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Journal/NDM45 2010 eng

Версия от 14:48, 7 января 2018; Kronrod (обсуждение | вклад) (New Minerals and Their Varieties, New Finds of Rare Minerals, Mineral Paragenesis)

New Data on Minerals, vol.45, 2010

New data on Minerals. Volume 45. 2010. 168 pages, 99 images, drawings, schemes.
Editor: Prof. Margarita I. Novgorodova.
Publication of the Institution of Russian Academy of Sciences, Fersman Mineralogical Museum RAS.

Summary

This volume contains papers on the newly discovered mineral species – aleksandrovite, the Sn-analogue of baratovite, and åskagenite-(Nd), a new mineral of epidote supergroup. Discoveries of the rare minerals – irarsite (from ores of the Shanuch deposit in Kamchatka), orickite, jaipurite, westerveldite, edgarite, tungstenite and other chalcogenides (from the Khibiny massif in Kola peninsula) are described. New data on accessory minerals from the Semeninskaya pit in the Aduy pegmatite field in the Ural Mts., on arsenosulvanite and other sulphides from the Lebedinoe deposit in the Aldan Mts., on the composition and features of native gold from an ore occurrence in South-Eastern Kamchatka, are given. Zoned crystals of monazite(Ce) from granite pegmatites of the Ilmeny Mts. are studied, including radiology dating. Problems of mineralogy and geochemistry of tetravalent uranium, uranium ores and sulfide-oxide associations in modern submarine pyrites, are covered.
In the chapter “Mineral museums and collections” there is a paper on the exhibition in the Fersman Mineralogical Museum RAS dedicated to the 125th anniversary of Alexander N. Labuntsov – the discoverer of apatite deposits in the Khibiny Mts.
The next chapter – “Personalities” – for the first time brings forward letters found in the RAS archives from Alexander N. Labuntsov to academician Vladimir I. Vernadsky. The “Mineralogical notes” chapter includes description of rare intergrowth twins of magnetite from the Kurzhunkul deposit, Kazakhstan, and discussion of previous mistakes in the calculation of the chemical composition of some minerals.
The “Discussions” is represented by the paper on the problems of the definition of a valid mineral species and metastable mineralization.
The journal is of interest to mineralogists, geochemists, geologists and also researchers of Natural History museums, collectors and amateurs.

Editorial Board
  • Editor in Chief Margarita I. Novgorodova, Doctor in Science, Professor
  • Executive Editor Elena A. Borisova, Ph.D.
  • Eugeny I. Semenov, Doctor in Science,
  • Svetlana N. Nenasheva, Ph.D.,
  • Elena N. Matvienko, Ph.D.,
  • Marianna B. Chistyakova, Ph.D.,
  • Mikhail E. Generalov, Ph.D.
Publishing group
  • Photo Michael B. Leybov
  • Leader of Publishing group Michael B. Leybov
  • Managing Editor Ludmila A. Cheshko
  • Art Director Nikolay O. Parlashkevich
  • Editor Andrey L. Cheshko
  • Design and Layout Ivan A. Glazov
  • Translators Maria S. Alferova, Il'ya A. Anisimov, Ivan A. Baksheev, Mark Fed’kun, Valerii V. Gerasimovskii, Mikhail Povarennykh
  • Editors (English Style) Patricia Gray, Frank C. Hawthorne, Peter Modreski


Authorized for printing by Institution of Russian Academy of Sciences, Fersman Mineralogical Museum RAS
Text, photo, drawings and schemes, Institution of Russian Academy of Sciences,
Fersman Mineralogical Museum RAS, 2010
Design BRITAN Ltd, 2010
Published by Institution of Russian Academy of Sciences, BRITAN Ltd Fersman Mineralogical Museum RAS Box 71 Moscow Bld. 18/2 Leninskii Prospekt Moscow 119071 Russia Phone/fax +7 (495) 629-48-12 Phone +7 (495) 952-00-67; fax +7 (495) 952-48-50 email: minbooks@online.ru
email: mineral@fmm.ru www.minbook.com
www.fmm.ru
Circulation 300 copies
Printed in Russia

Сontent

New Minerals and Their Varieties, New Finds of Rare Minerals, Mineral Paragenesis

Pdf icon.pngPautov L.А., Agakhanov А.А., Karpenko V.Y., Gafurov F.G. Aleksandrovite, KLi3Ca7Sn2[Si6O18]2F2 – a new tin mineral, p. 5 - 16

Aleksandrovite, KLi3Ca7Sn2[Si6O18]2F2 is a new mineral, the tin analogue of baratovite. It was discovered in a moraine boulder of microcline-calcite rock, along with quartz, albite, aegirine-hedenbergite pyroxene, in the Darai-Pioz glacier (Tajikistan). The mineral association is represented by baratovite, fluorite, miserite, Sn-bearing titanite, bazirite, pabstite, Sn-bearing sogdianite, sugilite, turkestanite, fluorapatite (apatite(CaF)). The new mineral occurs in two types: a) minute (up to 50–70 μm) lamellar grains with no zoning visible under BSE, and b) crystals (up to 0.8 mm) and aggregates of zoned and sectorial grains with separate zones of aleksandrovite, and baratovite or katayamalite. The mineral is colourless, transparent, with vitreous lustre and pearl lustre on cleaved surface. Streak colour is white. Cleavage is perfect along (001). Density (measured) = 3.05(2) g/cm3, density (calculated) = 3.07(2) g/cm3. Microhardness is 300 kg/mm2. Mohs hardness is 4–4.5. It fluoresces light-blue under short wave UV (254 nm). The mineral is biaxial, optically negative: np = 1.629(2), nm = 1.635(4), ng = 1.638(2) (589 nm); 2V (calculated) = –70.3°. Dispersion is strong, r > v. Elongation is positive, angle of extinction varies from 0° to 22°. Aleksandrovite is monoclinic, C2/c, a = 17.01(2), b = 9.751(6), c = 21.00(2) Å, b = 112.45(8)° , V = 3219(7) Å3 , Z = 4. The strongest X-Ray lines are as follows: (d in Å (I) (hkl)): 4.86(21)(31–1); 3.712(33)(312); 3.234(100)(006); 3.206(34)(223); 3.039(28)(025); 2.894(42)(314); 2.425(42)(008); 1.950(25)(426). Chemical analysis (EMPA, an average out of 17 analyses; Li2O – ICP OES, H2O – calculated; wt.%): SiO2 – 48.01, Al2O3 – 0.07, TiO2 – 2.86, SnO2 – 12.84, ZrO2 – 1.27, Nb2O5 – 0.11, Fe2O3 – 0.27, Ce2O3 – 0.04, MgO – 0.05, CaO – 25.52, SrO – 0.39, Na2O – 0.20, K2O – 2.91, Li2O – 3.01, F – 1.71, H2O – 0.39, (-O=F2) = 0.72, total 99.12. Empiric formula of aleksandrovite - (K0.93Na0.10)1.03Li3.02(Ca6.82Sr0.06Mn0.04Mg0.02)6.94(Sn1.28Ti0.54 Zr0.15Fe0.05Nb0.01)2.03(Si11.98Al0.02)12O36.00[F1.35(OH)0.65]2.00. IR spectrum of aleksandrovite is similar to that of baratovite, the strongest absorption strips are: 1083, 1024, 974, 950, 673, 607, 568, 520, 470, 440 cm-1. Compatibility index is 1 – (Kp/Kc) = –0.005. The mineral is named to honour of the well-known Russian geochemist, geologist and mineralogist Stanislav Mikhailovich Aleksandrov (born in 1932) for his great contribution in geology, geochemistry and mineralogy of tin. The type specimen is stored in the Fersman Mineralogical Museum RAS in Moscow (registration number 3825/1). читать далее...



Pdf icon.pngChukanov N.V., Göttlicher J., Möckel S., Sofer Z., Van К.V., Belakovskiy D.I. Åskagenite(Nd), Mn2+NdAl2Fe3+(Si2O7)(SiO4)O2 – a new mineral of the epidote supergroup, p. 17 - 22

A new epidote-supergroup mineral åskagenite-(Nd) was discovered in specimens from a granite pegmatite outcropped at the Åskagen deposit near the town of Filipstad, Värmland, Sweden, in association with potassic feldspar, quartz, bastnäsite, thorite, the Nd-dominant analogue of allanite-(Ce), brookite, gadolinite-(Y) and allophаne. The new mineral forms coarse prismatic and flattened crystals up to 1×4 cm in size. Åskagenite-(Nd) is black, with resinous lustre and brown streak, translucent in thin fragments; brittle, Mohs’ hardness 6, fracture conchoidal. Dmeas = 3.737(5) g/cm3 (for a metamict sample); Dcalc = 4.375 g/cm3 (for a sample heated at 600°C during 1 h in nitrogen). Åskagenite-(Nd) is optically isotropic, n = 1.712(2). IR spectrum is given. Chemical composition (electron microprobe, water determined by Alimarin method, Fe2+:Fe3+ by Mössbauer data, valency of Mn by XANES spectroscopic data, wt.%): CaO 0.27, Y2O3 2.27, La2O3 0.44, Ce2O3 7.99, Pr2O3 1.76, Nd2O3 11.21, Sm2O3 3.01, Yb2O3 0.21, ThO2 0.72, MnO 7.98, FeO 7.75, Fe2O3 9.16, Al2O3 15.85, SiO2 29.51, H2O 0.55, total; 98.75. Crystalchemical formula: (Mn2+0.69Fe2+0.26Ca0.03)∑0.98(Nd0.41Ce0.30Y0.12Sm0.10Pr0.07La0.02Yb0.01Th0.02)∑1.05(Al0.90Fe3+0.10)∑1.00Al1.00(Fe3+0.60Fe2+0.40)∑1.00Si2.99O11O[O0.63(OH)0.37]∑1.00. Strong lines of X-ray powder-diffraction pattern of a heated sample d, Å (I; hkl) are: 3.50(46; -211), 3.22(50; -212, 201), 2.897 (100; -301), 2.850(73; 020), 2.687(73; 120), 2.121(48; -403), 1.630(59; 124). Unit-cell parameters are: a = 8.78(1) Å, b = 5.710(6) Å, c = 10.02(1) Å, b = 114.6(2)°; V = 456.7(8) Å3, Z = 2; space group P21/m. Type material is deposited in the collections of the Technische Universität, Bergakademie Freiberg, Germany; inventory numbers are 82194 and 82218. читать далее...



Pdf icon.pngStepanov V.А., Kungurova V.Е., Gvozdev V.I. Irarsite discovery in copper-nickel ores of Shanuch deposit (Kamchatka), p. 23 - 27



Pdf icon.pngPopova V.I., Kotlyarov V.A. New data on the accessory minerals of the Semeninskaya pit of the Aduy pegmatite field (Urals), p. 28 - 32



Pdf icon.pngYakovleva О.S., Pekov I.V., Bryzgalov I.А., Men’shikov Yu.P. Chalcogenide mineralization in the alumina-rich fenites of the Khibiny alkaline complex (Kola Peninsula, Russia), p. 33 - 49



Pdf icon.pngNenasheva S.N., Karpenko V.Y. Features of arsenosulvanite from the Lebedinoe deposit, Central Aldan, p. 50 - 59



Pdf icon.pngNenasheva S.N., Karpenko V.Y., Pautov L.А. Sulfide mineralization of the Lebedinoe deposit, Central Aldan, p. 60 - 65



Pdf icon.pngBorisova Е.А. Native gold from Mutnovskoe ore occurrence, South-Eastern Kamchatka, Russia, p. 66 - 71



Pdf icon.pngPopova V.I., Hiller V.V., Erokhin Y.V., Popov V.A. Monazites of the late granitic pegmatites from Ilmeny mountains: an age chemical dating of zonal and sectorial crytals, p. 72 - 78



Pdf icon.pngDoynikova O.А., Sidorenko G.А. To mineralogy of tetravalent uranium, p. 79 - 90



Pdf icon.pngMozgova N.N., Borodaev Yu.S., Stepanova Т.V., Cherkashev G.А., Uspenskaya Т.Yu. Sulfide-oxide mineral assemblages as indicator of sulfur and oxygen regime in modern submarine massive sulfide deposits, p. 91 - 100



Pdf icon.pngChernikov А.А. Mineralogical and geochemical features of the uranium ore composition: scientific and practical importance, p. 101 - 111



Crystal Chemistry, Minerals as Prototypes of New Materials, Physical and Chemical Properties of Minerals

Pdf icon.pngPekov I.V., Yapaskurt V.O., Bryzgalov I.A., Zubkova N.V. Orickite from the Khibiny alkaline complex (Kola Peninsula) and its structure features, p. 113 - 120



Mineralogical Museums and Collections

Pdf icon.pngMatvienko E.N., Sokolova E.L., Borisova E.A., Pavlova T.M. Fersman Mineralogical Museum exhibit devoted to the 125th anniversary of A.N. Labuntsov, p. 122 - 127



Personalities

Pdf icon.pngBorisova E.A., Pavlova T.M., Labuntsova M.A. To A.N. Labuntsov’s 125th anniversary: A.N. Labuntsov’s letters to academician V.I. Vernadsky (from the Archive of Russian Academy of Sciences), p. 129 - 147



Mineralogical Notes

Pdf icon.pngPopov V.A., Epanchintsev S.G. Intergrowth twins of magnetite in ores of Kurzhunkul deposit, Kazakhstan, p. 149 - 150



Pdf icon.pngSemenov Е.I. Old mistakes in determination of mineral composition, p. 151



Discussion

Pdf icon.pngBorutzky B.Ye. The essays on fundamental and genetic mineralogy: 5. Mineral species and the metastable mineralization, p. 153 - 165



Pdf icon.pngMatvienko E.N. On 90th anniversary of Ilmeny state conservation area, p. 166 - 167



Pdf icon.pngAlferova M.S., Mokhova N.A. The new approach to the scientific museums: the “museum orienteering”, p. 168