Epitaxy of rare earth element fluorcarbonate minerals from carbonatite dyke at Bayan Obo, Inner Mongolia, China |
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Authors: | Xueming Yang Peishan Zhang Kejie Tao Xiaoyong Yang Shuangxi Chen Minglong Zou M. J. Le Bas R. N. Wilson R. Ranson L. S. Campbell T. C. Williams P. Henderson |
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Affiliation: | (1) Department of Earth and Space Sciences, University of Science and Technology of China, 230026 Hefei, China;(2) The Advanced Center for Earth Science and Astronomy, Chinese Academy of Sciences, 230026 Hefei, China;(3) Institute of Geology, Chinese Academy of Sciences, 100029 Beijing, China;(4) Anhui Institute of Experimental Geology, 230006 Hefei, China;(5) Department of Geology, University of Leicester, LEI 7RH Leicester, UK;(6) The Natural History Museum, SW7 SBD London, UK |
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Abstract: | Rare earth element fluorocarbonate minerals such as bastnaesite and parisite are firstly discovered in carbonatite dykes from Bayan Obo, Inner Mongolia, China. Bastnaesite rarely occurs as homogeneously single crystal, but contains microfine phase of parisite. They form regular intergrowth along (0001) plane net, which is identified as epitaxy. This eptactic texture results from the variation of chemical composition of crystallizing agents of those minerals that crystallize directly from carbonatite magma. |
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Keywords: | bastnaesite parisite epitaxy carbonatite Bayan Obo |
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