Journal/NDM42 2007 eng — различия между версиями

Версия 23:43, 12 января 2018

New Data on Minerals, vol.42, 2007

New Data on Minerals. volume 42. Мoscow: Аltum Ltd, 2007. 168 pages, 137 photos, and drawings.
Editor: Margarita I. Novgorodova, Doctor in Science, Professor.
Publication of Fersman Mineralogical Museum of Russian Academy of Science

Summary

This volume contains articles on new mineral species, among them – Faizievite, Guimarã esite, a rocherite-group mineral from Brazil, and Ferroskuterudite, arsenide of iron and cobalt from the Norilsk ore field; the description of new finds of recently discovered minerals – Pertsevite and Megacyclite with the structure of the last one; new data on mineralogical assemblages with bituminous matter in pegmatites of the Khibiny massif, on the features of occurrence of noble metals in ores and oxidized zone of the Onega deposits in South Karelia; the results of studying of Grossular, Vesuvianite and Achtrandite of the Talnakh region; the results of research of transformation of mineral paragenetic assemblages from copper sulfide ores of the Krasnov hydrotermal field; the nomenclature of the Loellingitegroup diarsenides.
The paper of the chairman and vicechairman, Subcommittee for Unnamed Minerals, IMA Commission on New Minerals, Nomenclature and Classification, published earlier in Canadian Mineralogist journal, is reproduced here in brief version by request of the Commission in order to introduce the new and approved coding system as widely as possible.
"Mineral Museums and Collections" section contains information on mineral collections of Fersman Mineralogical Museum: on art things of masters from the Urals on mineral collections of the Tsesarevichs and of General G.P. Chernik; on the story of one exhibit from the Museum – a black basalt with a golden monogram; and also there is in this section a description of the mineralogical collection of the GeoMuseum, Cologne University, Germany.
"Personalities" section includes the article on the exhibition "Jubilees and Their Heroes"; this exhibition was devoted to 290 years of Fersman Mineralogical Museum and other jubilees concerning with the Museum. Two more articles are devoted to Professors Alexander A. Godovikov and Georgiy P. Barsanov who had leaded this Museum in different periods.
In "Mineralogical Notes" section two articles are published. First, on carbonates in metakimberlite, Zarnitsa pipe, and second, on the twisted filiform magnesian calcite from rocks at Russian platform. The volume is interesting for mineralogists, geochemists, geologists, curators of Natural History museums, and collectors.

Editorial Board

Editor-in-Chief Margarita I. Novgorodova, Doctor in Science, Professor
Executive Editor Elena A. Borisova, Ph. D.
Evgeniy I. Semenov, Doctor in Science
Svetlana N. Nenasheva, Ph. D.
Elena N. Matvienko, Ph. D.
Marianna B. Chistyakova, Ph. D.

Publishing group

Photo: Michael B. Leybov
Leader of Publishing Group Michael B. Leybov
Executive Editor Ludmila A. Cheshko
Art Editor Nikolai O. Parlashkevich
Editor Alexander A. Prokubovsky
Translators Il’ya Anisimov, Maria S. Alferova,
Ivan S. Baksheev, Mark V. Fed’kin,
Boris Z. Kantor, Alexander S. Yakubchuk
Editors of Style(English) Peter Modreski, Patricia A.S. Gray, Frank C. Hawthorne
Design (idea) Dmitrii Ershov
Layout Ivan A. Glazov and Alexey A. Ludin

Authorized for printing by the Fersman Mineralogical Museum of Russian Academy of Science
Text, photos, drawings, Fersman Mineralogical Museum of Russian Academy of Science, 2007
Design AlLTUM Ltd, 2007
Published by Fersman Mineralogical Museum of Russian Academy of Science
bld. 18, korpus 2, Leninskiy Prospekt Moscow 119071 Russia
Phone: 74959520067; fax: 74959524850
email: mineral@fmm.ru; www.fmm.ru
ALTUM Ltd
Box 71
Moscow 117556 Russia
Phone/fax: +74956294812
email: minbooks@online.ru; www.minbook.com
Printed in Russia

Сontent

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

Atali A. Agakhanov, Leonid A. Pautov, Yulia A. Uvarova, Elena V. Sokolova, Frank C. Hawthorne, Vladimir Y. Karpenko, Farhod G. Gafurov. Faizievite K₂Na(Ca₆Na)Ti₄Li₆Si₂₄O₆₆F₂ – a New Mineral Species, p. 5 - 10

Faizievite, a new sodiumpotassiumcalciumlithium titanosilicate, was found in a quartz boulder in association with pectolite, baratovite, aegirine, polylithionite, leucosphenite, fluorite, etc. on a moraine of the Darai-Pioz glacier, Tadjikistan. It is colourless with a strong vitreous lustre, forms tabular plates without vicinal forms, and up to 0.3 cm in maximum dimension. Mohs hardness is 4–4.5, measured density is 2.83(2) g/cm³, calculated density is 2.819 g/cm³. Faizievite is optically positive, biaxial, n_p = 1.651(2), n_m= 1.655(2), n_g =1.657(2), 2V_meas. = -72(2)°, 2V_calc. = -70.4°. The crystal structure was refined to an R index of 7.5%. Faizievite is triclinic, space group P-1, cell dimensions: a = 9.8156(9)Å; b = 9.8249(9)Å; c = 17.3087(16)Å; a = 99.209(2)°, b = 94.670(2)°, g = 119.839(1)°, V = 1403.7(4)Å³, Z = 1. The strongest lines of the X-ray powder diffraction pattern are as follows: [d, Å, (I, %), (hkl)]: 5.60 (9) (0 0 3), 4.25 (60) (0 -2 1), 3.35 (100) (0 0 5), 3.14 (20) (1 -3 2), 3.06 (90) (-1 -2 3), 2.885 (55) (-2 1 5), 2.870 (10) (-2 3 2), 1.868 (17) (-1 4 4). The strongest lines of the IR absorption spectra are as follows: 1211, 1178, 1130, 1022, 940, 783, 683, 651, 557, 534, 460 cm¹. The chemical composition (microprobe, excepting data for Li₂O, Rb₂O, BaO, SrO – which was obtained by ICP OES, wt.%): SiO₂ – 60.65, CaO – 14.52, TiO₂ – 13.44, Nb₂O₅ – 0.11, SrO – 0.72, BaO – 0.24, K₂O – 3.93, Na₂O – 1.99, Li₂O – 3.76, Rb₂O – 0.13, F – 1.30, -O=F₂ – 0.55, total – 100.24. The empirical formula of faizievite is (K_1.98Rb_0.03)_2.01(Na_0.90□_0.10)_1.00(Ca_6.16Na_0.63Sr_0.17Ba_0.04)_7.00(Ti_4.00Nb_0.02)_4.02 Li_5.98Si₂₄O_66.00(F_1.63O_0.36)_1.99. The ideal formula is K₂Na(Ca₆Na)Ti₄Li₆Si₂₄O₆₆F₂. The name honors Faiziev Abdulkhak Radzhabovitch (born 1938) of Dushanbe, Tadjikistan, professor and membercorrespondent of the Academy of Sciences of the Republic of Tadjikistan. He is a wellknown mineralоgist, and author of numerous works on the mineralоgy and geochemistry of Central Asia. The sample with faizievite is stored in Fersman Mineralоgical Museum, Russian Academy of Science (Moscow). читать далее...

Nikita V. Chukanov, Daniel Atencio, Alexander E. Zadov, Luis A.D. Menezes Filho, Jose M.V. Coutinho. Guimarã esite, a New Zn-dominant Monoclinic Roscherite-group Mineral from Itinga, Minas Gerais, Brazil, p. 11 - 15

Guimarã esite¹, Ca₂(Zn,Mg,Fe)₅Be₄(PO₄)₆(OH)₄·6H₂O,monoclinic, is a new member of the roscheritegroup. It occurs as a late fracturefilling mineral in a phosphaterich granite pegmatite near the Piauí river, Itinga county, Minas Gerais, Brazil. Associated minerals are: albite, microcline, quartz, elbaite, lepidolite, schorl, eosphorite, moraesite, saleeite, zanazziite, an irondominant roscheritegroup mineral, opal. Guimarã esite forms peripheral zones (up to 0.1 mm thick) in crystals of roscheritegroup minerals. The inner zones of the crystals are Mgrich (and correspond to zanazziite) or Ferich (greifensteinite and/or ruifrancoite). Its colour is brown, the streak is white and the lustre is vitreous. Guimarã esite is transparent and nonfluorescent. Density (calc.) is 2.963 g/cm³. The mineral is biaxial (-), α 1.596(2), β 1.600(2), γ 1.602(2) (589 nm). 2V(obs.) 5575°, 2V(calc.) 70°. The optical X axis coincides with the elongation direction, dispersion: none observed. It is colourless under the microscope. The chemical composition is (wt. %, ranges are indicated in brackets; EDS mode electron microprobe): CaO 9.72 (9.619.79); MgO 4.00 (3.614.74); MnO 2.18 (0.893.26); FeO 2.65 (1.404.45); ZnO 19.06 (16.3320.50); Al2O3 1.70 (1.531.92); BeO (calculated) 8.975; P₂O₅ 38.20 (37.6137.78); H₂O (calculated by difference) 13.515, total 100.00. The empirical formula based on six (PO₄) groups per formula unit is Ca_1.93(Zn_2.61Mg_1.11Fe²⁺ _0.41Al_0.37Mn_0.34)_∑4.84Be_4.00(PO₄)_6.00(OH)_3.90·6.41H₂O. The strongest reflections of the powder diffraction pattern [d, Å (I, %) (hkl)] are: 9.98 (90) (110), 5.98 (100) (020), 4.82 (80) (310), 3.152 (90) (202), 3.052 (70) (421), 2.961 (70) (040, 202), 2.841 (70) (312), 2.708 (80) (041). Unit cell parameters refined from powder data are a = 15.98(1) Å, b = 11.84(2) Å, c = 6.63(1) Å, b = 95.15(15)°, V = 1249.4(34) Å3, Z = 2. The space group is C2/c. The name is for Djalma Guimarã es (18951973), in recognition of his outstanding contributions to Brazilian mineralogy and geology. Holotype specimen of guimarã esite is deposited in the Museu de Geociê ncias, Instituto de Geociê ncias, Universidade de Sã o Paulo, Brazil, registration number DR 591. читать далее...

Ernst M. Spiridonov, Yuliya D. Gritsenko. Ferroskutterudite, Nickelskutterudite, and Skutterudite from the Norilsk Ore Field, p. 16 - 27

@@ Строка 88: / Строка 88: @@
 | Авторы = Nikita V. Chukanov, Daniel Atencio, Alexander E. Zadov, Luis A.D. Menezes Filho, Jose M.V. Coutinho.
 | Название = Guimarã esite, a New Zn-dominant Monoclinic Roscherite-group Mineral from Itinga, Minas Gerais, Brazil, p. 11 - 15
-| Аннотация =
+| Аннотация = Guimarã esite<sup>1</sup>, Ca<sub>2</sub>(Zn,Mg,Fe)<sub>5</sub>Be<sub>4</sub>(PO<sub>4</sub>)<sub>6</sub>(OH)<sub>4</sub>·6H<sub>2</sub>O,monoclinic, is a new member of the roscheritegroup. It occurs as a late fracturefilling mineral in a phosphaterich granite pegmatite near the Piauí river, Itinga county, Minas Gerais, Brazil. Associated minerals are: albite, microcline, quartz, elbaite, lepidolite, schorl, eosphorite, moraesite, saleeite, zanazziite, an irondominant roscheritegroup mineral, opal. Guimarã esite forms peripheral zones (up to 0.1 mm thick) in crystals of roscheritegroup minerals. The inner zones of the
+crystals are Mgrich (and correspond to zanazziite) or Ferich (greifensteinite and/or ruifrancoite). Its colour
+is brown, the streak is white and the lustre is vitreous. Guimarã esite is transparent and nonfluorescent. Density
+(calc.) is 2.963 g/cm<sup>3</sup>. The mineral is biaxial (-), α 1.596(2), β 1.600(2), γ 1.602(2) (589 nm). 2V(obs.) 5575°,
+V(calc.) 70°. The optical X axis coincides with the elongation direction, dispersion: none observed. It is colourless under the microscope. The chemical composition is (wt. %, ranges are indicated in brackets; EDS mode electron microprobe): CaO 9.72 (9.619.79); MgO 4.00 (3.614.74); MnO 2.18 (0.893.26); FeO 2.65 (1.404.45); ZnO 19.06 (16.3320.50); Al2O3 1.70 (1.531.92); BeO (calculated) 8.975; P<sub>2</sub>O<sub>5</sub> 38.20 (37.6137.78); H<sub>2</sub>O (calculated by difference) 13.515, total 100.00. The empirical formula based on six (PO<sub>4</sub>) groups per formula unit is Ca<sub>1.93</sub>(Zn<sub>2.61</sub>Mg<sub>1.11</sub>Fe<sup>2+</sup>
+<sub>0.41</sub>Al<sub>0.37</sub>Mn<sub>0.34</sub>)<sub>∑4.84</sub>Be<sub>4.00</sub>(PO<sub>4</sub>)<sub>6.00</sub>(OH)<sub>3.90</sub>·6.41H<sub>2</sub>O. The strongest reflections of the powder diffraction pattern [d, Å (I, %) (hkl)] are: 9.98 (90) (110), 5.98 (100) (020), 4.82 (80) (310), 3.152 (90) (202), 3.052 (70) (421), 2.961 (70) (040, 202), 2.841 (70) (312), 2.708 (80) (041). Unit cell parameters refined from powder data are a = 15.98(1) Å, b = 11.84(2) Å, c = 6.63(1) Å, b = 95.15(15)°, V = 1249.4(34) Å3, Z = 2. The space group is C2/c. The name is for Djalma Guimarã es (18951973), in recognition of his outstanding contributions to
+Brazilian mineralogy and geology. Holotype specimen of guimarã esite is deposited in the Museu de Geociê ncias, Instituto de Geociê ncias, Universidade de Sã o Paulo, Brazil, registration number DR 591.
 | Файл = NDM_2007_42_Chukanov_eng.pdf
 }} {{NDM_article

Journal/NDM42 2007 eng — различия между версиями

Версия 23:43, 12 января 2018

Содержание

Summary

Editorial Board

Publishing group

Сontent

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

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

Mineralogical Museums and Collections

Personalities

Mineralogical Notes