概论. 北京: 地质出版社.
      赵一鸣, 张德全, 1997. 大兴安岭及其邻区铜多金属矿床成矿规律与远景评价. 北京: 地震出版社.
      郑明华, 等编著, 1993. 矿床地质原理. 成都: 成都科技大学出版社.
    • 加载中

    Catalog

      通讯作者: 陈斌, bchen63@163.com
      • 1. 

        沈阳化工大学材料科学与工程学院 沈阳 110142

      1. 本站搜索
      2. 百度学术搜索
      3. 万方数据库搜索
      4. CNKI搜索

      Figures(1)  / Tables(2)

      Article views (3507) PDF downloads(174) Cited by()
      Proportional views

      /

      DownLoad:  Full-Size Img  PowerPoint
      Return
      Return