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Siderite from Sikhote-Alin Mountains, Russia

Russia
 
  • Primorsky Krai
    • Dalnegorsk Urban District
      • Dalnegorsk
Simanenko, L.F., Ratkin, V.V. & Turchin, V.A. (2015): Mineral assemblages of the porphyry tin-polymetallic ores of Mount Krasnaya paleovolcano of the Krasnogorsky deposit in the Dal’negorsk ore district. Russ. J. of Pac. Geol. 9, 120-135.
Grant, R.W., Wilson, W.E. (2001) Famous Mineral Localities: Dal'negorsk, Primorskiy Kray, Russia. The Mineralogical Record, 32(1), 3-30.
Dobovol'skaya, M. G., Baskina, V. A., Balashova, S. P., Kenisarin, A. M., Arakelyants, M. M., Klimachev, L. A., & Muravitskaya, G. N. (1990). Order of Formation of the Ores and Mafic Dikes of the Nikolayevsk Deposit (Southern Primor'ye). International Geology Review, 32(4), 391-403.
    • Kavalerovo mining district
Кокорин, А. М., Гвоздев, В. И., Гоневчук, В. Г., Гоневчук, Г. А., Коростелев, П. Г., & Семеняк, Б. И. (2000). Месторождение Искра–новый объект Кавалеровского оловорудного района (геология, состав руд, генезис). Рудные месторождения континентальных окраин, (1), 226-247. Iskra deposit is a new object of the Kavalerovo tin district (geology, ore composition, genesis)
    • Krasnoarmeysky District
      • Arminsky ore district
Gonevchuk, V. G., Korostelev, P. G., & Semenyak, B. I. (2005). Genesis of the Tigrinoe tin deposit (Russia). Geology Of Ore Deposits C/C Of Geologiia Rudnykh Mestorozhdenii, 47(3), 223.
In Collection of Martin Slama, ex Veselin Atanasov, there are 2 papers in russian language on bertrandite from this locality available but not translated in english
    • Olginsky District
Kazachenko, V. T., Khanchuk, A. I., Lavrik, S. N., & Perevoznikova, E. V. (2013). Phlogopite-olivine rocks of the Taukha terrane in southeastern Sikhote Alin. Russian Journal of Pacific Geology, 7(5), 330-345.
[var. Oligonite] Dobrovol’skaya, M.G., Genkin, A.D., Bortnikov, N.S., and Golovanova, T.I. (2008): Geology of Ore Deposits 50(1), 75-85.
[var. Manganese-bearing Siderite] American Mineralogist, Vol. 64, 1979, pp. 432-435
 
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