Advanced Search

Indexed by SCI、CA、РЖ、PA、CSA、ZR、etc .

Volume 19 Issue 4
Aug 2008
Turn off MathJax
Article Contents
Jun DENG, Qing-fei WANG, Li WAN, Li-qiang YANG, Lei ZHOU, Jie ZHAO. Random Difference of the Trace Element Distribution in Skarn and Marbles from Shizishan Orefield, Anhui Province, China. Journal of Earth Science, 2008, 19(4): 319-326.
Citation: Jun DENG, Qing-fei WANG, Li WAN, Li-qiang YANG, Lei ZHOU, Jie ZHAO. Random Difference of the Trace Element Distribution in Skarn and Marbles from Shizishan Orefield, Anhui Province, China. Journal of Earth Science, 2008, 19(4): 319-326.

Random Difference of the Trace Element Distribution in Skarn and Marbles from Shizishan Orefield, Anhui Province, China

Funds:

the Special Plans of Science and Technology of the Ministry of Land and Resources 20010103

Trans-century Training Program Foundation by the Ministry of Education, 111 Project B07011

Changjiang Scholars and Innovative Research Team in University (PCSIRT) and State Key Laboratory of Geological Processes and Mineral Resources GPMR200640

More Information
  • Corresponding author: Deng Jun, E-mail: djun@cugb.edu.cn
  • Received Date: 28 Mar 2008
  • Accepted Date: 30 May 2008
  • Spatial distribution patterns of element concentrations can reflect the information of the mineralization processes. Both the Hurst exponent calculated by R/S analysis and the generalized fractal dimension calculated by using the multifractal model are important parameters for describing the spatial distribution of elements. Five long drill holes, named as M1, S1, S2, S3, and S4, have been selected in the Shizishan (狮子山) skarn orefield in Tongling (铜陵), Anhui (安徽) Province, China. Marbles are well developed around M1 and skarn rocks are largely distributed along S1, S2, S3, and S4 drill holes. The drill holes were sampled evenly with an interval of 10 m and 16 trace elements have been measured. The mean of the ΔD (q) (the height of the generalized dimension spectrum) in the M1 drill hole is the lowest. In addition, the mean of the Hurst exponents of the 16 elements in the M1 drill hole is also much smaller than that of S1, S2, S3, S4 drill holes, which is in accordance with the analysis of the generalized dimension. It is indicated by the generalized dimension and Hurst exponent that the distribution of trace elements in the marbles is more random than that in the skarn. The result suggests that the mineralization process can change the randomness and persistence features of the element distribution.

     

  • loading
  • Agterberg, F. P., 2001. Multifractal Simulation of Geochemical Map Patterns. Journal of China University of Geosciences, 12 (1): 31-39. http://www.cqvip.com/main/confirm.aspx?id=1001444218
    Agterberg, F. P., Cheng, Q. M., Brown, A., et al., 1996. Multifractal Modeling of Fractures in the Lac Bonnet Batholith, Manitoba. Computer and Geosciences, 22 (5): 497-507. doi: 10.1016/0098-3004(95)00117-4
    Chang, Y. F., Liu, X. P., Wu, Y. C., 1991. The Cu, Fe Metallogenic Belt in the Middle-Lower Reaches of Yangtze River. Geological Publishing House, Beijing. 379 (in Chinese with English Abstract).
    Cheng, Q., 1999. Spatial and Scaling Modeling for Geochemical Anomaly Separation. Journal of Geochemical Exploration, 65 (5): 175-194. http://www.sciencedirect.com/science/article/pii/S037567429900028X
    Cheng, Q., 2000. Multifractal Theory and Geochemical Element Distribution Pattern. Earth Science— Journal of China University of Geosciences, 25 (3): 311-318 (in Chinese with English Abstract). http://www.researchgate.net/publication/284071739_Multifractal_theory_and_geochemical_element_distribution_pattern
    Cheng, Q., 2001. Selection of Multifractal Scaling Breaks and Separation of Geochemical and Geophysical Anomaly. Journal of China University of Geosciences, 12 (1): 54-59. http://d.wanfangdata.com.cn/Periodical_dqkx-e200101008.aspx
    Cheng, Q., 2002. Multifractal Modeling and GIS Spatial Analysis of Complex Fault Systems. Geoinformatics, 13 (2): 46-49. doi: 10.6010/geoinformatics.13.46
    Cheng, Q., 2004. Quantifying the Generalized Self-Similarity of Spatial Patterns for Mineral Resources Assessment. Earth Science—Journal of China University of Geosciences, 29 (6): 733-744 (in Chinese with English Abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200406012.htm
    Cheng, Q., Agterberg, F. P., Ballantyne, S. B., 1994. The Separation of Geochemical Anomalies from Background by Fractal Methods. Journal of Geochemical Exploration, 51 (2): 109-130. doi: 10.1016/0375-6742(94)90013-2
    Deng, J., Fang, Y., Yang, L., et al., 2001. Numerical Modelling of Ore-Forming Dynamics of Fractal Dispersive Fluid Systems. Acta Geologica Sinica, 75: 220-232. http://d.wanfangdata.com.cn/Periodical/dzxb-e200102012
    Deng, J., Huang, D. H., Wang, Q. F., et al., 2004a. Experimental Remolding on the Caprock's 3D Strain Field of the Indosinian-Yanshanian Epoch in Tongling Deposit Concentrating Area. Science in China (Series D), 34 (11): 993-1001 (in Chinese).
    Deng, J., Huang, D. H., Wang, Q. F., et al., 2004b. Surplus Space Method: A New Numerical Model for Prediction of Shallow-Seated Magmatic Bodies. Acta Geologica Sinica, 78 (6): 1245-1249. doi: 10.1111/j.1755-6724.2004.tb00781.x
    Deng, J., Wang, Q. F., Huang, D. H., et al., 2006. Transport Network and Flow Mechanism of Shallow Ore-Bearing Magma in Tongling Ore Cluster Area. Science in China (Series D), 49 (3): 252-260 (in Chinese). doi: 10.1007/s11430-006-0397-2
    Deng, J., Wang, Q. F., Wan, L., et al., 2007a. Singularity of Au Distribution in Altered Rock Type Deposit—An Example from Dayingezhuang Gold Ore Deposit. In: Zhao, P. D., ed., The 12th Conference of the International Association for Mathematical Geology. China University of Geosciences Press, Wuhan. 44-47.
    Deng, J., Wang, Q. F., Yang, L. Q., et al., 2007b. Reconstruction of Ore Controlling Structures Resulting from Magmatic Intrusion into the Tongling Ore Cluster Area during the Yanshanian Epoch. Acta Geologica Sinica, 81 (2): 287-296. doi: 10.1111/j.1755-6724.2007.tb00952.x
    Hentschel, H. G. R., Procaccia, I., 1983. The Infinite Number of Generalized Dimensions of Fractals and Strange Attractors. Physica D, 8: 435. doi: 10.1016/0167-2789(83)90235-X
    Hurst, H. E., Black, R. P., Simaike, Y. M., 1965. Long-Term Storage: An Experimental Study. Constable, London. 1-145.
    Li, C., Ma, T., Cheng, J., 2004. A Fractal Interpolatory Approach to Geochemical Exploration Data Processing. Mathematical Geology, 36 (5): 593-606. doi: 10.1023/B:MATG.0000037738.34898.5e
    Malamud, B. D., Turcotte, D. L., 1999. Self-Affine Time Series: I. Generation and Analyses. Advances in Geophysics, 40: 1-90. http://www.sciencedirect.com/science/article/pii/S0065268708602939
    Panahi, A., Cheng, Q., 2004a. Modeling Lake Sediment Geochemical Distribution Using Principal Component, Indicator Kriging and Multifractal Power-Spectrum Analysis: A Case Study from Gowganda, Ontario. Geochemistry-Exploration, Environment, Analysis, 4 (4): 59-70. http://citeseerx.ist.psu.edu/viewdoc/download;jsessionid=08E670182372482277081E9059F77D85?doi=10.1.1.112.3595&rep=rep1&type=pdf
    Panahi, A., Cheng, Q., 2004b. Multifractality as a Measure of Spatial Distribution of Geochemical Patterns. Mathematical Geology, 36 (7): 827-846. doi: 10.1023/B:MATG.0000041181.32596.5d
    Turcotte, D. L., 1997. Fractals and Chaos in Geology and Geophysics. Cambridge University Press, Cambridge. 398.
    Wang, Q. F., Deng, J., Wan, L., 2007a. Fractal Analysis of Element Distribution in Damoqujiao Gold Deposit, Shandong Province, China. Proceedings of the 12th Conference of the International Association Mathematical Geology, 8: 262-265. http://d.g.wanfangdata.com.cn/Conference_WFHYXW175766.aspx
    Wang, Q. F., Deng, J., Wan, L., et al., 2007b. Discussion on the Kinetic Controlling Parameter of the Stability of Orebody Distribution in Altered Rocks in the Dayingezhuang Gold Deposit, Shandong. Acta Petrologica Sinica, 23 (4): 861-864 (in Chinese with English Abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200704019.htm
    Xie, S. Y., Bao Z. Y., 2004. Fractal and Multifractal Properties of Geochemical Fields. Mathematical Geology, 36 (7): 847-864. doi: 10.1023/B:MATG.0000041182.70233.47
    Xu, Y., Cheng, Q., 2001. A Multifractal Filter Technique for Processing Regional Geochemical Maps for Mineral Exploration. Geochemistry-Exploration, Environment, Analysis, 1 (2): 147-156. doi: 10.1144/geochem.1.2.147
    Zhao, Y. M., Zhang, Y. N., Bi, C. S., 1999. Geology of Gold-Bearing Skarn Deposits in the Middle and Lower Yangtze River Valley and Adjacent Regions. Ore Geology Reviews, 14 (3-4): 227-249. doi: 10.1016/S0169-1368(99)00008-6
  • 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(4)  / Tables(3)

    Article Metrics

    Article views(777) PDF downloads(29) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return