Spectroscopy and Spectral Analysis, Volume. 33, Issue 10, 2694(2013)
Study on the Micro-FTIR and Raman Spectra of the Alluvial Diamonds from Yangtze Craton and Their Geological Significances
The FTIR and Raman spectra of 10 diamonds from Yuanshui, Hunan province show that the alluvial diamonds from this area are mostly IaAB type, with a significant character that the A-center is enriched relatively; the nitrogen concentration in the diamonds is between 38.20 and 840.67 μg·g-1, which has a tremendous distinction in different crystal. The residence time of the diamonds in the mantle are between 0.043 and 3.315 Ga, which is also has a great difference in different diamond grains. The remotest residence time (3.315 Ga) of one diamond is older than the most aged rock (3.285 Ga) in Xiang-E-Qian-Gui contiguous zone. A remarkable environment change had took place during the process of diamonds formation. The formation depth of dodecahedral diamonds is deeper than that of the octahedral ones.
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ZENG Xiang-qing, ZHENG Yun-long, YANG Zhi-jun, AI Qun, HU Piao-ye. Study on the Micro-FTIR and Raman Spectra of the Alluvial Diamonds from Yangtze Craton and Their Geological Significances[J]. Spectroscopy and Spectral Analysis, 2013, 33(10): 2694
Received: Jan. 29, 2013
Accepted: --
Published Online: Oct. 23, 2013
The Author Email: Xiang-qing ZENG (yangzhj@mail.sysu.edu.cn)