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Can Rao, Rucheng Wang, Huan Hu, and Wenlan Zhan (2009): Complex internal textures in oxide minerals from the Nanping No. 31 dyke of granitic pegmatite, Fujian Province, southeastern China. Canadian Mineralogist 47(5), 1195-1212.

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Year2009
Original EntryCan Rao, Rucheng Wang, Huan Hu, and Wenlan Zhan (2009): Complex internal textures in oxide minerals from the Nanping No. 31 dyke of granitic pegmatite, Fujian Province, southeastern China. Canadian Mineralogist 47(5), 1195-1212.
Mindat Ref. ID15946265Long-form Identifiermindat:1:5:15946265:4
GUID0
Full ReferenceCan Rao, Rucheng Wang, Huan Hu, and Wenlan Zhan (2009): Complex internal textures in oxide minerals from the Nanping No. 31 dyke of granitic pegmatite, Fujian Province, southeastern China. Canadian Mineralogist 47(5), 1195-1212.
Plain TextCan Rao, Rucheng Wang, Huan Hu, and Wenlan Zhan (2009): Complex internal textures in oxide minerals from the Nanping No. 31 dyke of granitic pegmatite, Fujian Province, southeastern China. Canadian Mineralogist 47(5), 1195-1212.

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LocalityCitation Details
Pegmatite No. 31, Nanping pegmatite field, Yanping District, Nanping, Fujian, China

Mineral Occurrences

LocalityMineral(s)
Pegmatite No. 31, Nanping pegmatite field, Yanping District, Nanping, Fujian, Chinaⓘ Hydroxylapatite, ⓘ Zircon

See Also

These are possibly similar items as determined by title/reference text matching only.

Rao, C., Wang, R. C., Hu, H., Zhang, W. L. (2009) COMPLEX INTERNAL TEXTURES IN OXIDE MINERALS FROM THE NANPING No. 31 DYKE OF GRANITIC PEGMATITE, FUJIAN PROVINCE, SOUTHEASTERN CHINA. The Canadian Mineralogist, 47 (5) 1195-1212 doi:10.3749/canmin.47.5.1195
Can Rao, Rucheng Wang, Huan Hu, and Wenlan Zhan (2009): Canadian Mineralogist 47(5), 1195-1212
Rao, Can, Wang, Ru Cheng, Hu, Huan (2011) Paragenetic assemblages of beryllium silicates and phosphates from the Nanping No. 31 granitic pegmatite dyke, Fujian Province, southeastern China. The Canadian Mineralogist, 49 (5). 1175-1187 doi:10.3749/canmin.49.5.1175
Can Rao, Rucheng Wang, and Huan Hu (2009): Electron-Microprobe Compositions and Genesis of Beryls from the Nanping No. 31 Granitic Pegmatite (Fujian Province, Southeastern China). Geological Journal of China Universities 15(4), 496-505 (in Chinese with English abstract).
Rao, C.; Wang, R. C.; Zhang, A. C.; Hu, H. (2012) The Corundum + Tourmaline Nodules Related to Hydrothermal Alteration of Spodumene in the Nanping No. 31 Pegmatite Dyke, Fujian Province, Southeastern China. The Canadian Mineralogist, 50 (6). 1623-1635 doi:10.3749/canmin.50.6.1623
Rao, C., Hatert, F., Wang, R. C., Gu, X. P., Bo, F. Dal, Dong, C. W. (2015) Minjiangite, BaBe2(PO4)2, a new mineral from Nanping No. 31 pegmatite, Fujian Province, southeastern China. Mineralogical Magazine, 79 (5) 1195-1202 doi:10.1180/minmag.2015.079.5.13
Rao, Can; Wang, Rucheng; Yang, Yueqing; Hatert, Frédéric; Xia, Qunke; Yue, Xuege; Wang, Wumengyu (2017) Insights into post-magmatic metasomatism and Li circulation in granitic systems from phosphate minerals of the Nanping No. 31 pegmatite (SE China). Ore Geology Reviews, 91. doi:10.1016/j.oregeorev.2017.08.017
Rao, C., Wang, R., Hatert, F., Gu, X., Ottolini, L., Hu, H., Dong, C., Dal Bo, F., Baijot, M. (2014) Strontiohurlbutite, SrBe2(PO4)2, a new mineral from Nanping No. 31 pegmatite, Fujian Province, Southeastern China. American Mineralogist, 99 (2) 494-499 doi:10.2138/am.2014.4547
Rao, Can, Wang, Ru Cheng, Hatert, Frédéric, Baijot, Maxime (2014) Hydrothermal transformations of triphylite from the Nanping No. 31 pegmatite dyke, southeastern China. European Journal of Mineralogy, 26 (1) 179-188 doi:10.1127/0935-1221/2014/0026-2357
Rao, C., Wang, R. C., Hatert, F., & Baijot, M. (2014). Hydrothermal transformations of triphylite from the Nanping No. 31 pegmatite dyke, southeastern China. European Journal of Mineralogy, 26(1), 179-188.
Rao, Can, Wang, Ru-Cheng, Hatert, Frédéric, Wu, Run-Qiu, Wang, Qi (2020) Mineralogy and Geochemistry of Sr-Bearing Phosphates from the Nanping No. 31 Pegmatite (SE China): Implications for Sr Circulation and Post-Magmatic Processes in Granitic Systems. Minerals, 10 (6) 541 doi:10.3390/min10060541
 
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