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Journal/NDM38 2003 eng — различия между версиями
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| Авторы = Atali A. Agakhanov, Leonid A. Pautov, Dmitriy I. Belakovskiy, Elena V. Sokolova, Frank C. Hawthorne. | | Авторы = Atali A. Agakhanov, Leonid A. Pautov, Dmitriy I. Belakovskiy, Elena V. Sokolova, Frank C. Hawthorne. | ||
| − | | Название = Telyushenkoite | + | | Название = Telyushenkoite CsNa<sub>6</sub>[Be<sub>2</sub>(Si,Al,Zn)<sub>18</sub>O<sub>39</sub>F<sub>2</sub>] – a new cesium mineral of the leifite group, p. 5 - 8 |
| − | | Аннотация = | + | | Аннотация = A new mineral, telyushenkoite, was discovered in the Dara-i-Pioz alkaline massif (Tajikistan). It occurs as white |
| + | or colorless vitreous equant anhedral grains up to 2cm wide in coarsegrained boulders of reedmergnerite | ||
| + | associated with microcline, polylithionite, shibkovite and pectolite. The mineral has distinct cleavage, Mohs | ||
| + | hardness = 6, VHN<sub>100</sub> = 714(696737) kg/mm<sup>2</sup>, Dmeas. = 2.73(1), Dcalc. = 2.73g/cm<sup>3</sup>. In transmitted light, | ||
| + | telyushenkoite is colorless and transparent. It is uniaxial positive, ω = 1.526(2), ε = 1.531(2). Singlecrystal | ||
| + | X-ray study indicates trigonal symmetry, space group P3m1, a = 14.3770(8), c = 4.8786(3) Å, V = 873.2(1)Å<sup>3</sup> | ||
| + | , Z = 1. The strongest lines in the powderdiffraction pattern are [d(I,hkl)]: 12.47(7,010), 6.226(35,020), | ||
| + | 4.709(21,120), 4.149(50,030), 3.456(40,130), 3.387(75,121), 3.161(100,031), 2.456 (30,231). The chemical composition | ||
| + | (electron microprobe, BeO by colorimetry) is SiO<sub>2</sub> 64.32, Al<sub>2</sub>O<sub>3</sub> 7.26, BeO 3.53, ZnO 1.71, Na<sub>2</sub>O 13.53, | ||
| + | K<sub>2</sub>O 0.47, Cs<sub>2</sub>O 6.76, Rb2O 6.76, F 2.84, O = F 1.20, total 99.37 wt.%, corresponding to | ||
| + | (Cs<sub>0.69</sub>Na<sub>0.31</sub>K<sub>0.14</sub>Rb<sub>0.02</sub>)<sub>1.16</sub>Na<sub>6.00</sub> [Be<sub>2.04</sub>(Si<sub>15.46</sub>Al<sub>2.06</sub>Zn<sub>0.30</sub>)<sub>17.82</sub>O<sub>38.84</sub>F<sub>2.16</sub>]. Telyushenkoite, ideally CsNa<sub>6</sub>[Be<sub>2</sub> (Si<sub>15</sub>Al<sub>3</sub>)<sub>18</sub> O<sub>39</sub>F<sub>2</sub>], | ||
| + | is the Cs-dominant analogue of leifite, ideally NaNa<sub>6</sub>[Be<sub>2</sub>(Si<sub>15</sub>Al<sub>3</sub>)<sub>18</sub>O<sub>39</sub>F<sub>2</sub>]. | ||
| Файл = NDM_2003_38_Agakhanov_e.pdf | | Файл = NDM_2003_38_Agakhanov_e.pdf | ||
}}{{NDM_article | }}{{NDM_article | ||
| Строка 88: | Строка 99: | ||
Kseniya A. Rozenberg, Ramiza K. Rastsvetaeva, Giovanni Ferraris. | Kseniya A. Rozenberg, Ramiza K. Rastsvetaeva, Giovanni Ferraris. | ||
| Название = NeskevaaraiteFe, – Fe, NaK<sub>3</sub>Fe(Ti,Nb)<sub>4</sub>(Si<sub>4</sub>O<sub>12</sub>)<sub>2</sub>(O,OH)<sub>4.6</sub>H<sub>2</sub>O – a new labuntsovite group mineral, p. 9 - 14 | | Название = NeskevaaraiteFe, – Fe, NaK<sub>3</sub>Fe(Ti,Nb)<sub>4</sub>(Si<sub>4</sub>O<sub>12</sub>)<sub>2</sub>(O,OH)<sub>4.6</sub>H<sub>2</sub>O – a new labuntsovite group mineral, p. 9 - 14 | ||
| − | | Аннотация = | + | | Аннотация = Neskevaaraite-Fe, a new labuntsovitegroup mineral, was found in the Vuoriyarvi alkaline-ultramafic pluton, |
| + | Northern Karelia, within a hydrothermally altered carbonatite body. The mineral occurs as rough brown | ||
| + | translucent prismatic crystals up to 6 mm long. Associated minerals are dolomite, calcite, phlogopite, fluorapatite, | ||
| + | pyrite, pyrrhotite, chalcopyrite, serpentine, and nenadkevichite. Another occurrence is a fieldsparecalcite | ||
| + | vein located in the Kukisvumchorr Mt., Khibiny, Kola Peninsula, where the new mineral is closely | ||
| + | associated with labuntsoviteFe. | ||
| Файл = NDM_2003_38_Chukanov_e.pdf | | Файл = NDM_2003_38_Chukanov_e.pdf | ||
}}{{NDM_article | }}{{NDM_article | ||
| Авторы = Leonid A. Pautov. | | Авторы = Leonid A. Pautov. | ||
| Название = Pabstite from the Dara-i-Pioz moraine (Tadjikistan), p. 15 - 19 | | Название = Pabstite from the Dara-i-Pioz moraine (Tadjikistan), p. 15 - 19 | ||
| − | | Аннотация = | + | | Аннотация = Pabstite was discovered in the moraine of the DaraiPioz glacier (Garmsky district, Tadjikistan) in a leucocratic |
| + | rock mainly composed of microcline, quartz, and albite. Subordinated minerals are aegirine, titanite, | ||
| + | astrophyllite, bafertisite, galena, sphalerite, ilmenite, pyrochlore, fluorite, zircon, fluorapatite, and calcite. | ||
| + | Pabstite forms grains and wellfaced crystals (0.10.5 mm), growing on quartz crystals in small cavities abundant | ||
| + | in the rock. Its composition is close to the final member BaSnSi3O9 in the series pabstitebenitoite. | ||
| + | Microprobe analysis has shown: SiO<sub>2</sub> – 37.43; TiO<sub>2</sub> – 0.19; ZrO<sub>2</sub> – 0.16; SnO<sub>2</sub> – 30.05; BaO – 32.41; total | ||
| + | 100.24. The empirical formula is Ba<sub>1.02</sub>(Sn<sub>0.96</sub>Ti<sub>0.01</sub>Zr<sub>0.01</sub>)<sub>0.98</sub>Si<sub>3.01</sub>O<sub>9</sub>. Refraction parameters of pabstite are n<sub>o</sub> = | ||
| + | 1.668(2); n<sub>e</sub> = 1.657(2), which is much lower than cited figures for pabstite from the type locality. Strong | ||
| + | dependence of pabstite optical properties on titanium contents is shown. The find of pabstite at DaraiPiozе | ||
| + | is the first find of pabstite in alkaline rocks and, apparently, the second find of this mineral in the world. | ||
| Файл = NDM_2003_38_Pautov_e.pdf | | Файл = NDM_2003_38_Pautov_e.pdf | ||
}}{{NDM_article | }}{{NDM_article | ||
| Строка 121: | Строка 146: | ||
| Файл = NDM_2003_38_Novgorodova_e.pdf | | Файл = NDM_2003_38_Novgorodova_e.pdf | ||
}} | }} | ||
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====Crystal Chemistry, Minerals as Prototypes of New Materials, Physical and Chemical Properties of Minerals==== | ====Crystal Chemistry, Minerals as Prototypes of New Materials, Physical and Chemical Properties of Minerals==== | ||
{{NDM_article | {{NDM_article | ||
Версия 21:53, 25 января 2018
New Data on Minerals.Moscow.: Ocean Pictures, 2003. volume 38, 172 pages, 66 color photos.
Содержание
Summary
Articles of the volume are devoted to mineralogy, including descriptions of new mineral species (telyushenkoite – a new
caesium mineral of the leifite group, neskevaaraite-Fe – a new mineral of the labuntsovite group) and new finds of minerals
(pabstite from the moraine of the Dara-i-Pioz glacier, Tadjikistan, germanocolusite from Kipushi, Katanga, minerals
of the hilairite group from Khibiny and Lovozero massifs). Results of study of mineral associations in gold-sulfidetellyride
ore of the Kairagach deposit, Uzbekistan are presented. Features of rare germanite structure are revealed. The
cavitation model is proposed for the formation of mineral microspherulas. Problems of isomorphism in the stannite
family minerals and additivity of optical properties in minerals of the humite series are considered. The section
Mineralogical Museums and Collections includes articles devoted to the description and history of Museum collections
(article of the Kolyvan grinding factory, P.A.Kochubey's collection, new acquisitions) and the geographical location of
mineral type localities is discussed in this section. The section Mineralogical Notes includes the article about photographing
minerals and Reminiscences of the veteran research worker of the Fersman Mineralogical Museum, Doctor
in Science M.D. Dorfman about meetings with known mineralogists and geochemists – N.A. Smoltaninov, P.P.
Pilipenko, Yu.A. Bilibin.
The volume is of interest for mineralogists, geochemists, geologists, and to museum curators, collectors and amateurs
of minerals.
Editorial Board
- Editor in Chief Margarita I .Novgorodova, Doctor in Science, Professor
- Editor in Chief of the volume: Elena A.Borisova, Ph.D
- Moisei D. Dorfman, Doctor in Science
- Svetlana N. Nenasheva, Ph.D
- Marianna B. Chistyakova, Ph.D
- Elena N. Matvienko, Ph.D
- Мichael Е. Generalov, Ph.D
- N.A.Sokolova – Secretary
- Patricia A. S. Gray, English Style
- Translators: Dmitrii Belakovskii, Michael Girfanov, Boris Kantor, Il'ya Kubancev, Victor Zubarev
Publishing group
- Photo: Michael B. Leibov
- Michael R. Кalamkarov
- Boris Z. Kantor
- Natalia A. Pekova
- Leader of publishing group Michael B. Leibov
- Executive Editor Ludmila А. Cheshko (Еgorova)
- Art Director Nikolay О. Parlashkevich
- Design Dmitrii Ershov
- Layout Sophia B. Dvoskina
Library of Congress Cataloging-in-Publication Data
Novye dannye o mineralakh. English.
New data on minerals / [edited by Margarita I. Novgorodova].-- [1st American pbk. ed.].
p. cm.
At head of title: Russian Academy of Science, Fersman Mineralogical Museum.
Includes bibliographical references.
ISBN 5900395502 (pbk.)
1. Mineralogy. I. Novgorodova, M. I. (Margarita Ivanovna) II. Mineralogicheskiæi muzeæi im. A.E. Fersmana. III. Title.
QE351.N68 2003
549--dc22
2003016532
Authorized for printing by the Fersman Mineralogical Museum of the Russian Academy of Science
© Text, photo, drawings, Fersman Mineralogical Museum Russian Academy of Science, 2003
© Design, Ocean Pictures, 2003
Published by Fersman Mineralogical Museum RAS
Bld. 18/2 Leninsky Prospekt, Moscow, 117071, Russia
phone (7495) 9520067; fax (7495) 9524850
email: mineral@fmm.ru; www.fmm.ru
Ocean Pictures Ltd
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CO 80123, USA
tel/fax (303) 9042726
phone/fax (7495) 2033574
email: minbooks@online.ru; www.minbook.com
Printed in Russia
Сontent
New Minerals and Their Varieeties: New Finds of Rare Minerals, Mineral Paragenesis
Atali A. Agakhanov, Leonid A. Pautov, Dmitriy I. Belakovskiy, Elena V. Sokolova, Frank C. Hawthorne.
Telyushenkoite CsNa6[Be2(Si,Al,Zn)18O39F2] – a new cesium mineral of the leifite group, p. 5 - 8
A new mineral, telyushenkoite, was discovered in the Dara-i-Pioz alkaline massif (Tajikistan). It occurs as white or colorless vitreous equant anhedral grains up to 2cm wide in coarsegrained boulders of reedmergnerite associated with microcline, polylithionite, shibkovite and pectolite. The mineral has distinct cleavage, Mohs hardness = 6, VHN100 = 714(696737) kg/mm2, Dmeas. = 2.73(1), Dcalc. = 2.73g/cm3. In transmitted light, telyushenkoite is colorless and transparent. It is uniaxial positive, ω = 1.526(2), ε = 1.531(2). Singlecrystal X-ray study indicates trigonal symmetry, space group P3m1, a = 14.3770(8), c = 4.8786(3) Å, V = 873.2(1)Å3 , Z = 1. The strongest lines in the powderdiffraction pattern are [d(I,hkl)]: 12.47(7,010), 6.226(35,020), 4.709(21,120), 4.149(50,030), 3.456(40,130), 3.387(75,121), 3.161(100,031), 2.456 (30,231). The chemical composition (electron microprobe, BeO by colorimetry) is SiO2 64.32, Al2O3 7.26, BeO 3.53, ZnO 1.71, Na2O 13.53, K2O 0.47, Cs2O 6.76, Rb2O 6.76, F 2.84, O = F 1.20, total 99.37 wt.%, corresponding to (Cs0.69Na0.31K0.14Rb0.02)1.16Na6.00 [Be2.04(Si15.46Al2.06Zn0.30)17.82O38.84F2.16]. Telyushenkoite, ideally CsNa6[Be2 (Si15Al3)18 O39F2], is the Cs-dominant analogue of leifite, ideally NaNa6[Be2(Si15Al3)18O39F2]. читать далее...
Nikita V. Chukanov, Viktor.V. Subbotin, Igor V. Pekov, Aleksandr E. Zadov, Anatoliy I. Tsepin,
Kseniya A. Rozenberg, Ramiza K. Rastsvetaeva, Giovanni Ferraris.
NeskevaaraiteFe, – Fe, NaK3Fe(Ti,Nb)4(Si4O12)2(O,OH)4.6H2O – a new labuntsovite group mineral, p. 9 - 14
Neskevaaraite-Fe, a new labuntsovitegroup mineral, was found in the Vuoriyarvi alkaline-ultramafic pluton, Northern Karelia, within a hydrothermally altered carbonatite body. The mineral occurs as rough brown translucent prismatic crystals up to 6 mm long. Associated minerals are dolomite, calcite, phlogopite, fluorapatite, pyrite, pyrrhotite, chalcopyrite, serpentine, and nenadkevichite. Another occurrence is a fieldsparecalcite vein located in the Kukisvumchorr Mt., Khibiny, Kola Peninsula, where the new mineral is closely associated with labuntsoviteFe. читать далее...
Leonid A. Pautov.
Pabstite from the Dara-i-Pioz moraine (Tadjikistan), p. 15 - 19
Pabstite was discovered in the moraine of the DaraiPioz glacier (Garmsky district, Tadjikistan) in a leucocratic rock mainly composed of microcline, quartz, and albite. Subordinated minerals are aegirine, titanite, astrophyllite, bafertisite, galena, sphalerite, ilmenite, pyrochlore, fluorite, zircon, fluorapatite, and calcite. Pabstite forms grains and wellfaced crystals (0.10.5 mm), growing on quartz crystals in small cavities abundant in the rock. Its composition is close to the final member BaSnSi3O9 in the series pabstitebenitoite. Microprobe analysis has shown: SiO2 – 37.43; TiO2 – 0.19; ZrO2 – 0.16; SnO2 – 30.05; BaO – 32.41; total 100.24. The empirical formula is Ba1.02(Sn0.96Ti0.01Zr0.01)0.98Si3.01O9. Refraction parameters of pabstite are no = 1.668(2); ne = 1.657(2), which is much lower than cited figures for pabstite from the type locality. Strong dependence of pabstite optical properties on titanium contents is shown. The find of pabstite at DaraiPiozе is the first find of pabstite in alkaline rocks and, apparently, the second find of this mineral in the world. читать далее...
Igor V. Pekov, Nikita V. Chukanov, Natalia N. Kononkova, Dmitirii Yu. Pushcharovsky.
Raremetal «zeolites» of the hilairite group, p. 20 - 33
Svetlana N. Nenasheva.
On the Chemical Composition of Germanite, p. 34 - 40
Svetlana N. Nenasheva, Leonid A. Pautov.
On Germanocolusite from Kipushi (Katanga), p. 41 - 44
Vladimir A. Kovalenker, Olga Yu. Plotinskaya, Rustam I. Koneev.
Mineralogy of Epithermal Gold-Sulfide-Telluride Ores of the Kairagach Gold Deposit, (Uzbekistan), p. 45 - 56
Margarita I. Novgorodova, Stepan N. Andreev, Alexander A. Samokhin.
Cavitation model of mineral microspherula formation in hydrothermal ores, p. 57 - 63
Crystal Chemistry, Minerals as Prototypes of New Materials, Physical and Chemical Properties of Minerals
Tat'yana L. Evstigneeva, Vyacheslav S. Rusakov, Yurii K. Kabalov.
Isomorphism in the minerals of stannite-family, p. 65 - 69
Boris B. Shkursky.
Additive models of optical
properties in minerals of humite polysomatic series, p. 70 - 79
Mineralogical Museums and Collections
Marianna B. Chistyakova, Nina R. Budanova. Articles of Kolyvan grinding factory in the
Fersman Mineralogical museum of the Russian Academy of Science, p. 81 - 88
Marina L. Moisseeva. Petr A.
Kochubei and His Mineral Collection in A.E. Fersman Mineralogical Museum, p. 89 - 98
Mikhail E. Generalov.
Ten Taels More to the Fund of the Museum, p. 99 - 100
Dmitriy I. Belakovskiy.
New acquisitions of the Fersman Mineralogical Museum Russian Academy of Sciences (1997–2001), p. 101 - 112
Alexander A. Evseev.
Geographical Location of Mineral Type Localities, p. 113 - 124
Leo V. Bulgak.
Archive of the Mineralogical Museum: replensishment of collection in 1909–1914., p. 125 - 128
Tat'yana M. Pavlova.
The role of A.E. Fersman in the Mineralogical museum
of the Russian Academy of Science, p. 129 - 134
Vyacheslav D.Dusmatov. A.E.
Fersman's contribution to the systenatic collection of the mineralogical museum of the Russian Academy of Sciences, p. 135 - 141
Mineralogical Notes
Boris Z. Kantor.
Photographing Minerals, p. 143 - 146
Moisei D. Dorfman.
Reminiscences, p. 147 - 151
Book reviews, p. 152
