Coalingite from kimberlite breccia of the Manchary pipe, Central Yakutia

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• 作者：N. V. Zayakina ; O. B. Oleinikov ; T. I. Vasileva ; N. A. Oparin
• 刊名：Geology of Ore Deposits
• 出版年：2015
• 出版时间：December 2015
• 年：2015
• 卷：57
• 期：8
• 页码：732-736
• 全文大小：803 KB
• 参考文献：Cesnokov, B., Kotrly, M., and Nisanbajev, T., Brennende Abraumhalden und Aufschlüsse im Tscheljabinsker Kohlenbecken—eine reiche Mineralienküche, Mineral. Welt, 1998, Bd. 9, pp. 54–63.
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  Smelov, A.P., Andreev, A.P., Altukhiva, Z.A., Babushkina, S.A., Bekrenev, K.A., Zaitsev, A.I., Izbekov, E.D., Koroleva, O.V., Mishnin, V.M., Okrugin, A.V., and Surnin, A.A., Kimberlites of the Manchary pipe: a new kimberlite field in Central Yakutia, Russian Geol. Geophys., 2010, vol. 51, no. 1, pp. 121–126.CrossRef
  
• 作者单位：N. V. Zayakina (1)
  O. B. Oleinikov (1)
  T. I. Vasileva (1)
  N. A. Oparin (1)
  
  1. Institute of Geology of Diamond and Precious Metals, Siberian Branch, Russian Academy of Sciences, pr. Lenina 39, Yakutsk, 677980, Russia
  
• 刊物主题：Mineral Resources;
• 出版者：Springer US
• ISSN：1555-6476

文摘

Coalingite, Mg₁₀Fe₂(CO₃)(OH)₂₄ · 2H₂O, rare Mg–Fe hydrous carbonate, has been found in the course of the mineralogical study of a disintegrated kimberlite breccia from the Manchary pipe of the Khompu–May field located in the Tamma Basin, Central Yakutia, 100 km south of Yakutsk. Coalingite occurs as small reddish brown platelets, up to 0.2 mm in size. It is associated with lizardite, chrysotile and brucite, which are typical kimberlitic assemblage. Coalingite is a supergene mineral, but in this case, it is produced by the interaction of brucite-bearing kimberlite and underground water circulating through a vertical or oblique fault zone. Original Russian Text © N.V. Zayakina, O.B. Oleinikov, T.I. Vasileva, N.A. Oparin, 2015, published in Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, 2015, No. 1, pp. 115–121.