First report of metamict alluaudite (A sodium iron manganese phosphate mineral) from Pisangan, Ajmer district, Rajasthan
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  • 作者:Yamuna Singh ; R. Viswanathan ; K. L. Mundra…
  • 关键词:Mineralogy ; Metamict Alluaudite ; Pisangan. Rajasthan
  • 刊名:Journal of the Geological Society of India
  • 出版年:2016
  • 出版时间:January 2016
  • 年:2016
  • 卷:87
  • 期:1
  • 页码:55-61
  • 全文大小:2,012 KB
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  • 作者单位:Yamuna Singh (1)
    R. Viswanathan (1)
    K. L. Mundra (2)
    P. Jagadeesan (3)
    A. K. Sharma (1)

    1. Department of Atomic Energy, Government of India, Atomic Minerals Directorate for Exploration and Research, Begumpet, Hyderabad, 500 016, India
    2. Department of Atomic Energy, Government of India, Atomic Minerals Directorate for Exploration and Research, Pratapnagar, Jaipur, 302 033, India
    3. Department of Atomic Energy, Government of India, Atomic Minerals Directorate for Exploration and Research, Nagarbhavi, Bangalore, 560 072, India
  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Geology
    Geosciences
    Geography
    Mineralogy
  • 出版者:Springer India, co-published with Geological Society of India
  • ISSN:0974-6889
文摘
For the first time we report alluaudite from India, which is metamict and is hosted in a zoned pegmatite, near Pisangan, Ajmer district, Rajasthan. Alluaudites known till date, all over the world, are non-metamict type. Therefore, the alluaudite reported from the area is the first locality in the world for the metamict-type of alluaudite. The most conspicuous features exhibited by the alluaudite are various types of cracks in different directions and shapes, including its isotropic nature. The calculated crystallographic parameters of the reported alluaudite are: a0 = 11.9874 Å, b0 = 12.5144 Å, and c0 = 6.4136 Å, β = 114.240 with unit-cell volume (V) = 877.31 Å3, which are in agreement with the values of alluaudite standard. Geochemical data indicates high content of P (32.30% P2O5), Fe (30.2% Fe2O3), Mn (10.62% MnO), besides Mg (7.71% MgO), Ca (5.60% CaO), Na (3.40% Na2O) and Si (2.30% SiO2), and appreciable amount of water of hydration (3.50% LOI). It is highly radioactive due to uranium (2.28% U3O8) and thorium (185 ppm Th). Calculated structural formula of the alluaudite is Na1+ 0.59Ca2+ 0.54Mn2+ 0.80Mg2+ 1.02Fe3+ 2.03Al3+ 0.037U4+ 0.043P5+ 2.45O12. The chondrite-normalised plot shows enrichment of HREE relative to LREE with pronounced negative Eu-anomaly (Eu/Eu* = 0.46). Such a high negative Eu-anomaly suggests extremely fractionated nature of the host pegmatite. Keywords Mineralogy Metamict Alluaudite Pisangan. Rajasthan

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