Formation of the world's largest REE deposit through protracted fluxing of carbonatite by subduction-derived fluids-Reference-Cited by-同舟云学术

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Formation of the world's largest REE deposit through protracted fluxing of carbonatite by subduction-derived fluids

Published:2013-05-07 Issue:1 Volume:3 Page:
ISSN:2045-2322
Container-title:Scientific Reports
language:en
Short-container-title:Sci Rep

Author:

Ling Ming-Xing,Liu Yu-Long,Williams Ian S.,Teng Fang-Zhen,Yang Xiao-Yong,Ding Xing,Wei Gang-Jian,Xie Lu-Hua,Deng Wen-Feng,Sun Wei-Dong

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://www.nature.com/articles/srep01776.pdf

Reference60 articles.

1. Yuan, Z. X., Bai, G., Wu, C. Y., Zhang, Z. Q. & Ye, X. J. Geological Features and Genesis of the Bayan Obo Ree Ore Deposit, Inner-Mongolia, China. Applied Geochemistry 7, 429–442 (1992).

2. Chao, E. C. T., Back, J. M., Minkin, J. A. & Yinchen, R. Host-rock controlled epigenetic, hydrothermal metasomatic origin of the Bayan Obo REE-Fe-Nb ore deposit, Inner Mongolia, P.R.C. Applied Geochemistry 7, 443–458 (1992).

3. Liu, Y. L., Williams, I. S., Chen, J. F., Wan, Y. S. & Sun, W. D. The significance of paleoproterozoic zircon in carbonatite dikes associated with the bayan obo REE-Nb-Fe deposit. American Journal of Science 308, 379–397 (2008).

4. Kynicky, J., Smith, M. P. & Xu, C. Diversity of Rare Earth Deposits: The Key Example of China. Elements 8, 361–367 (2012).

5. Yang, X. M. & Le Bas, M. J. Chemical compositions of carbonate minerals from Bayan Obo, Inner Mongolia, China: implications for petrogenesis. Lithos 72, 97–116 (2004).

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