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-jun; ZHOU Wen-xiu; ZENG Xuan; HUANG Shan-shan; LI Xiao-xiao; CHEN Yao-ming

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

Journals >Spectroscopy and Spectral Analysis >Volume 37 >Issue 6 >Page 1739 > Article

Spectroscopy and Spectral Analysis
Vol. 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-jun^1、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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DOI: 103964/jissn1000-0593(2017)06-1739-06 Cite this Article

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 Copy Citation Text

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References

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

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

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

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

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

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

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

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