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Journal/NDM42 2007 eng — различия между версиями
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| Строка 132: | Строка 132: | ||
| Авторы = Andrey A. Chernikov, Viktor T. Dubinchuk, Dmitriy O. Ozhogin, Natalia I. Chistyakova. | | Авторы = Andrey A. Chernikov, Viktor T. Dubinchuk, Dmitriy O. Ozhogin, Natalia I. Chistyakova. | ||
| Название = Features of Occurrence and Distribution of Noble Metals in Ores and Oxidized Zone of the Onega Uranium-Vanadium Deposits, South Karelia, p. 43 - 49 | | Название = Features of Occurrence and Distribution of Noble Metals in Ores and Oxidized Zone of the Onega Uranium-Vanadium Deposits, South Karelia, p. 43 - 49 | ||
| − | | Аннотация = | + | | Аннотация = Complex uraniumvanadium ores with Mo, Cu, Bi and Pb from the Onega deposits, which contain large reserves |
| + | of vanadium and probably noble metals (Pd, Au, Ag, Pt), are limited by nearsurface and deepseated bedded oxidized | ||
| + | zones. In addition, deep joint oxidized zone and hydrothermal roscoelite–chromceladonite–dolomite | ||
| + | veinlets occur at the deposits. The highest contents (much higher than 10 ppm) of noble metals have been identified | ||
| + | in these veinlets. Minerals of noble metals are native gold, selenides, less frequent selenidesulfides, tellurides, | ||
| + | and compounds with bismuth, lead, and other elements. Redeposited native copper, auricupride, native platinum, | ||
| + | froodite, isoferoplatinum, palladium analogue of auricupride, the new natural phase, and the phase AuO(OH) have | ||
| + | been identified in the oxidized zones with the highest contents of noble metals. Gold segregations from the | ||
| + | nearsurface oxidized zone of low noblemetal content (lower than 10 ppm) are fine clusters up to 0.1 µm in size. | ||
| + | In the upper part of the deepseated oxidized zone, gold occurs as broken spindleshaped 23 µm particles. Close | ||
| + | to the intermediate part of the deepseated oxidized zone, gold crystals are disseminated in blades of native copper | ||
| + | that reach several tens of µm in size.<br> | ||
| + | The results obtained confirm previous assumption on the probable increase in noblemetal reserves adjacent to | ||
| + | explored uraniumvanadium deposits. | ||
| Файл = NDM_2007_42_Chernikov_eng.pdf | | Файл = NDM_2007_42_Chernikov_eng.pdf | ||
}} {{NDM_article | }} {{NDM_article | ||
| Авторы = Mariya S. Alferova. | | Авторы = Mariya S. Alferova. | ||
| Название = Grossular, Vesuvianite and Achtarandite Mineralogy of the Talnakh Region, p. 50 - 61 | | Название = Grossular, Vesuvianite and Achtarandite Mineralogy of the Talnakh Region, p. 50 - 61 | ||
| − | | Аннотация = | + | | Аннотация = Achtarandite, the pseudomorph after unknown mineral is a minerlogical enigma. The second locality of |
| + | achtarandite described in Talnakh region, Otdel'naya mountain, by its mineral assocaition is an analogue of | ||
| + | the typelocality in Yakutia republic, Wiluy river valley. The comprehensive investigation was applied to the | ||
| + | rockforming minerals – grossular, vesuvianite and achtarandite, and also to the mineral and fluid inclusions | ||
| + | enclosed.<br> | ||
| + | The experimental modelling of Cl-containing mayenite – the achtarandite proto-mineral synthesis was carried | ||
| + | out.<br> | ||
| + | It is established that the specific mineral association containing achtarandite happened during two stages: | ||
| + | skarn and aposkarn. During the first stage there were formed central parts of garnet and vesuvianite crystals, | ||
| + | fassaite which remained as inclusions in vesuvianite, and Cl-containing mayenite. During the second stage | ||
| + | there were formed edges of garnet and vesuvianite crystals, amesite, titanite, mackinawite, and Cl-containing | ||
| + | mayenite was replaced by achtarandite. | ||
| Файл =NDM_2007_42_Alferova_eng.pdf | | Файл =NDM_2007_42_Alferova_eng.pdf | ||
}} {{NDM_article | }} {{NDM_article | ||
| Авторы = Nadezhda N. Mozgova, Yury S. Borodaev, Irina F. Gablina, Tamara V. Stepanova, Georgiy A. Chekashev, Tatyana Yu. Uspenskaya. | | Авторы = Nadezhda N. Mozgova, Yury S. Borodaev, Irina F. Gablina, Tamara V. Stepanova, Georgiy A. Chekashev, Tatyana Yu. Uspenskaya. | ||
| Название = Features of Transformation of Mineral Paragenetic Assemblages from Copper Sulfide Ores of the Krasnov Hydrothermal field (16°38’ N Mid-Atlantic Ridge), p. 62 - 76 | | Название = Features of Transformation of Mineral Paragenetic Assemblages from Copper Sulfide Ores of the Krasnov Hydrothermal field (16°38’ N Mid-Atlantic Ridge), p. 62 - 76 | ||
| − | | Аннотация = | + | | Аннотация = Copper sulfide ores of the 5–80 thousands age from the Krasnov relic hydrothermal field (16°38', Mid-Atlantic |
| + | Ridge) have been studied with optical microscope, electron microscope equipped with energy dispersion system | ||
| + | (SEM-EDS), electron microprobe, and X-ray diffraction.<br> | ||
| + | According to the mineralogy, three types of paragenetic assemblages are recognized. Type I is homogeneous | ||
| + | isocubanite with Cu-rich sulfides (bornite and copper sulfides of the chalcocite-digenite series). Type II is exsolved | ||
| + | isocubanite and its unique products of subsequent transformation. Type III is oxide-sulfate-sulfide, which is characterized | ||
| + | by iron specialization and is divided into two subtypes: with predominant pyrite (IIIa) and with predominant | ||
| + | Fe-Cu sulfates and Fe oxides (IIIb). Type III contains relics of the highly modified type II paragenesis. The | ||
| + | age relationship of type I has not been established. | ||
| Файл = NDM_2007_42_Mozgova_eng.pdf | | Файл = NDM_2007_42_Mozgova_eng.pdf | ||
}} {{NDM_article | }} {{NDM_article | ||
| Авторы = Dorian G.W. Smith and Ernest H. Nickel. | | Авторы = Dorian G.W. Smith and Ernest H. Nickel. | ||
| Название = Codification of Unnamed Minerals, p. 77 - 79 | | Название = Codification of Unnamed Minerals, p. 77 - 79 | ||
| − | | Аннотация = | + | | Аннотация = The Subcommittee for Unnamed Minerals of the IMA Commission on New Minerals, Nomenclature and |
| + | Classification (CNMNC, formerly CNMMN) has developed a codification system that includes the year of publication | ||
| + | and qualitative chemical composition for unnamed minerals reported in the literature. Such minerals are | ||
| + | divided into two categories: Those regarded as being "valid as unnamed minerals" are those that do not correspond | ||
| + | to existing species, have not been reported previously, and whose published descriptions enable them to be recognized | ||
| + | if found elsewhere. Unnamed minerals regarded as being "invalid as unnamed minerals" are those whose | ||
| + | published descriptions are inadequate for their confident recognition if found elsewhere, or which correspond to | ||
| + | existing mineral species or unnamed minerals published previously. | ||
| Файл = NDM_2007_42_Smith_eng.pdf | | Файл = NDM_2007_42_Smith_eng.pdf | ||
}} | }} | ||
Версия 00:14, 13 января 2018
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
Содержание
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, np = 1.651(2), nm= 1.655(2), ng =1.657(2), 2Vmeas. = -72(2)°, 2Vcalc. = -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 (K1.98Rb0.03)2.01(Na0.90□0.10)1.00(Ca6.16Na0.63Sr0.17Ba0.04)7.00(Ti4.00Nb0.02)4.02 Li5.98Si24O66.00(F1.63O0.36)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 Ca1.93(Zn2.61Mg1.11Fe2+ 0.41Al0.37Mn0.34)∑4.84Be4.00(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, β = 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
CoNiFe triarsenides skutterudite, nickelskutterudite and ferroskutterudite have been identified in the Norilsk ore field for the first time. They are hosted in the apophyllite–anhydrite–dolomite–calcite metamorphic hydrothermal veins that occur within the proximal zone of the magmatic CoNiCu sulfide ores, which have been affected by epigenetic prehnitepumpellyite and zeolite facies metamorphism. The CoNiFe triarsenides have overgrown the CoNi diarsenide segregations with which they form complex intergrowths. Both skutterudite and nickelskutterudite, and skutterudite and ferroskuterudite, from Norilsk form continuous isomorphic series. Clear negative correlation between Ni and Fe and strong positive correlation between Co and Fe and Co and S have been identified. читать далее...
Werner Schreyer, Heintz-Jurgen Bernhardt, Olaf Medenbach, Vladimir V. Rudnev, Nikolay N. Pertsev.
The New Finds of Pertsevite, p. 28 - 32
A revision of samples and thin sections collections of kotoitebearing rocks by optics and Electron Micro Probe methods has permited to find two new occurrences of pertsevite Mg2(B,Si)(O,F,OH)4. In comparison with the pertsevite holotype having a rather broad meaning of B/Si the new founds of the mineral are more homogeneous in XSi 0.12–0.20 in the sample from Titovskoye deposit, East Verkhoyansk region, and 0.24–0.32 from Gonochan deposit (Djugdjur Ridge, near Okhotsk Sea Coast). The last has the predominance of hydroxile over fluorine. The compositions of accompanied minerals – kotoite, ludwigite and humite group minerals have been studied and presented as well. Pertsevite was formed after kotoite and clinohumite with their reciprocal replacement owing to their chemical interaction. читать далее...
Vera N. Ermolaeva, Nikita V. Chukanov, Igor V. Pekov, Zoya V. Shlyukova.
New Data on Mineral Assemblages with Bituminous Matter in Pegmatites of the Khibiny Massif, p. 33 - 42
The new occurrences of solid bituminous substances (SBS) have been found in peralkline pegmatites of the Khibiny massif, Kola Peninsula, Russia. Mineral assemblages containing rounded and droplike segregations of SBS ranging from 1 to 10 mm in size are described. In most cases, SBS are ingrown into the grains of microporous titanium, niobium, and zirconium silicates and locally overgrow their surface. Microinclusions of Th and REE minerals frequently occur within the SBS segregations. The new findings confirm a hypothesis of catalytic role of the zeolitelike titanium, niobium, and zirconium silicates to form SBS, as well as key role of organic matters to transfer and concentrate Th and REE during hydrothermal stage of the pegmatite formation. At final stage, most thorium and part of REE incorporate into mineral phases, which saturate SBS, whereas Ca (occasionally together with part of Th and REE) remains in organic phase as carboxylate salts and/or organometallic compounds. читать далее...
Andrey A. Chernikov, Viktor T. Dubinchuk, Dmitriy O. Ozhogin, Natalia I. Chistyakova.
Features of Occurrence and Distribution of Noble Metals in Ores and Oxidized Zone of the Onega Uranium-Vanadium Deposits, South Karelia, p. 43 - 49
Complex uraniumvanadium ores with Mo, Cu, Bi and Pb from the Onega deposits, which contain large reserves
of vanadium and probably noble metals (Pd, Au, Ag, Pt), are limited by nearsurface and deepseated bedded oxidized
zones. In addition, deep joint oxidized zone and hydrothermal roscoelite–chromceladonite–dolomite
veinlets occur at the deposits. The highest contents (much higher than 10 ppm) of noble metals have been identified
in these veinlets. Minerals of noble metals are native gold, selenides, less frequent selenidesulfides, tellurides,
and compounds with bismuth, lead, and other elements. Redeposited native copper, auricupride, native platinum,
froodite, isoferoplatinum, palladium analogue of auricupride, the new natural phase, and the phase AuO(OH) have
been identified in the oxidized zones with the highest contents of noble metals. Gold segregations from the
nearsurface oxidized zone of low noblemetal content (lower than 10 ppm) are fine clusters up to 0.1 µm in size.
In the upper part of the deepseated oxidized zone, gold occurs as broken spindleshaped 23 µm particles. Close
to the intermediate part of the deepseated oxidized zone, gold crystals are disseminated in blades of native copper
that reach several tens of µm in size.
The results obtained confirm previous assumption on the probable increase in noblemetal reserves adjacent to
explored uraniumvanadium deposits. читать далее...
Mariya S. Alferova.
Grossular, Vesuvianite and Achtarandite Mineralogy of the Talnakh Region, p. 50 - 61
Achtarandite, the pseudomorph after unknown mineral is a minerlogical enigma. The second locality of
achtarandite described in Talnakh region, Otdel'naya mountain, by its mineral assocaition is an analogue of
the typelocality in Yakutia republic, Wiluy river valley. The comprehensive investigation was applied to the
rockforming minerals – grossular, vesuvianite and achtarandite, and also to the mineral and fluid inclusions
enclosed.
The experimental modelling of Cl-containing mayenite – the achtarandite proto-mineral synthesis was carried
out.
It is established that the specific mineral association containing achtarandite happened during two stages:
skarn and aposkarn. During the first stage there were formed central parts of garnet and vesuvianite crystals,
fassaite which remained as inclusions in vesuvianite, and Cl-containing mayenite. During the second stage
there were formed edges of garnet and vesuvianite crystals, amesite, titanite, mackinawite, and Cl-containing
mayenite was replaced by achtarandite. читать далее...
Nadezhda N. Mozgova, Yury S. Borodaev, Irina F. Gablina, Tamara V. Stepanova, Georgiy A. Chekashev, Tatyana Yu. Uspenskaya.
Features of Transformation of Mineral Paragenetic Assemblages from Copper Sulfide Ores of the Krasnov Hydrothermal field (16°38’ N Mid-Atlantic Ridge), p. 62 - 76
Copper sulfide ores of the 5–80 thousands age from the Krasnov relic hydrothermal field (16°38', Mid-Atlantic
Ridge) have been studied with optical microscope, electron microscope equipped with energy dispersion system
(SEM-EDS), electron microprobe, and X-ray diffraction.
According to the mineralogy, three types of paragenetic assemblages are recognized. Type I is homogeneous
isocubanite with Cu-rich sulfides (bornite and copper sulfides of the chalcocite-digenite series). Type II is exsolved
isocubanite and its unique products of subsequent transformation. Type III is oxide-sulfate-sulfide, which is characterized
by iron specialization and is divided into two subtypes: with predominant pyrite (IIIa) and with predominant
Fe-Cu sulfates and Fe oxides (IIIb). Type III contains relics of the highly modified type II paragenesis. The
age relationship of type I has not been established. читать далее...
Dorian G.W. Smith and Ernest H. Nickel.
Codification of Unnamed Minerals, p. 77 - 79
The Subcommittee for Unnamed Minerals of the IMA Commission on New Minerals, Nomenclature and Classification (CNMNC, formerly CNMMN) has developed a codification system that includes the year of publication and qualitative chemical composition for unnamed minerals reported in the literature. Such minerals are divided into two categories: Those regarded as being "valid as unnamed minerals" are those that do not correspond to existing species, have not been reported previously, and whose published descriptions enable them to be recognized if found elsewhere. Unnamed minerals regarded as being "invalid as unnamed minerals" are those whose published descriptions are inadequate for their confident recognition if found elsewhere, or which correspond to existing mineral species or unnamed minerals published previously. читать далее...
Crystal Chemistry, Minerals as Prototypes of New Materials, Physical and Chemical Properties of Minerals
Nataliya V. Zubkova, Igor V. Pekov, Nikita V. Chukanov, Dmitriy V. Lisitsin, Murtasali Kh. Rabadanov,
Dmitriy Yu. Pushcharovsky.
New Data on Megacyclite, p. 81 - 92
Raisa A. Vinogradova.
On Composition and Nomenclature of the Loellingite-group Diarsenides, p. 93 - 95
Mineralogical Museums and Collections
Marianna B. Chistyakova.
Stone-cutting in the Urals. Articles of masters from Ekaterinburg in
the Fersman Mineralogical Museum Russian Academy of Sciences, p. 97 - 113
Elena A. Borisova, Rolf Hollerbach.
The Mineralogical Collection of the GeoMuseum, Cologne University, Germany, p. 114 - 119
Nina A. Mohova, Mikhail E. Generalov.
General and His Collection. The Mineral Collection of G.P. Chernik at the Fersman Mineralogical Museum, RAS, p. 120 - 128
Marianna B. Chistyakova.
A Monogram on Basalt, p. 129 - 131
Mikhail E. Generalov.
Is this a Regal Engagement? On the Mineral Collection of The Throne Crown Prince, p. 132 - 137
Personalities
Elena A. Borisova, Tatyana M. Pavlova.
2006–2007: Jubilees and Their Heroes, p. 139 - 145
Svetlana N. Nenasheva.
Alexander Alexandrovich Godovikov. Life and Activity, p. 146 - 153
Professor Georgii Pavlovich Barsanov and V.I. Vernadsky and A.E. Fersman Mineralogical-Geochemical School, p. 154 - 156
Mineralogical Notes
Elena L. Sokolova, Ernst M. Spiridonov.
Ca-bearing Strontianite, Barite, Dolomite, and Calcite from Metakimberlite, Zarnitsa pipe, Yakutia, p. 158 - 162
Tamara T. Abramova, Leili L. Panas'yan, Mikhail S. Chernov, Vyacheslav N. Sokolov, Vladimir M. Ladygin, Olga I. Gusarova, Ernst M. Spiridonov.
Twisted Filiform Magnesian Calcite from Carbonate Rocks at Russian Platform, p. 163 - 167
'Fersmaniada–2008': Competition for the best scientific work by the young geologists and mineralogists,
within the International conference 'Fersmanovskie chteniya', p. 168
