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    Volume 34 Issue 6
    Jun.  2009
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    ZHANG Xiao-wen, XIANG Hua, ZHONG Zeng-qiu, ZHOU Han-wen, ZHANG Li, YANG Nian, WANG Jing, 2009. U-Pb Dating and Trace Elements Composition of Hydrothermal Zircons from Jianfengling Granite, Hainan: Restriction on the Age of Hydrothermal Event and Mineralization of Baolun Gold Deposit. Earth Science, 34(6): 921-930.
    Citation: ZHANG Xiao-wen, XIANG Hua, ZHONG Zeng-qiu, ZHOU Han-wen, ZHANG Li, YANG Nian, WANG Jing, 2009. U-Pb Dating and Trace Elements Composition of Hydrothermal Zircons from Jianfengling Granite, Hainan: Restriction on the Age of Hydrothermal Event and Mineralization of Baolun Gold Deposit. Earth Science, 34(6): 921-930.

    U-Pb Dating and Trace Elements Composition of Hydrothermal Zircons from Jianfengling Granite, Hainan: Restriction on the Age of Hydrothermal Event and Mineralization of Baolun Gold Deposit

    • Received Date: 2009-07-06
    • Publish Date: 2009-11-25
    • Detailed studies on zircons from the Jianfengling granite in the Baolun gold deposit indicate that the zircons can be divided into magmatic and hydrothermal zircons. The magmatic zircons are colorless, transparent, prismatic, euhedral crystal with few inclusions, and have moderate U, Th contents (mostly less than 1000μg/g). LA-ICP-MS U-Pb analyses of these zircons gave a weighted mean 206Pb/238U concordia age of 240±2.1Ma, which is interpreted as the age of emplacement for the Jianfengling granite. Hydrothermal zircons are brown, translucence to opaque, and have extremely high U, Th and trace elements contents, the highest U, Th contents being 30000μg/g, 20000μg/g, respectively. Hydrothermal zircons have high common Pb contents (206Pbc=0.77%-11.0%). LA-ICP-MS U-Pb analyses of these zircons gave the age from 106 to 120Ma, with a weighted mean 206Pb/238U age of 112.8±4.3Ma, which is interpreted as the age of hydrothermal event. It is indicated that there is a strong hydrothermal process at ca. 112.8Ma, which might be related to Yanshanian magmatism in this area. Gold mineralization of Baolun gold deposit is most likely related with this hydrothermal event. U-Pb dating on hydrothermal zircons could be used to constrain the timing of hydrothermal event and constrain the timing of gold mineralization related with hydrothermal event.

       

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    • Andersen, T., 2002. Correction of common lead in U-Pb analyses that do not report 204Pb. Chemical Geology, 192 (1-2): 59-79. doi: 10.1016/S0009-2541(02)00195-X
      Cathles, L. M., Erendi, A. H. J., Barrie, T., 1997. How long can a hydrothermal system be sustained by a single intrusive event? Economic Geology, 92 (7-8): 766-771. doi: 10.2113/gsecongeo.92.7-8.766
      Chen, B. L., Ding, S. J., Li, Z. J., et al., 2001. Metallogenic age of Baolun gold deposit, Hainan Province. Geochi mica, 30 (6): 525-532 (in Chinese with English abstract).
      Cherniak, D. J., Watson. E. B., 2001. Pb diffusion in zircon. Chemical Geology, 172 (1-2): 5-24. doi: 10.1016/S0009-2541(00)00233-3
      Claoué-Long, J. C., King, R. W., Kerrich, R., 1990. Archaean hydrothermal zircon in the Abitibi greenstone belt: Constraints on the timing of gold mineralisation. Earth and Planetary Science Letters, 98 (1): 109-128. doi: 10.1016/0012-821X(90)90091-B
      Claoué-Long, J. C., King, R. W., Kerrich. R., 1992. Reply to comment by F. Corfu and D. W. Davis on "Archaean hydrothermal zircon in the Abitibi greenstone belt: Constraints on the timing of gold mineralization". Earth and Planetary Science Letters, 109 (3-4): 601-609. doi: 10.1016/0012-821X(92)90118-F
      Corfu, F., Hanchar, J. M., Hoskin, P. W. O., et al., 2003. Altas of zircon textures. Reviews in Mineralogy and Geochemistry, 53: 469-500. doi: 10.2113/0530469
      Ding, S. J., Huang, D. X., Li, Z. J., et al., 2001. Geological features and minerialzation of the Baolun gold deposit, Hainan. Chinese Geology, 28 (5): 28-34, 18 (in Chinesewith English abstract).
      Dubinska, E., Bylina, P., Kozlowski, A., et al., 2004. U-Pb dating of serpentinization: Hydrothermal zircon from a metasomatic rodingite shell (Sudetic ophiolite, SW Poland). Chemical Geology, 203 (3-4): 183-203. doi: 10.1016/j.chemgeo.2003.10.005
      Geisler, T., Pidgeon, R. T., Kurtz, R., et al., 2003a. Experimental hydrothermal alteration of partially metamict zircon. American Mineralogist, 88 (10): 1496-1513. doi: 10.2138/am-2003-1013
      Geisler, T., Rashwan, A. A., Rahn, M. K. W., et al., 2003b. Low-temperature hydrothermal alteration of natural metamict zircons from the eastern desert, Egypt. Mineralogical Magazine, 67 (3): 485-508. doi: 10.1180/0026461036730112
      Geisler, T., Zhang, M., Salje, E. K. H., 2003c. Recrystallization of almost fully amorphous zircon under hydrothermal conditions: An infrared spectroscopic study. Journal of Nuclear Materials, 320 (3): 280-291. doi: 10.1016/S0022-3115(03)00187-9
      Harrison, T. M., Duncan, I., McDougall, I., 1985. Diffusion of 40Ar in biotite: Temperature, pressure and compositional effects. Geochimica et Cosmochimica Acta, 49 (11): 2461-2468. doi: 10.1016/0016-7037(85)90246-7
      Henry, C. D., Elson, H. B., McIntosh, W. C., et al., 1997. Brief duration of hydrothermal activity at Round Mountain, Nevada, determined from 40Ar/39Ar geochronology. Economic Geology, 92 (7-8): 807-826. doi: 10.2113/gsecongeo.92.7-8.807
      Hodges, K. V., 1991. Pressure-temperature-time paths. Annual Review of Earth and Planetary Sciences, 19: 207-236. doi: 10.1146/annurev.ea.19.050191.001231
      Hoskin, P. W. O., 2005. Trace-element composition of hydrothermal zircon and the alteration of Hadean zircon from the Jack Hills, Australia. Geochimica et Cosmochimica Acta, 69 (3): 637-648. doi: 10.1016/j.gca.2004.07.006
      Hoskin, P. W. O., Ireland, T. R., 2000. Rare earth element chemistry of zircon and its use as a provenance indicator. Geology, 28 (7): 627-630. doi: 10.1130/0091-7613(2000)28<627:REECOZ>2.0.CO;2
      Hoskin, P. W. O., Schaltegger, U., 2003. The composition of zircon and igneous and metamorphic petrogenesis. Reviews in Mineralogy and Geochemistry, 53 (1): 27-62. doi: 10.2113/0530027
      Hu, F. F., Fan, H. R., Yang, J. H., et al., 2004. Mineralizing age of the Rushan lode gold deposit in the Jiaodong Peninsula: SHRIMP U-Pb dating on hydrothermal zircon. Chinese Science Bulletin, 49 (15): 1629-1636. doi: 10.1007/BF03184134
      Kerrich, R., King, R., 1993. Hydrothermal zircon and baddeleyite in Val-d'Or Archean mesothermal gold deposits: Characteristics, compositions, and fluid-inclusion properties, withi mplications for timing of primary gold mineralization. Canadian Journal of Earth Sciences, 30 (12): 2334-2351. doi: 10.1139/e93-203
      Kerrich, R., Kyser, T. K., 1994. 100 Ma timing paradox of Archean gold, Abitibi greenstone-belt (Canada): New evidence from U-Pb and Pb-Pb evaporation ages of hydrothermal zircons. Geology, 22 (12): 1131-1134. doi: 10.1130/0091-7613(1994)022<1131:MTPOAG>2.3.CO;2
      Lee, J. W., Williams, I. S., Ellis, D. J., 1997. Pb, U and Th diffusionin natural zircon. Nature, 390 (6656): 159-162. doi: 10.1038/36554
      Liu, X. M., Gao, S., Di wu, C. R., et al., 2007. Simultaneous in-situ determination of U-Pb age and trace elements in zircon by LA-ICP-MS in 20μm spot size. Chinese Science Bulletin, 52 (9): 1257-1264. doi: 10.1007/s11434-007-0160-x
      Liu, Y. L., Ding, S. J., Zhang, X. W., et al., 2002. Ore-forming age of the Baolun gold deposit, Ledong Country, Hainan. Geological Review, 48 (Suppl. ): 84-87 (in Chinese with English abstract).
      Ludwig, K. R., 2003. User's manual for Isoplot 3.00: A geochronological toolkit for Microsoft Excel. Berkeley Geochronology Center Special Publication, Berkeley, CA, No4.47.
      Martin-Martin, J. D., Tritlla, J., Cardellach, E., et al., 2006. Tectonically driven fluid flow and associated low-grade metamorphism during the Alpine compression in the eastern Iberian Chain (Spain). Journal of Geochemical Exploration, 89 (1-3): 267-270. doi: 10.1016/j.gexplo.2005.11.062
      Pelleter, E., Cheilletz, A., Gasquet, D., et al., 2007. Hydrothermal zircons: A tool for ion microprobe U-Pb dating of gold mineralization (Tamlalt-Menhouhou gold deposit Morocco). Chemical Geology, 245 (3-4): 135-161. doi: 10.1016/j.chemgeo.2007.07.026
      Ramezani, J., Dunning, G. R., Wilson, M. R., 2000. Geologic setting, geochemistry of alteration, and U-Pb age of hydrothermal zircon from the Silurian Stog'er tight gold prospect, New foundland appalachians, Canada. Exploration and Mining Geology, 9 (3-4): 171-188. doi: 10.2113/0090171
      Rizvanova, N. G., Levchenkov, O. A., Belous, A. E., et al., 2000. Zircon reaction and stability of the U-Pb isotope system during interaction with carbonate fluid: Experimental hydrothermal study. Contributions to Mineralogy and Petrology, 139 (1): 101-114. doi: 10.1007/s004100050576
      Rubatto, D., 2002. Zircon trace element geochemistry: Partitioning with garnet and the link between U-Pb ages and metamorphism. Chemical Geology, 184 (1-2): 123-138. doi: 10.1016/S0009-2541(01)00355-2
      Shu, B., Wang, P. A., Dong, F. X., et al., 2006. Fluid inclusion and stableisotope studies of the Baolun gold deposit, southwestern Hainan, China. Geological Bulletin of China, 25 (7): 880-893 (in Chinese with English abstract).
      Shu, B., Wang, P. A., Li, Z. J., et al., 2004. Research on mineralizing age of Baolun gold deposit in Hainan Province and its significance. Geoscience, 18 (3): 316-320 (in Chinese with English abstract).
      Sinha, A. K., Wayne, D. M., Hewitt, D. A., 1992. The hydrothermal stability of zircon: Preliminary experimental and isotopic studies. Geochimica et Cosmochimica Acta, 56 (9): 3551-3560. doi: 10.1016/0016-7037(92)90398-3
      Watson, E. B., Cherniak, D. J., Harrison, T. M., et al. 1997. The incorporation of Pbinto zircon. Chemical Geology, 141 (1-2): 19-31. doi: 10.1016/S0009-2541(97)00054-5
      Wu, Y. B., Zheng, Y. F., 2004. Genesis of zircon and its constraints on interpretation of U-Pb age. Chinese Science Bulletin, 49 (15): 1554-1569. doi: 10.1007/BF03184122
      Xie, C. F., Zhu, J. C., Ding, S. J., et al., 2006. Age and petrogenesis of the Jianfengling granite and its relationship to metallogenesis of the Baolun gold deposit, Hainan Island. Acta Petrologica Sinica, 22 (10): 2493-2508 (in Chinese with English abstract).
      Yeats, C. J., McNaughton, N. J., Groves, D. I., 1996. SHRIMP U-Pb geochronological constraints on Archean volcanic-hosted massive sulfide and lode gold mineralization at Mount Gibson, Yilgarn craton, western Australia. Economic Geology, 91 (8): 1354-1371. doi: 10.2113/gsecongeo.91.8.1354
      Yuan, H. L., Gao, S., Liu, X. M., et al., 2004. Accurate U-Pb age and trace element determinations of zircon by laser ablation-inductively coupled plasma-mass spectrometry. Geostandards and Geoanalytical Research, 28 (3): 353-370. doi: 10.1111/j.1751-908X.2004.tb00755.x
      陈柏林, 丁式江, 李中坚, 等, 2001. 海南抱伦金矿床成矿时代研究. 地球化学, 30 (6): 525-532. doi: 10.3321/j.issn:0379-1726.2001.06.004
      丁式江, 黄定香, 李中坚, 等, 2001. 海南抱伦金矿地质特征及其成矿作用. 中国地质, 28 (5): 28-34, 18. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200105004.htm
      刘玉琳, 丁式江, 张小文, 等, 2002. 海南乐东抱伦金矿床成矿时代研究. 地质论评, 48 (增刊): 84-87. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP2002S1015.htm
      舒斌, 王平安, 董法先, 等, 2006. 海南西南部抱伦金矿床流体包裹体及稳定同位素特征. 地质通报, 25 (7): 880-893. doi: 10.3969/j.issn.1671-2552.2006.07.016
      舒斌, 王平安, 李中坚, 等, 2004. 海南抱伦金矿的成矿时代研究及其意义. 现代地质, 18 (3): 316-320. doi: 10.3969/j.issn.1000-8527.2004.03.008
      谢才富, 朱金初, 丁式江, 等, 2006. 海南尖峰岭花岗岩体的形成时代、成因及其与抱伦金矿的关系. 岩石学报, 22 (10): 2493-2508. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200610009.htm
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