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Zapiski RMO (Proceedings of the Russian Mineralogical Society)
ISSN 0869-6055                     zrmo.minsoc.ru
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Year 2017 Part 146 Issue 3
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Article list
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Vetrin V. R., Belousova E. A., Kremenetskiy A. A.
Lu-Hf isotope systematics of zircon from xenoliths of the lower crust of the Belomorian mobile belt
pages 1-16
Vishnevsky A. V., Belogub E. V., Charykova M. V., Krivovichev V. G., Blinov I. A.
Thermodynamics of arsenates, selenites and sulfates in the oxidation zone of sulfide ores. XIV. Minerals of selenium in the oxidation zone of the Jubileynoe massive sulfide deposit, the South Urals
pages 17-29
New minerals
Yakovenchuk V. N., Pakhomovsky Ya. A., Konoplyova N. G., Panikorovskii T. L., Mikhailova Yu. A., Bocharov V. N., Krivovichev S. V., Ivanyuk G. Yu.
Epifanovite, NaCaCu5(PO4)4lAsO2(OH)2] ? 7H2O a new mineral from the Kester deposit (Sakha-Yakutia, Russia)
pages 30-38
Panikorovskii T. L., Krivovichev S. V., Yakovenchuk V. N., Ivanyuk G. Yu.
The crystal structure of epifanovite
pages 39-50
Minerals and mineral parageneses
Aplonov V. S., Zolotarev A. A.
Peculiarities of the chemical composition of spinel group minerals in the Talnakh copper-nickel ore deposit (North-West of the Siberian platform)
pages 51-68
Putintseva E. V., Spiridonov E.M.
llmenite group minerals in the oldest Russian diamondiferous kimberlites of Kimozero, Karelia
pages 69-86
Konopleva N.G., Ivanyuk G. Yu., Pakhomovsky Ya. A., Yakovenchuk V. N., Mikhailova Yu. A.
Micas of the phlogopite-annite series in rocks of the Khibiny massif (Kola Peninsula, Russia)
pages 87-103
Investigation techiques for minerals, rocks and ores
Brivin S. N., Dolivo-Dobrovolsky D. V., Krzhizhanovskaya M.G.
Software for processing the X-ray powder diffraction data obtained from the curved image plate detector of Rigaku RAXIS Rapid ll diffractometer
pages 104-107
јрхеоминералоги€
Summanen I. M., Chazhengina S. Yu., Svetov S. A.
Mineralogy and technological analysis of ceramics (on materials from medieval sites of the Nomi-Western Ladoga Area)
pages 108-123
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pages 124-126
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