Spectroscopy and Spectral Analysis, Volume. 37, Issue 6, 1739(2017)

Study on the CL and FTIR Spectra of the Alluvial Diamond from Western Yangtze Craton and Its Significance in the Growth Rate Analysis of the Diamond

YANG Zhi-jun1,2、*, ZHOU Wen-xiu1, ZENG Xuan1, HUANG Shan-shan1, LI Xiao-xiao1, and CHEN Yao-ming1
Author Affiliations
  • 1[in Chinese]
  • 2[in Chinese]
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    References(9)

    [1] [1] Orlov Y. The Mineralogy of the Diamond. John Wiley &Sons, Inc., 1977. 116.

    [3] [3] Yang Z J, Li H Z, Peng M S, et al. Chinese Science Bulletin, 2008, 53(1): 137.

    [4] [4] Jiang T, Xu K. Carbon, 1995, 33(12): 1663.

    [5] [5] Davies G. Nature, 1981, 290: 40.

    [6] [6] Field J E. The Properties of Natural and Synthetic Diamond. London: Academic Press, 1992. 36, 81.

    [7] [7] Chrenko R M, Tuft R E, Strong H M. Nature, 1977, 270: 141.

    [8] [8] Evans T, Harris J W. Nitrogen Aggregation, Inclusion Equilibration Temperatures and the Age of Diamonds. 4th International Kimberlite Conference Extended Abstracts Geological Society of Australia, Abstracts Series, 1986, 16: 386.

    [9] [9] Evans T, Qi Z. Proc. Roy. Soc. Lond., 1982, 318A: 159.

    [11] [11] Taylor W R, Jaques A L, Ridd M. American Mineralogist, 1990, 75: 1290.

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    YANG Zhi-jun, ZHOU Wen-xiu, ZENG Xuan, HUANG Shan-shan, LI Xiao-xiao, CHEN Yao-ming. Study on the CL and FTIR Spectra of the Alluvial Diamond from Western Yangtze Craton and Its Significance in the Growth Rate Analysis of the Diamond[J]. Spectroscopy and Spectral Analysis, 2017, 37(6): 1739

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    Paper Information

    Received: Jan. 4, 2016

    Accepted: --

    Published Online: Jul. 10, 2017

    The Author Email: YANG Zhi-jun (yangzhj@mailsysueducn)

    DOI:103964/jissn1000-0593(2017)06-1739-06

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