Silicate, Fe-Oxide, and Au–Cu–Ag Microspherules in Ores and Pyroclastic Rocks of the Kostenga Iron Deposit, in the Far East of ... View Full Text


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Article Info

DATE

2021-05

AUTHORS

N. V. Berdnikov, V. G. Nevstruev, P. K. Kepezhinskas, V. O. Krutikova, N. S. Konovalova, I. A. Astapov

ABSTRACT

Numerous silicate, Fe-oxide, and Cu–Au–Ag microspherules are found in Fe ores and pyroclastic rocks of the Kostenga deposit, Lesser Khingan (Far East of Russia). The silicate spherules contain immiscible Fe and Si glasses, vapor voids, and mineral inclusions. The Fe-oxide spherules host magnetite with a small amount of ilmenite and Fe-rich silicate glass. The Cu–Au–Ag spherules contain inclusions with dominant CuO in their composition. These microspherules are considered to form due to rapid uplift and degassing of liquation-differentiated ore-silicate melts. The possible volcanic formation of ores and precious metal mineralization is discussed for these types of the deposits. More... »

PAGES

236-251

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    64 mineralization
    65 numerous silicates
    66 ore
    67 precious metal mineralization
    68 pyroclastic rocks
    69 rapid uplift
    70 rocks
    71 silicate
    72 silicate glasses
    73 silicate spherules
    74 small amount
    75 spherules
    76 types
    77 uplift
    78 vapor void
    79 voids
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