• 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

    留言板

    尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

    姓名
    邮箱
    手机号码
    标题
    留言内容
    验证码

    贵州织金含稀土磷矿床的Sm-Nd同位素年龄及其地质意义

    施春华 胡瑞忠

    施春华, 胡瑞忠, 2008. 贵州织金含稀土磷矿床的Sm-Nd同位素年龄及其地质意义. 地球科学, 33(2): 205-209.
    引用本文: 施春华, 胡瑞忠, 2008. 贵州织金含稀土磷矿床的Sm-Nd同位素年龄及其地质意义. 地球科学, 33(2): 205-209.
    SHI Chun-hua, HU Rui-zhong, 2008. Samarium-Neodymium Radiometric Dating and Its Geologic Implication of the Zhijin REE-Bearing Phosphorites, Guizhou Province, Southwest China. Earth Science, 33(2): 205-209.
    Citation: SHI Chun-hua, HU Rui-zhong, 2008. Samarium-Neodymium Radiometric Dating and Its Geologic Implication of the Zhijin REE-Bearing Phosphorites, Guizhou Province, Southwest China. Earth Science, 33(2): 205-209.

    贵州织金含稀土磷矿床的Sm-Nd同位素年龄及其地质意义

    基金项目: 

    中国科学院知识创新工程重要方向项目 KZCX3-SW-125

    浙江林学院科学研究发展基金项目 2351000584

    详细信息
      作者简介:

      施春华(1976-), 女, 目前主要从事旅游环境地球化学等教学与科研工作.E-mail: shichunhua7924@163.com

    • 中图分类号: P597

    Samarium-Neodymium Radiometric Dating and Its Geologic Implication of the Zhijin REE-Bearing Phosphorites, Guizhou Province, Southwest China

    • 摘要: 为探讨贵州织金含稀土磷矿床的形成时间和成矿物源, 利用Sm-Nd同位素稀释法对该矿床磷块岩中6个小壳化石及胶磷矿样品进行了年龄测定.样品的质谱分析测试结果显示, 样品的147Sm/144Nd与143Nd/144Nd构成了一条相关性良好的线性等时线; 计算结果表明织金含稀土磷矿床具有533±22Ma的Sm-Nd等时年龄, εNd (t) 值为-2.44~-2.77, 表明它们具有相同的成因和相近的形成时代, 本次测得年龄代表着真实的成矿年龄; 二阶段Nd的模式年龄为1313~1338Ma.结合前人对该矿床稀土元素地球化学的研究成果表明, 织金含稀土磷矿床的成矿物源有新生地幔物质组分的加入.

       

    • 图  1  织金含稀土磷矿床地质简图及采样位置

      1.三叠系; 2.二叠系; 3.石炭系; 4.寒武系明心寺组; 5.寒武系牛蹄塘组; 6.震旦系灯影组; 7.地层界线; 8.断层; 9.采样位置

      Fig.  1.  Geological sketch map of the Zhijin

      图  2  样品的Sm-Nd等时线

      Fig.  2.  Sm-Nd isochron for the sample

      表  1  样品的Sm、Nd同位素测定结果

      Table  1.   Sm, Nd isotopic compositions of samples

    • Chen, J. F., 1989. Nd isotopes of the lower metamorphite and sedimentary rock and their provenance in the south of Anhui. Chinese Science Bulletin, 34 (20): 1572-1574 (in Chinese). doi: 10.1360/csb1989-34-20-1572
      Cowie, J. W., Johnson, M. R. W., 1985. The chronology of the geological record. Geol. Soc. Lond. Mem. , 10: 47-64. doi: 10.1144/GSL.MEM.1985.010.01.06
      Davidek, K., Landing, E., Bowring, S. A., et al., 1998. New upper most Cambrian U-Pb date from Avalonian Wales and age of the Cam-Ordovician boundary. Geological Magazine, 133: 303-309.
      DePaolo, D. J., 1988. Neodymiumisotope geochemistry: An introduction. Springer-Verlag, Berlin, 76-80.
      DePaolo, D. J., Wasserburg G. J., 1976. Nd isotopic variations and petrogenetic models. Geophy. Res. Lett. , 3: 249-252. doi: 10.1029/GL003i005p00249
      Dongye, M. X., 2001. Regional oreforming regulation of phosphorite in Yangtze massif in the times of Doushantuo and Meishucun ages. Geology of Chemical Minerals, 23 (4): 193-209 (in Chinese with English ab-stract).
      Du, Y. S., Zhu, J., Gu, S. Z., 2006. Sedimentary geochemistry and tectonic significance of Ordovician cherts in Sunan, North Qilian Mountains. Earth Science—Journal of China University of Geosciences, 31 (1): 101-109 (in Chinese with English abstract).
      Grotzinger, J. P., Bowring, S. A., Aylor, H. Z., et al., 1995. Biostratigraphic and geochronologic constraints on early animal evolution. Science, 270: 598-604. doi: 10.1126/science.270.5236.598
      Landing, E., Bowring, S. A., Davidek, K. L., et al., 1998. Duration of the Cambrian: U-Pb ages of the volcanic ashes from Avalon and Gondwana. Canadian Journalof Earth Sciences, 35: 329-338. doi: 10.1139/e97-107
      Li, X. H., 1996. Nd isotopic evolution of sediments from the southern margin of the Yangtze block and its tectonic significance. Acta Petrologica Sinica, 12 (3): 359-369 (in Chinese with English abstract).
      Liu, J. R., 1999. Disscussion on comprehensive utilization of Xinhua phosphorite ore in Zhijin, Guizhou. Guizhou Geology, 16 (3): 253-258 (in Chinese with English ab-stract).
      Luo, H. L., Jiang, Z. W., Tang, L. D., 1994. The model section of the Lower Cambrian, China. The Science and Technology Publishing House of Yunnan, Kunming (in Chinese).
      Luo, H. L., Jiang, Z. W., Wu, X. C., et al., 1991. Lucubrate of the Precambrian and Cambrian of the Meishucun sectionin Jinning, Guizhou Province. Acta Geologica Sinica, 85 (4): 367-375 (in Chinese with English abstract).
      Michard, A., 1985. Nd isotopes in French Phanerozoic shales: External vs. internal aspects of crustal evolution. Geochimica et Cosmochimica Acta, 49 (2): 601-610. doi: 10.1016/0016-7037(85)90051-1
      Qian, Y., 1977. Hyolitha and other fossil of the Meishucun age of Early Cambrian in the Southwest China. Acta Palaeontologica Sinica, 16 (2): 29-34 (in Chinese).
      Qian, Y., Yin, G. Z., 1984. Study of Early Cambrian small shelly fossils in Guizhou. Analects of Stratigraphic Paleontology, 13: 64-68 (in Chinese).
      Shi, C. H., Hu, R. Z., Wang, G. Z., 2006. Element geochemistry of Zhijin phosphorites, Guizhou Province. Acta Mineralogica Sinica, 26 (2): 169-174 (in Chinese with English abstract).
      The National Stratum Committee Secretariat, 1998. The chronological scale of China (recommended scheme). Journal of Stratigraphy, 22 (4): 299-303 (in Chinese).
      Wang, Y. X., Yang, J. D., Tao, X. C., et al., 1988. The test method of samariumand neodymiumisotope andits application of fossil, mineral and rock sample. Journal of Nanjing University (Natural Sciences), 24 (3): 297-308 (in Chinese with English abstract).
      Wu, X. H., Han, Z. J., Cai, J. F., et al., 1999. Phosphorite of Guizhou. Geological Publishing House, Beijing (in Chinese).
      Xing, Y. S., Yin, C. Y., Gao, L. Z., 1999. Boundaries and subdivision of the Simian System. Geoscience, 13 (2): 202-204 (in Chinese with English abstract).
      Xue, X. F., 1984. The section of the boundary of Precambrianand Cambrian in Jinning Meishucun, Yunnan Province. The People's Publishing House of Yunnan, Kunming (in Chinese).
      Yang, J. D., Sun, W. G., Wang, Z. Z., et al., 1996. Sm-Nd isotopic age of Precambrian-Cambrian boundary in China. Geological Magazine, 133 (1): 53-61. doi: 10.1017/S001675680000724X
      Yang, J. D., Sun, W. G., Wang, Y. X., et al., 1992. Samarium-neodymiumisotope radiometric dating of the fossil on the boundary of Precambrian-Cambrian at the section of Meishucun in Jinning, Yunnan Province. Science in China (Ser. B), 25 (3): 322-327 (in Chinese).
      Yang, W. D., Xiao, J. K., Yu, B. S., et al., 1997. Sedimentation, geochemistry and the continuable exploitation stratagemof phosphorite in Yunnan and Guizhou Provinces. Geological Publishing House, Beijing (in Chinese).
      Zhang, J., Chen, D. L., 2000. Scanning electron microscope study of the ore-bearing REE in Xinhua phosphorite, Zhijin, Guizhou. Journal of Mineralogy and Petrology, 20 (3): 59-64 (in Chinese with English abstract).
      Zheng, S. F., Wang, Y. G., 1984. The petrology of Meishucun age phosphorites in the Yangzi, Guizhou Province. In: Wang, Y. G., et al. eds., The Upper Precambrian and Sinian-Cambrian boundary in Guizhou. The People'sPublishing House of Guizhou, Guiyang, 135-146 (in Chinese).
      陈江峰, 1989. 皖南浅变质岩和沉积岩的汝同位素组成及沉积物物源区. 科学通报, 34 (20): 1572-1574. doi: 10.3321/j.issn:0023-074X.1989.20.002
      东野脉兴, 2001. 扬子地块陡山沱期与梅树村期磷矿区域成矿规律. 化工矿产地质, 23 (4): 193-209. doi: 10.3969/j.issn.1006-5296.2001.04.001
      杜远生, 朱杰, 顾松竹, 2006. 北祁连肃南一带奥陶纪硅质岩沉积地球化学特征及其多岛洋构造意义. 地球科学——中国地质大学学报, 31 (1): 101-109. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200601014.htm
      李献华, 1996. 扬子南缘沉积岩的Nd同位素演化及其大地构造意义. 岩石学报, 12 (3): 359-369. doi: 10.3321/j.issn:1000-0569.1996.03.001
      刘家仁, 1999. 试谈织金磷矿的综合利用问题. 贵州地质, 16 (3): 253-258. https://www.cnki.com.cn/Article/CJFDTOTAL-GZDZ199903012.htm
      罗惠麟, 蒋志文, 唐良栋, 1994. 中国下寒武统建阶层型剖面. 昆明: 云南科技出版社.
      罗惠麟, 蒋志文, 武希彻, 等, 1991. 云南晋宁梅树村剖面前寒武系—寒武系界线的深入研究. 地质学报, 85 (4): 367-375. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE199104006.htm
      钱逸, 1977. 华中西南区早寒武世梅树村阶的软舌螺纲及其他化石. 古生物学报, 16 (2): 29-34. https://www.cnki.com.cn/Article/CJFDTOTAL-GSWX197702006.htm
      钱逸, 尹恭正, 1984. 贵州早寒武世早期小壳动物化石的研究. 地层古生物论集, 13: 64-68. https://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDJ198400018008.htm
      全国地层委员会秘书处, 1998. 中国地质年代表(推荐方案). 地层学杂志, 22 (4): 299-303.
      施春华, 胡瑞忠, 王国芝, 2006. 贵州织金磷矿岩元素地球化学特征. 矿物学报, 26 (2): 169-174. doi: 10.3321/j.issn:1000-4734.2006.02.009
      王银喜, 杨杰东, 陶仙聪, 等, 1988. 化石、矿物和岩石样品的Sm-Nd同位素实验方法研究及其应用. 南京大学学报(自然科学版), 24 (3): 297-308. https://www.cnki.com.cn/Article/CJFDTOTAL-NJDZ198802017.htm
      吴祥和, 韩至钧, 蔡继锋, 等, 1999. 贵州磷块岩. 北京: 地质出版社.
      邢裕盛, 尹崇玉, 高林志, 1999. 震旦系的范畴、时限及内部划分. 现代地质, 13 (2): 202-204. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ902.019.htm
      薛啸峰, 1984. 中国云南晋宁梅树村震旦系-寒武系界线层型剖面. 昆明: 云南人民出版社.
      杨杰东, 孙卫国, 王银喜, 等, 1992. 云南晋宁梅树村剖面前寒武系-寒武系界线化石Sm-Nd同位素年龄测定. 中国科学(B), 25 (3): 322-327. https://www.cnki.com.cn/Article/CJFDTOTAL-JBXK199203015.htm
      杨卫东, 肖金凯, 于炳松, 等, 1997. 滇黔磷块岩沉积学、地球化学与可持续开发战略. 北京: 地质出版社.
      张杰, 陈代良, 2000. 贵州织金新华含稀土磷矿床扫描电镜研究. 矿物岩石, 20 (3): 59-64. doi: 10.3969/j.issn.1001-6872.2000.03.011
      郑淑芬, 王砚耕, 1984. 贵州扬子区梅树村期磷块岩岩石学. 见: 王砚耕, 等, 贵州上前寒武系及寒武系界线. 贵阳: 贵阳人民出版社, 135-146.
    • 加载中
    图(2) / 表(1)
    计量
    • 文章访问数:  3836
    • HTML全文浏览量:  507
    • PDF下载量:  96
    • 被引次数: 0
    出版历程
    • 收稿日期:  2007-05-25
    • 刊出日期:  2008-03-25

    目录

      /

      返回文章
      返回