Минералогический Музей им. А.Е. Ферсмана
Москва, Ленинский проспект 18 корпус 2,
тел. (495) 954-39-00
  • Intro banner1.jpg
  • Intro banner2.jpg
  • Intro banner3.jpg
  • Intro banner1a.jpg
  • Intro banner2a.jpg
  • Intro banner3a.jpg
  • Intro banner4.jpg
  • Intro banner5.jpg
  • Intro banner6.jpg
  • Intro banner2b.jpg
  • Intro banner3b.jpg
  • Intro banner7.jpg
  • Intro banner8.jpg
  • Intro banner9.jpg
  • Intro banner10.jpg
  • Intro banner11.jpg

Journal/2019 engl — различия между версиями

(Editorial Board)
Строка 1: Строка 1:
 
[[Файл:2019engl.jpg|thumb|350px|right|New Data on Minerals, Volume 53, 2019]]
 
[[Файл:2019engl.jpg|thumb|350px|right|New Data on Minerals, Volume 53, 2019]]
'''New Data on Minerals. Volume 53, 2019,''' 160 pages, 166 photos, drawings, and schemes. <br>
+
'''New Data on Minerals. Volume 53, 2019'''<br>
 
__TOC__
 
__TOC__
 
<div class="mw-collapsible mw-collapsed">
 
<div class="mw-collapsible mw-collapsed">
 
=====Summary=====
 
=====Summary=====
 
<div class="mw-collapsible-content">
 
<div class="mw-collapsible-content">
 
+
The periodical journal New Data on Minerals has been published since 1907. The Fersman Mineralogical Museum of Russian Academy of Sciences is its founder. In the last two issues, the Russian mining company ALROSA is the general partner.
 +
In the 53rd issue, an attempt was made to renew the historically established tradition of publishing in the journal a summary of the scientific achievements of the employees of the RAS Ministry of Museum. For 2017-2018 Scientific knowledge in the fields of mineralogy and crystallography was significantly expanded, and a significant contribution was made to understanding the processes of mineral formation. The pages of the journal show results on the properties and genesis of minerals and the characteristics of their paragenesis in various, often unique deposits and ore occurrences in Russia and other regions of the world. The current results of a mineralogical study of the Arkhangelsk diamondiferous province, Pamir pegmatites, fumaroles of the Tolbachinsky valley and coal fire sublimates of Ravat, rare-earth mineralization of the Mochalin Log, thallium mineralization of the Vorontsov deposit and finds of Kirkite at the Berezovsky gold ore deposit in the Urals are presented. Brief descriptions of 31 new mineral species are given. The authors presented the results of a study of olivine from magnesian skarns of the Baikal region and the extremely igneous extreme magnesian olivine (Fo> 96) and olivine containing up to 0.48 wt.% P2O5. In olivine of magnesian skarns, a substantial titanium content was first recorded.<br>
 +
The issue presents a series of materials on general approaches and specific methodological developments for presenting the information that mineralogical collections carry. Here, questions of the scientific and general culture of the importance of minerals are highlighted, which allows the reader to look at mineralogical samples as works of art, and compare the expertise of such exhibits with art history, removing it from the plane of a purely scientific and utilitarian assessment.<br>
 +
In addition to scientific and museum articles, you can find a bibliographic sketch about the oldest employee of the Ministry of Museum of the Russian Academy of Sciences M. B. Chistyakova, author of the book “Stone-cutting products in the collection of the Mineralogical Museum named after A.E. Fersman ”, which contains the first detailed description of this unique collection. The reader will find a fascinating story about the Italian instrumental master Antonio Cetti and his mineralogical collection, which later became part of the museum fund. A brief historical review is given on the creation and development of a periodical of the Mineralogical Museum named after A.E. Fersman of the Russian Academy of Sciences from its origins back in 1907 to the present day.<br>
 
This journal is of interest for mineralogists, geochemists, geologists, staff of natural history museums, collectors, and rocks aficionados.
 
This journal is of interest for mineralogists, geochemists, geologists, staff of natural history museums, collectors, and rocks aficionados.
 
</div>
 
</div>
 
</div>
 
</div>
 +
 
<div class="mw-collapsible mw-collapsed">
 
<div class="mw-collapsible mw-collapsed">
 
 
===== Editorial Board =====
 
===== Editorial Board =====
 
<div class="mw-collapsible-content">
 
<div class="mw-collapsible-content">
 
+
'''Editor in Chief'''<br>
'''Editor in Chief:''' P.Yu. Plechov - Doctor of Geology and Mineralogy, Professor <br>
+
P.Yu. Plechov - Doctor of Geology and Mineralogy, Professor <br>
 
'''Members of Editorial Board:'''<br>
 
'''Members of Editorial Board:'''<br>
 
I.V. Pekov - Corresponding Member of the Russian Academy of Sciences, Doctor of Geology and Mineralogy<br>
 
I.V. Pekov - Corresponding Member of the Russian Academy of Sciences, Doctor of Geology and Mineralogy<br>
Строка 26: Строка 29:
 
L.A. Pautov - Senior Researcher <br>
 
L.A. Pautov - Senior Researcher <br>
 
<br>
 
<br>
 
+
'''Editor, Design, Layout'''<br>
E.V.Kronrod -  PhD in Chemistry<br>
+
E.V. Kronrod - PhD in Chemistry<br>
</div>
 
</div>
 
<div class="mw-collapsible mw-collapsed">
 
 
 
=====Publishing group=====
 
<div class="mw-collapsible-content">
 
 
 
'''Photo''' - M.B. Leybov<br>
 
'''Leader of Publishing group''' - M.B. Leybov<br>
 
'''Managing Editor''' - L.A. Cheshko<br>
 
'''Design''' - D. Ershov<br>
 
'''Layout''' - I.A. Eyes<br><br>
 
You can order the current issue or subscribe to the magazine at www.minbook.com or by email minbooks@online.ru
 
 
</div>
 
</div>
 
</div>
 
</div>
  
 
===Сontent===
 
===Сontent===
 +
==== '''Issue 1''' ====
 
{{NDM_article
 
{{NDM_article
| Авторы = Plechov P.Yu.  
+
| Авторы = Pekov I.V.  
| Название = From the editors.
+
| Название = In development of some issues of museum science in the field of mineralogy. I. On the specifics of mineralogical collections, pp. 1-5
| Аннотация = The 51st issue of the Magazine "New Data on Minerals" is a special. It is dedicated to the 300th anniversary of the Fersman Mineralogical Museum of RAS. Therefore, we expanded the section devoted to the collections and history of the Museum, and placed a brief report on the scientific conference held at the Presidium of the RAS and the Minmuseum in November 2016 and dedicated to the 300th anniversary of the Fersman Mineralogical Museum of the RAS.
+
| Аннотация = The article is devoted to the individual characteristics of mineralogical collections that distinguish them from the collections of other objects of inanimate nature. These features are important for understanding and evaluating the general cultural significance of the mineralogical collections and individual exhibits in them. A wide intraspecific diversity, often often most pronounced precisely in visually defined characteristics, important in the museum-collection aspect, is a striking feature of a large number of minerals. In many cases, when evaluating mineralogical samples, the decisive role is played by their “unmeasured” characteristics, perceived “through feelings”, primarily compositional characteristics. This brings together exhibits of mineralogical collections, which are valued, inter alia, for aesthetic merits, with piece-wise, "non-serial" works of art, and determines, in particular, the need to take into account the "artistic" aspect in assessing the significance of an exhibit of a mineralogical collection, and brings together the expertise of such exhibits from art history, deducing it is from the plane of a purely scientific and utilitarian assessment.<br>
 +
'''Keywords:''' mineralogical museum; mineralogical collection; natural science collection; mineralogical sample.''
 
| Файл =  
 
| Файл =  
 
}} {{NDM_article
 
}} {{NDM_article
| Авторы = Gliko A.O.
+
| Авторы = Pekov I.V.  
| Название = 300 years of the Fersman Mineralogical Museum of Russian Academy of Sciences. Greetings to the 300th anniversary of the museum from the academician-secretary of the Department of Earth Sciences of Russian Academy of Sciences.
+
| Название = In development of some issues of museum science in the field of mineralogy. II. On Different Aspects of the Importance of a Mineralogical Sample, pp. 6-15
| Аннотация = The Department of Earth Sciences of Russian Academy of Sciences wholeheartedly congratulates with the 300th anniversary! We must remember the main stages of the history of the Museum. In 1716, in the Kunstkamera founded by Peter the Great, the Mineralogical Cabinet was created. It became the part of the Geological Museum of the Russian Academy of Sciences.
+
| Аннотация = The article is devoted to various aspects of the scientific and general cultural significance of the mineral sample, primarily as an exhibit of the mineralogical collection. Various characteristics of the mineralogical specimen are discussed, objective (museum-collection quality, rarity, unusual) and subjective (degree of knowledge, historical value, etc.), criteria for their evaluation and corresponding assessment systems, as well as approaches and specific methodological techniques that can be use in museum work when characterizing the significance of a mineralogical sample and to highlight outstanding exhibits of mineralogical collections. Special attention is paid to the duality of the concept of “rarity of a mineral” and the appropriateness of its definition in the museum business through the total number of authentically diagnosed samples of this mineral present in the collections.<br>
 +
'''Keywords:''' Mineralogical Museum; mineralogical collection; mineralogical sample; mineralogical sample quality; the degree of knowledge of the mineralogical sample; the rarity of the mineral.
 
| Файл =  
 
| Файл =  
 
}}
 
}}
  
====New minerals and their varieties, new finds of rare minerals, mineral paragenesis====
 
 
{{NDM_article
 
{{NDM_article
| Авторы = Begizov V.D., Zavyalov E.N.  
+
| Авторы = Pekov I.V.  
| Название = Ferodsit (Fe, Rh, Ir, Ni, Cu, Pt, Co) 9-xS8 is a new mineral from the Nizhny Tagil ultrabasic massif
+
| Название = In development of some issues of museum science in the field of mineralogy. III. On the concept of "mineral discovery" in the broad sense and its characteristics, pp. 16-22
| Аннотация = Ferodsite was found in bedrock of the Nizhny Tagil ultrabasic massif (Urals) and in the Conder placer (Khabarovsk Territory). The new mineral is in intergrowth and association with Pt-Fe minerals, chendeite and platinum sulfides. The mineral is black with a bronze hue, metallic luster, perfect cleavage according to (111). Grain sizes are mainly 10–50 μm, splices up to 100 μm. In reflected light, light, brownish-gray, slight birefringence. The chemical composition corresponds to the formula (Fe, Rh, Ni, Ir, Cu, Pt) 9xS8, where x varies from 0 to 1. Syngony is tetragonal, a = 10.009 (5) Å, c = 9.840 (8) Å, V = 985.78 ( 9) Å3, Z = 4. A sample with ferodsite is stored in the Mineralogical Museum named after A.E. Fersman RAS. The article has 3 tables, 1 figure, a list of references from one name. Key words: ferodsite, platinum minerals, Nizhny Tagil ultrabasic massif, Conder.  
+
| Аннотация = The article is devoted to the concept of "finding a mineral" in the broad sense, which is defined as the entire set of samples of this mineral found (collected) at a given mineralogical object (location of the mineral). The issues related to the indicator of museum-collection quality of mineral finds are discussed in most detail, criteria for its evaluation in application to various minerals and corresponding evaluation systems are proposed. <br>
 +
'''Keywords:''' Mineralogical Museum; mineralogical collection; geographic information in mineralogy; mineral discovery.  
 
| Файл =  
 
| Файл =  
 
}}{{NDM_article
 
}}{{NDM_article
| Авторы = Ermolaeva V.N., Chukanov N.V., Yanchev S., Van K.V.
+
| Авторы = Borisova E.A.
| Название = Endogenous paragenesis of non-sulfide minerals of chalcophilic elements in the orogenic zone of the “Mixed Series” of the Pelagonian Massif, Macedonia
+
| Название = Book of MB Chistyakova “Stone-cutting products in the collection of the Fersman Mineralogical Museum of RAS", pp. 23-26
| Аннотация = New data on the specific metasomatic association of oxide minerals containing chalcophilic elements from metasomatic rocks of the orogenic zone of the “Mixed Series” metamorphic complex located in the Pelagonian massif, Macedonia are obtained. Based on the ratios of the mineral phases, the following order of the sequence of formation of minerals is revealed:
+
| Аннотация = In 2019, a monograph by Marianna Borisovna Chistyakova was published, dedicated to the description of the collection of ornamental and precious stones of the Mineralogical Museum named after A.E. Fersman of the Russian Academy of Sciences. On February 6, 2019, there was a presentation of this publication, published with the help of the Gokhran of Russia and sponsor E.E. Bogomolov.<br>
zincochromite + zircon + Zn-containing talcum powder + barite-> franklinite + heterolith-> ganite -> romeite + almeidaite -> Fe3 + analogue of zincheggombite -> ferricoronadite + Mn-analog of plumboferrite. In the process of metasomatic conversion under highly oxidizing conditions, the sequential addition of Zn, Al, Sb, and Pb led to the formation of zinc spinelids (including ganite, replacing franklinite and heterolith), the Sb-containing iron analog of zincheggombite (epitaxy on zinc spinelides), and ferricoronadal (late hydrotherm streaks). The introduction of As occurred in 2 stages.
+
'''Keywords:''' collection of ornamental and precious stones, stone-cutting products, Mineralogical Museum, A.E. Fersman.
 
| Файл =  
 
| Файл =  
 
}} {{NDM_article
 
}} {{NDM_article
| Авторы = Karpenko V.Yu., Pautov L.A., Agakhanov A.A.
+
| Авторы = Generalov M.E.
| Название = About Ni-Zn-containing folbortite (“Uzbekite”) from vanadium schists of South Kyrgyzstan
+
| Название = In the wake of the Danish Italian. Collection Antonio Cetti (Antonio Cetti) in the Mineralogical Museum. A.E. Fersman, pp. 27-34
| Аннотация = The results of the re-study of "Uzbekite" - water copper vanadate, described for the first time in Kara-Chagyr, Kyrgyzstan, based on materials from the funds of the Fersman Mineralogical Museum of RAS (Moscow) and authors` fees. “Uzbekit” from Kara-Chagyr was identified as folbortite with high contents of zinc and nickel (wt.%): ZnO up to 5.2 (average ~ 1.0–2.5); NiO up to 2.4 (average ~ 0.5–2.0). Elevated Zn and Ni contents were also found in folwortite at the U-deposit Kara-Tangi, Kyrgyzstan. Microprobe analyzes of folbortite from Kyrgyzstan and from the Karatau ridge, Kazakhstan, and water content for some samples are presented. Crystals of various morphology are described: lamellar, skeletal, forming sagenite type lattices, and unusual needle ones. Powder patterns for lamellar and needle crystals are given; their cell parameters, respectively: a = 10.620 (2), b = 5.893 (2), c = 7.213 (2) Å; b = 94.96 (2) °; V = 449.7 (4) Å3, Z = 2 and a = 10.616 (2), b = 5.899 (2), c = 7.212 (2) Å; b = 94.96 (2) °; V = 450.0 (4) Å ^ 3, Z = 2. It was shown that “Uzbekite” from other locations is either folbortite (Potekhino, Khakassia, Russia), or it is mixed with other minerals (case-like crystals of tangeite filled with a mixture of vesigneite and folbortite from Agalyk, Uzbekistan). An assumption was made of the existence of phases close to folbortite, but different in structure.
+
| Аннотация = New data are published about Antonio Cetti and his mineralogical collection, acquired for the Kunstkamera in 1806 and later merged into the collection of the Mineralogical Museum named after A.E. Fersman. The information obtained helped to clarify the possible period of its formation, to connect samples to this collection for which authorship was not indicated or inaccurate in the documents of the museum.<br>
 +
'''Keywords:''' history of the mineralogical collection, collector of natural science collections, Antonio Chetti, Kunstkamera, Mineralogical Museum, A.E. Fersman.
 +
| Файл =
 +
}}
 +
 
 +
==== '''Issue 2''' ====
 +
{{NDM_article
 +
| Авторы = Plechov P.Yu., Pekov I.V., Belakovsky D.I., Pautov L.A., Kasatkin A.V., Agakhanov A.A., Moiseev M.M., Karpenko V.Yu., Nekrylov N .A., Gritsenko Yu.D., Garanin V.K.
 +
| Название = Diversity of minerals and their paragenesis: scientific results of the Ferman Mineralogical Museum of RAS in 2018, pp. 36-57
 +
| Аннотация = The article is a summary of the main scientific results of the employees of the Fersman Mineralogical Museum of RAS (MinMuseum RAS) for 2018. Brief descriptions of 31 new mineral species are given: horseradish, rhabdoborite- (V), rhabdoborite- (W), manaevite- (Ce), paraberceliitis, whitework, zubkovit, achirofanit, aleutite, elasmochloite, canauerite, udinite, arsenudinite, akoperite, akoperit, (La), Radekškodaite- (La), Glaskovite, ferrierite, Dalnegorskite, red matte, Antophagastite, Pliniusite, Jarjemskyite, Alekskhomyakovite, Milanriderite, Kruenite, Falgarite, Badakhshanite- (Y), Nataliya-Kulikit, Avdey Perdeit.<br>
 +
The current results of the mineralogical study of the Arkhangelsk diamondiferous province, the Pamir pegmatites, the fumaroles of the Tolbachinsky dol and coal fire sublimates of Ravat, the rare-earth mineralization of the Mochalin Log and the thallium mineralization of the Vorontsov deposit in the Urals are summarized.<br>
 +
The results of studying olivine of magnesian skarn and rare finds for igneous rocks of extreme magnesian olivine (Fo> 96) and olivine containing up to 0.48 wt.% P2O5 are presented. In olivine of magnesian skarns, a substantial titanium content was first recorded. The data on the composition of chromium spinelide inclusions in olivine from the volcanic rocks of Kamchatka are summarized.<br>
 +
'''Keywords:''' MinMuseum RAS, report on scientific work for 2018, 31 new minerals, new data on the mineralogy of natural objects, variations in the composition of rock-forming minerals.
 
| Файл =  
 
| Файл =  
}} {{NDM_article
+
}}
| Авторы = Tishchenko A.I., Kasatkin A.V., Skoda R.
+
==== '''Issue 3''' ====
| Название = Silicides (nagchuit, lingzhiit, lobusait and collet) in the Sarmatian limestones of Crimea
+
{{NDM_article
| Аннотация = Nagchuit, lingzhiit, lobusaite and collet were found in a powdery, insoluble in HCl diluted residue of a dark gray color from organogenic clastic limestone of the Evpatoria deposit (Crimea). Among the silicide grains, nagchuit and lingzhiite predominate; lobusaite is found in subordinate quantities. Nagchuit and lingzhiit often grow together, forming grains up to 120 microns in size. Lobusaite is observed in the form of individual rare grains up to 100 microns in size. Tsangpoit was found in three grains up to 15 microns in size in close intergrowth with lingzhiit. Single grains of native silicon, presumably panguitite and unnamed Ti and W silicide, were also noted. The chemical composition (wt.%, Microprobe) of nagchuita (average of 9 anal.): Al 0.11, Ti 0.01, V 0.09, Cr 0.15, Mn 0.54, Fe 63.25 , Co 0.35, Ni 0.61, Cu 0.10, Zn 0.17, Zr 0.26, Si 33.63, sum 99.27, corresponds to the empirical formula (calculation for 2 atoms) Fe0.96Mn0.01Co0.01Ni0.01Si1.01; lingzhiita (average of 8 ann.): Al 1.83, V 0.03, Cr 0.09, Mn 0.23, Fe 46.54, Co 0.23, Ni 0.04, Zr 0.18, Si 49.94, sum 99.11, corresponds to the empirical formula (calculation for 3 atoms) Fe0. 93Al0.08Si1.99; lobusaite (average of 4 ann.): Al 1.20, V 0.06, Cr 0.15, Mn 0.11, Fe 42.60, Ni 0.10, Zr 0.73, Si 54.71, sum 99.66, corresponds to the empirical formula (calculation for 2 Si atoms) Fe0.78Al0. 05Zr0.01Si2.00; collet (average of 3 ann.): Mg 0.06, Al 1.05, Ca 0.12, Sc 0.05, Ti 24.58, V 0.36, Cr 0.43, Mn 0.36, Fe 31.49, Co 0.18, Ni 0.44, Cu 0.22, Zn 0.03, Zr 3.50 , Nb 0.58, Mo 0.55, Cd 0.12, In 0.11, Sn 0.09, Cs 0.21, W1.97, Si 32.70, sum 99.20, corresponds to the empirical formula (calculation for 4 atoms) Ti0.86Zr0.07W0.02V0.01Nb0.01Mo0. 01Fe0.94Ca0.01Cr0.01Mn0.01Co0.01Ni0.01Cu0.01Si1.95Al0.07. Diagnostics of nagchuit, lingzhiit and lobusaite is confirmed by x-ray; for other minerals, due to their rarity and small size, X-ray characteristics were not obtained. Lobusaite and zangpoite were the first in Russia, and they were first found in the Crimea and Linguiite.
+
| Авторы = Sandalov F.D., Koshlyakova N.N., Pekov I.V., Yapaskurt V.O., Khanin D.A., Sidorov E.G.
| Файл =
+
| Название = Cassiterite from fumarole exhalations of the Tolbachik volcano (Kamchatka): chemical composition and morphogenetic features, pp. 60-70
}} {{NDM_article
+
| Аннотация = In the present work, cassiterite of fumarole genesis was first characterized. It was found in the deposits of the active fumarole Arsenatnaya (Second slag cone of the Northern breakthrough of the Great Fissure Tolbachinsky eruption 1975–76, Tolbachinsky dol, Tolbachik volcanic massif, Kamchatka), where it is closely associated with “salt” minerals - sylvin, halite - and alkaline sulfates of the group aphthalitis, as well as with anhydrous arsenates of Ca, Mg, Na, Fe and Cu. Cassiterite here is represented by “fluffy” soft radial-radiant aggregates of fine-needle to hairy crystals in the cavities, which is a consequence of rapid crystallization from the gas phase. It also forms a sagenite lattice on hematite, which was recorded for cassiterite for the first time.<br>
| Авторы = Krinov D.I., Saltykov A.S., Dymkov Yu.M., Azarova Yu.V., Koltsov V.Yu.
+
'''Keywords:''' cassiterite, tin in hematite, isomorphism, exhalation mineral formation, fumarole, Tolbachik volcano, Kamchatka.
| Название = On calcium uranium titanosilicate and its significance for the technological processing of uranium ores
 
| Аннотация = When studying samples from various uranium deposits of Aldan (Elkonsky gold-uranium ore cluster) and the Novokonstantinovskoye deposit (Ukraine), a mineral was discovered with the composition: UO2 »58–62%; CaO 5-7%; TiO2 »18–22%; SiO2 »10–11%, which can be described by the idealized formula Ca (U, Ca) 3Ti3 [SiO4] 2 (O, OH) 8 (calculated for 16 oxygen atoms). It was established in breccias with carbonate cement of various compositions developed in quartz-feldspar metasomatites in the form of microgranular clusters and clusters of prismatic crystals (10–50 μm) in breccia cement. Sometimes it performs cracks in veins of glandular dolomite in polyphase breccias. Energy dispersive spectra showed the absence of superposition of the lines of the studied phase and associated minerals. The chemical composition was determined using a CamScan electron scanning microscope with a Link spectrometer and AN10000 analyzer. The results obtained allow us to consider this mineral as a potentially new mineral species, conventionally called "calcium uranium titanosilicate." The mineral was formed in association with glandular dolomite, siderite and / or ankerite. Probably, his education preceded brannerite. The mineral fraction in the uranium component of ores is 20–80%, that is, “calcium uranium titanosilicate” is one of the main ore minerals in the considered objects. The prevalence of it and other calcium-containing ore minerals in the studied ores, as well as the presence of a carbonate component in them, makes it necessary to modernize the methods for extracting useful components from them. The use of circulating volumes of solutions, the absence of the need for additional enrichment and other measures will positively affect the economic and environmental performance of production.  
 
 
| Файл =
 
| Файл =
 
}}{{NDM_article
 
}}{{NDM_article
| Авторы = Nenasheva S.N., Agakhanov A.A.
+
| Авторы =  Pekov I.V.
| Название = New data on minerals of the Shishim mine, Shishim mountains, Southern Urals, Russia
+
| Название = In development of some issues of museum science in the field of mineralogy. IV. On extraordinary mineralogical objects and their significance, pp. 71-79
| Аннотация = The new minerals were found in skarne samples from the Shishimsky mine (South Ural): thaumasite Ca3 (SO4) [Si (OH) 6] (CO3) · 12H2O, described in the Urals only in the Nikolai-Maximiliansky mine; CaO lime, known at the Gumeshevsky deposit and in the burnt dumps of the Chelyabinsk coal basin; ferroacermanite Ca2Fe [Si2O7], not previously encountered in nature, but known as a synthetic product. In addition, new mineral phases were discovered: the AMg10 phase [(Si6.6Al3.4) 10O28] · 8.6H2O and the phase X with the empirical formula (Ca1.98V0.02) 2.00 (OH) 0.86 (PO4) 0.86 (Si2O7) 0.07 ( SO4) 0.14Cl0.03. Ferroacermanite is a ferruginous analogue of ackermanite Ca2Mg [Si2O7], a mineral of the melilite group. Earlier, minerals of this group were not found in the Urals. The listed minerals and mineral phases new for the Shishimsky mine are in close intergrowth with each other and with calcite, monticellite, forsterite, diopside, chondrodite, perovskite, cordierite, magnesioferrite and other minerals already known on this mine.
+
| Аннотация = The article is devoted to questions of the importance of mineralogical objects - the locations of minerals - in the scientific, museum-collection and environmental aspects. Extraordinary mineralogical objects are discussed, their importance scientifically and generally culturally, criteria for classifying a mineralogical object as extraordinary, the principles of ranking them by significance and a classification scheme proposed for this, taking into account, among other things, the nature of the mineralogical material originating from this object.<br>
 +
'''Keywords:''' mineralogical museum, mineralogical collection, mineralogical object, location of minerals, geographical information in mineralogy, natural monument.
 
| Файл =  
 
| Файл =  
 
}}{{NDM_article
 
}}{{NDM_article
| Авторы = Slukin A.D., Boeva ​​N.M., Zhegallo E.A., Zaitseva L.V.
+
| Авторы = Kasatkin A.V., Skoda R.
| Название = Laterite bauxite biominerals - new data from electron microscopic studies
+
| Название = Find of Kirkyite at the Berezovsky gold ore deposit (Middle Urals), pp. 80-85
| Аннотация =  A systematic study of lateritic bauxite using electron microscopes revealed abundant products of the interaction of organic matter (biota) and minerals. New data were obtained on the mineralization in tropical conditions of algal deposits, wood, the root system of vegetation, biofilms and bacteria and their subsequent transformation into biomorphoses, perfect crystals of goethite, hematite, gibbsite, calcite and bizarre forms of psilomelan. Unique photographs demonstrate the ground products of the digestive tract of digging and crawling organisms and the single prismatic Gibbsite crystals formed from them, and then their mass development. It has been established that monomineral gibbsite is crystallized in the passages and burrows of worms in bauxites. In the free spaces of large pores and caverns on the surface of biofilms, similar products turn into a mixture of gibbsite, hematite, calcite, in some places, halloysite and psilomelan. Undoubtedly, the composition of mineral associations is affected by microlocal conditions and the influx of calcium, silicon, and other chemical elements with capillary waters during dry seasons. Biomineralization products are microscopic in size, but they have universal and global significance for all weathering crusts (especially tropical ones) and the associated sedimentary deposits of bauxite, iron and manganese ores, kaolin and bentonite.
+
| Аннотация =  A rare lead sulfovismuthite-sulfoarsenite Kirkyite Pb10Bi3As3S19 was installed by us in a sample from the Berezovsky gold ore deposit (Sverdlovsk region, Middle Urals), stored in the systematic collection of the Mineralogical Museum named after AE Fersman RAS under the number 71444. The mineral forms inclusions up to 50 microns in size in kozalite. The empirical formula of the Kirkite Pb9.92 (Bi2.91Sb0.18) is Σ3.09As2.97S19.01. The parameters of the monoclinic unit cell are: a = 8.582 (18), b = 26.12 (4), c = 8.80 (2) Å, β = 119.8 (2) °, V = 1711 (6) ų. Kirkiit was found for the first time in the Russian Federation.<br>
 +
'''Keywords:''' kirkiit, kozalit, Berezovskoye gold deposit, Middle Urals, the first mineral discovery in Russia.
 
| Файл =  
 
| Файл =  
 
}}{{NDM_article
 
}}{{NDM_article
| Авторы = Putintseva E.V., Spiridonov E.M.
+
| Авторы = Nenasheva S.N., Borisova E.A., Pavlova T.M.
| Название = The oldest diamondiferous kimberlites and metakimberlites of Kimozer, Karelia in Russia
+
| Название = The article is dedicated to the oldest employee of the Mineralogical Museum named after A.E. Fersman, Marianna Borisovna Chistyakova (1929–2015), who worked at the museum for more than 60 years and was the custodian of funds and expositions of the collection of precious and ornamental stones.<br>
| Аннотация =  The history of the formation of the mineral composition of the oldest in Russia kimberlites Kimoser, Karelia is considered. Kimberlites broke through gabbro-dolerites and schungite-bearing sedimentary rocks of the Ludovic (Paleoproterozoic) and contain their xenoliths. All these rocks are tectonized and similarly metamorphosed. The kimberlite minerals are described - phlogopite, chrome spinelides, ilmenite group (heikilite, picroilmenite, Mn ilmenite, pyrophanite), titanomagnetite, apatite, zircon, baddeleyite. The evolution of the composition of chrome spinels and minerals of the ilmenite group is considered, their common feature is the enrichment of Mn. It can be assumed that Kimozero kimberlites arose with the participation of carbonatite melts of high alkalinity. The xenolith metagabbro-dolerites in kimberlites compose albite, clinocoisite, epidote, chlorites, actinolite, prenite, pumpelli (Fe), titanite, quartz, Al kronstedtite, hematite, Mn-Mg ferroaxinite, lennylene peite; these are formations of the prenite-pumpellite facies. The metamorphosed kimberlites of Kimoser are the petrotype of metakimberlites of the prenite-pumpellite facies (PPF). Serpentines (antigorite, relict lysardite), tremolite, actinolite, calcite, dolomite, clinochlorine, magnetite, titanite, corrensite, talcum, apatite, rutile, hematite, ferropepsybrucite, allanite- (Ce), hydroxylbastnose are described - (La), hydroxylparisite- (Ce), hydroxylparisit- (La), bastnesite- (Ce), parisit- (Ce), monazite- (Ce), niobeshinite- (Ce), apatite, zircon, baddeleyite, pentlandite, pyrrhotite , polydimite, zygenite, thorite, bixbyite, relict and late millerite. There are no strontium minerals. Minerals REE metakimberlites - allanite, bastnesite, parisite, monazite, niobeshinite inherited Ce, Ce-La and Ce-La-Nd specificity of magmatic calcite, perovskite and apatite. The boundaries of the crystals of minerals REE and titanite, antigorite, tremolite –inductive surfaces of joint growth. The most common allanite is (Ce). Specificity of metamorphogenic allanite: its crystals are non-zonal, significant variability of REE contents and Fe3 + / Fe2 + ratios in crystals spaced apart by a few tens of microns from each other, compositional diversity: some crystals are selectively Ce, others are rich in La, and in the third, Nd> La. Allanite in clinochlor aggregates is poor in Ti, Cr, and V; in intergrowths with titanite, it contains 1–2 wt.% TiO2, and in contact with ferrichromite, it contains up to 9 wt.% Cr2O3. Most of Kimozer's allanite belongs to the allanite – ferriallanite series (up to 30% of the ferriallanite minal), the smaller part to the allanite – chromallanite series. In subsequent metamorphism processes, allanite was replaced by hydroxylbastnesite and hydroxylparisite or monazite. Germination of bastnesitis and parisitis are common. Monazite (Ce) is extremely poor in Y, P and Th, poor in Nd and enriched in La, usually developed in antigorite metakimberlites. Kimozero metakimberlites contain irregularly shaped non-zircon zircon and baddeleyite up to “diffuse”. These minerals lack Nb, Th, Y, Ti. Metamorphogenic zircon is poor in hafnium and contains 0.5–0.7 wt.% HfO2. A new genetic type is distinguished - metamorphogenic-hydrothermal REE and Zr mineralization in metakimberlites of PPF. The Sm-Nd dating of metakimberlites from the prenite-pumpellite facies reflects the time of their metamorphism, and not the time of kimberlite introduction.  
+
'''Keywords:''' Fersman Mineralogical Museum of RAS, a collection of ornamental and precious stones, a museum exposition, stone-cutting products, MB Chistyakova.
 
| Файл =  
 
| Файл =  
 
}}
 
}}
  
====Mineralogical museums and collections====
+
==== '''Issue4''' ====
 
{{NDM_article
 
{{NDM_article
| Авторы = Garanin V.K., Borisova E.A., Mokhova N.A.
+
| Авторы =Pautov L.A., Mirakov M.A., Makhmadsharif S., Karpenko V.Yu., Fayziev A.R.  
| Название = To the 300th anniversary of the Fersman Mineralogical Museum of Russian Academy of Sciences: Collection History
+
| Название = Finding of native tellurium in sublimates of a natural underground fire in the tract Kukhi-Malik at the Fan-Yagnob coal deposit (Tajikistan), pp. 95-99
| Аннотация =  The history of the mineralogical collection of the museum, now bearing the name of the outstanding mineralogist and geochemist Academician A.E. Fersman, dates back to the beginning of the XVIII century, when in 1716 under the Kunstkamera Peter I the Mineral Cabinet was created. Now it is one of the largest collections of minerals in the world, with more than 140,000 samples in the main fund. Museum exhibitions showcase around 15,000 exhibits. Among them are more than 3,700 mineral species, samples from private collections that have entered the museum over its 300-year history, unique stone-carving products of the imperial lapidary factories and the famous company Carl Faberge. The paper briefly describes the history of collections and provides some information about their authors.  
+
| Аннотация =  The discovery of native tellurium in sublimates of high-temperature fumaroles in a natural underground coal fire in the tract Kukhi-Malik near the village of Rawat in the Fan-Yagnob coal deposit in the Sogd region of Tajikistan is described. Tellurium is represented by well-formed prismatic crystals (0.1 mm), on which the faces m {10¯10}, ¯e {01¯12}, r {10¯11} are most developed, and a number of unidentified forms are less common with {0001}. In association with tellurium are Fe and K sulfates, Tl and K sulfate, and anglesite. Tellurium crystals are zonal; the central part is enriched in selenium (up to 10 wt.%). The physical properties and main reflections of the X-ray powder diffraction pattern are presented. <br>
 +
'''Keywords:''' native tellurium, selenium-containing tellurium, an isomorphic series of selenium - tellurium, minerals of sublimates, fumaroles, coal fire, Tajikistan, Fan-Yagnob deposit, Ravat, Kuhi-Malik.
 
| Файл =
 
| Файл =
 
}}{{NDM_article
 
}}{{NDM_article
| Авторы =Sveshnikova O.L., Gritsenko Yu.D., Pautov L.A., Spiridonov E.M.  
+
| Авторы =Borisova E.A., Plechov P.Yu.  
| Название = Mineralogical Museum named after Alexander Evgenievich Fersman: 300 years of searches and achievements
+
| Название =To the 110th anniversary of the periodical publication of the Mineralogical Museum named after A.E. Fersman Russian Academy of Sciences, pp. 100-113
| Аннотация = The history of the Mineralogical Museum of the Russian Academy of Sciences is the history of the formation and development of mineralogy in Russia. From the first years of its existence, the most important task of the Museum, along with the replenishment of collections, was their scientific study. The three hundred year history of the Museum is closely connected with the names of many prominent scientists of its time. The article considers the contribution of most of them to the development of the Museum and mineralogy. The role of academicians V.I. Vernadsky and A.E. Fersman, whose activities contributed to the transformation of the Museum into a center of mineralogical research of a high scientific level. In modern conditions, the Museum has the status of a research institute of the Russian Academy of Sciences, while remaining one of the largest mineral storages in the world (more than 150,000 exhibits).  
+
| Аннотация = In 2017, 110 years have passed since the publication of the first issue of the periodical of the museum, now bearing the name of Academician A.E. Fersman. The article gives a brief overview of the issues of the journal for the first decade of its existence (the period from 1907 to 1917–1918).<br>
 +
'''Keywords:''' Fersman Mineralogical Museum of RAS, New Data on Minerals, History of the Mineralogical Journal.  
 
| Файл =  
 
| Файл =  
 
}}{{NDM_article
 
}}{{NDM_article
| Авторы =Generalov M.E.
+
| Авторы =Mirakov M.A., Pautov L.A., Karpenko V.Yu., Fayziev A.R., Makhmadsharif S
| Название = Wagner and his motives
+
| Название = Pauflerit β-VO (SO4) in the sublimates of a natural underground fire in the tract Kuhi-Malik (Rawat) at Fan- Yagnob coal deposit, Tajikistan, pp. 114-121
| Аннотация =  A search for data on Wagner, the author of the collection acquired by the Kunstkamera in 1806, allowed him to be identified with the pharmacist Johann (Jan) Wagner, a native of the Saxon family, who transferred to Russian citizenship in 1811, the ancestor of the dynasty that gave Russia a number of famous people. An analysis of the Wagner collection shows that his main interest was ore deposits located in territories belonging to the Habsburg monarchy.
+
| Аннотация =  A description of the finding of β-VO (SO4) pauflerite in the sublimates of high-temperature gas emissions from a natural coal fire in the Kukhi-Malik tract near the village of Ravat, Fan-Yagnob coal deposit, Tajikistan, in brecciated siltstones. Pauflerite crystals are elongated-prismatic, measuring 40–100 microns; simple forms: b {010}, m {101} (most developed), e 110}, p {111}, δ {212}. Doubles are observed in (010) (?). The mineral is transparent, green, fragile. Glitter glass. Powflerite is optically biaxial, 2V close to 90º. The dispersion of the optical axes is very weak, v> r. The plane of the optical axes is perpendicular to the elongation of the crystals; np = 1.733 (2), nm = 1.778 (3), ng calc. = 1.823 (4). Pleochroism: by Ng - green color, by Nm and Np - light green. Absorption scheme Ng> Nm> Np. Composition (cf. 3 ann., Electron probe data, wt.%): VO2 49.87, SO3 50.01, amount 99.88. The empirical formula is V0.97O (S1.02O4). The parameters of the rhombic unit cell (Ǻ): a = 7.392 (3), b = 6.272 (2), c = 7.064 (3). For the first time, a powder x-ray and drawings of powderedite crystals are shown. According to the presence of the mineral phases V, Cd, Mo, Tl, Bi, Sn, In, Sb, Se, Te, As, the sublimates of a coal fire at the Fan-Yagnobskoye deposit are close to the sublimates of the volcanic fumaroles of Kamchatka, Kuril, Italy, due to the common extraction mechanisms the gases of these elements from the host rocks, their transfer and deposition in the unloading zones.<br>
| Файл =
+
'''Keywords:''' pauflerite, vanadium, vanadil, sulfate, minerals of sublimates, fumaroles, coal fire, Tajikistan, Fan-Yagnob deposit, Ravat, Kuhi-Malik.
}}{{NDM_article
 
| Авторы =Sveshnikova O.L.
 
| Название = The exhibition "Minerals of crystal-bearing quartz veins" in the Mineralogical Museum named after A.E. Fersman Russian Academy of Sciences
 
| Аннотация =  The exhibition, created in the museum in 2016 and called “Minerals of crystal-bearing quartz veins”, is built mainly on the material from crystal-bearing deposits of the Subpolar Urals. In this region, 2 types of crystal-bearing veins are currently distinguished. One, known as alpine veins, refers to lateral secretions, the other is hydrothermally metamorphic in nature. The cavities in both types of veins are made of almost the same complex of minerals, consisting almost exclusively of lithophilic elements. The main cavity mineral is quartz; among the minerals associated with it, adularia, albite, carbonates, and titanium-containing minerals are most common: rutile, brookite, anatase, ilmenite, titanite; boron minerals: tourmaline and axinite; epidote, chlorite, etc. All these minerals, represented, as a rule, by perfectly formed crystals, are on display at the exhibition. Particular attention is paid to the ontogeny of quartz crystals. The exhibition shows crystals of various habit, varying degrees of shape distortion, possessing some particular macrostructure (or anatomy). Examples of the importance of studying the ontogeny of minerals for solving genetic problems are given.
 
 
| Файл =
 
| Файл =
}}
 
 
====Mineralogical notes====
 
{{NDM_article
 
| Авторы =Generalov M.E.
 
| Название = Saint from the collection of crystals
 
| Аннотация =  An analysis of the pattern on a quartz sample with actinolite inclusions from the collection of the Mineralogical Museum of the Russian Academy of Sciences suggests that it depicts St. Jerome Stridonsky revered in Western Christianity and suggests that this subject is historically connected with the period when the Netherlands attempted to colonize Brazil (mid XVII century).
 
| Файл =
 
}}
 
 
====Persons====
 
{{NDM_article
 
| Авторы =Dokuchaev A.Ya., Krekhan G.-R., Kargin A.V., Kurdyukov E.B., Leksin A.B., Lobanov K.V., Smolyaninova V.N., Sukhanov M.K., Yutkina E.V.
 
| Название = Outstanding Arctic Explorer E.V. Toll in documents and materials of the Ore and Petrographic Museum (IGEM RAS, Moscow)
 
| Аннотация = Letters of the outstanding Russian polar explorer Eduard Vasilievich Toll, the scientific keeper of the Mineralogical Museum of the Imperial Academy of Sciences (1887–1896) and the head of the Russian Polar Expedition (RPE) 1900–1902 were published for the first time. (Novosibirsk islands). The letters are addressed to Uncle Academician General Fedor Bogdanovich (Friedrich Karl) Schmidt, the director of this museum, who was directly responsible for organizing the RPE. The letters provide details of the expedition’s preparations, starting in 1885. Historical information is provided to more fully understand their contents.
 
| Файл =
 
}}{{NDM_article
 
| Авторы =Criulina G.Yu., Garanin V.K., Borisova E.A.
 
| Название = International scientific conference dedicated to the 300th anniversary of the Mineralogical Museum named after A.E. Fersman Russian Academy of Sciences, November 21–24, 2016, Moscow
 
| Аннотация = International conference dedicated to the 300th anniversary of the Mineralogical Museum named after A.E. Fersman, was held from November 21 to November 24, 2016 in the building of the Russian Academy of Sciences on the square. Yu.A. Gagarina and in the conference hall of the museum. Guests and participants of the conference were more than 200 people: outstanding academicians, professors and other mineral scientists from Russia and abroad, graduate students, students, mineral lovers, philanthropists, businessmen. In total, over 40 oral presentations and 20 posters were presented.
 
| Файл =
 
 
}}
 
}}

Версия 14:48, 3 июня 2020

New Data on Minerals, Volume 53, 2019

New Data on Minerals. Volume 53, 2019

Summary

The periodical journal New Data on Minerals has been published since 1907. The Fersman Mineralogical Museum of Russian Academy of Sciences is its founder. In the last two issues, the Russian mining company ALROSA is the general partner. In the 53rd issue, an attempt was made to renew the historically established tradition of publishing in the journal a summary of the scientific achievements of the employees of the RAS Ministry of Museum. For 2017-2018 Scientific knowledge in the fields of mineralogy and crystallography was significantly expanded, and a significant contribution was made to understanding the processes of mineral formation. The pages of the journal show results on the properties and genesis of minerals and the characteristics of their paragenesis in various, often unique deposits and ore occurrences in Russia and other regions of the world. The current results of a mineralogical study of the Arkhangelsk diamondiferous province, Pamir pegmatites, fumaroles of the Tolbachinsky valley and coal fire sublimates of Ravat, rare-earth mineralization of the Mochalin Log, thallium mineralization of the Vorontsov deposit and finds of Kirkite at the Berezovsky gold ore deposit in the Urals are presented. Brief descriptions of 31 new mineral species are given. The authors presented the results of a study of olivine from magnesian skarns of the Baikal region and the extremely igneous extreme magnesian olivine (Fo> 96) and olivine containing up to 0.48 wt.% P2O5. In olivine of magnesian skarns, a substantial titanium content was first recorded.
The issue presents a series of materials on general approaches and specific methodological developments for presenting the information that mineralogical collections carry. Here, questions of the scientific and general culture of the importance of minerals are highlighted, which allows the reader to look at mineralogical samples as works of art, and compare the expertise of such exhibits with art history, removing it from the plane of a purely scientific and utilitarian assessment.
In addition to scientific and museum articles, you can find a bibliographic sketch about the oldest employee of the Ministry of Museum of the Russian Academy of Sciences M. B. Chistyakova, author of the book “Stone-cutting products in the collection of the Mineralogical Museum named after A.E. Fersman ”, which contains the first detailed description of this unique collection. The reader will find a fascinating story about the Italian instrumental master Antonio Cetti and his mineralogical collection, which later became part of the museum fund. A brief historical review is given on the creation and development of a periodical of the Mineralogical Museum named after A.E. Fersman of the Russian Academy of Sciences from its origins back in 1907 to the present day.
This journal is of interest for mineralogists, geochemists, geologists, staff of natural history museums, collectors, and rocks aficionados.

Editorial Board

Editor in Chief
P.Yu. Plechov - Doctor of Geology and Mineralogy, Professor
Members of Editorial Board:
I.V. Pekov - Corresponding Member of the Russian Academy of Sciences, Doctor of Geology and Mineralogy
V.K. Garanin - Doctor of Geology and Mineralogy, Professor
M.I. Novgorodova - Doctor of Geology and Mineralogy, Professor
B.E. Borutsky - Doctor of Geology and Mineralogy
B.E Spiridonov - Doctor of Geology and Mineralogy
S.N. Nenasheva - PhD in Geology and Mineralogy
E.N. Matvienko - PhD in Geology and Mineralogy
M.E. Generalov - PhD in Geology and Mineralogy
L.A. Pautov - Senior Researcher

Editor, Design, Layout
E.V. Kronrod - PhD in Chemistry

Сontent

Issue 1

Pekov I.V. In development of some issues of museum science in the field of mineralogy. I. On the specifics of mineralogical collections, pp. 1-5

The article is devoted to the individual characteristics of mineralogical collections that distinguish them from the collections of other objects of inanimate nature. These features are important for understanding and evaluating the general cultural significance of the mineralogical collections and individual exhibits in them. A wide intraspecific diversity, often often most pronounced precisely in visually defined characteristics, important in the museum-collection aspect, is a striking feature of a large number of minerals. In many cases, when evaluating mineralogical samples, the decisive role is played by their “unmeasured” characteristics, perceived “through feelings”, primarily compositional characteristics. This brings together exhibits of mineralogical collections, which are valued, inter alia, for aesthetic merits, with piece-wise, "non-serial" works of art, and determines, in particular, the need to take into account the "artistic" aspect in assessing the significance of an exhibit of a mineralogical collection, and brings together the expertise of such exhibits from art history, deducing it is from the plane of a purely scientific and utilitarian assessment.
Keywords: mineralogical museum; mineralogical collection; natural science collection; mineralogical sample.



Pekov I.V. In development of some issues of museum science in the field of mineralogy. II. On Different Aspects of the Importance of a Mineralogical Sample, pp. 6-15

The article is devoted to various aspects of the scientific and general cultural significance of the mineral sample, primarily as an exhibit of the mineralogical collection. Various characteristics of the mineralogical specimen are discussed, objective (museum-collection quality, rarity, unusual) and subjective (degree of knowledge, historical value, etc.), criteria for their evaluation and corresponding assessment systems, as well as approaches and specific methodological techniques that can be use in museum work when characterizing the significance of a mineralogical sample and to highlight outstanding exhibits of mineralogical collections. Special attention is paid to the duality of the concept of “rarity of a mineral” and the appropriateness of its definition in the museum business through the total number of authentically diagnosed samples of this mineral present in the collections.
Keywords: Mineralogical Museum; mineralogical collection; mineralogical sample; mineralogical sample quality; the degree of knowledge of the mineralogical sample; the rarity of the mineral.




Pekov I.V. In development of some issues of museum science in the field of mineralogy. III. On the concept of "mineral discovery" in the broad sense and its characteristics, pp. 16-22

The article is devoted to the concept of "finding a mineral" in the broad sense, which is defined as the entire set of samples of this mineral found (collected) at a given mineralogical object (location of the mineral). The issues related to the indicator of museum-collection quality of mineral finds are discussed in most detail, criteria for its evaluation in application to various minerals and corresponding evaluation systems are proposed.
Keywords: Mineralogical Museum; mineralogical collection; geographic information in mineralogy; mineral discovery.



Borisova E.A. Book of MB Chistyakova “Stone-cutting products in the collection of the Fersman Mineralogical Museum of RAS", pp. 23-26

In 2019, a monograph by Marianna Borisovna Chistyakova was published, dedicated to the description of the collection of ornamental and precious stones of the Mineralogical Museum named after A.E. Fersman of the Russian Academy of Sciences. On February 6, 2019, there was a presentation of this publication, published with the help of the Gokhran of Russia and sponsor E.E. Bogomolov.
Keywords: collection of ornamental and precious stones, stone-cutting products, Mineralogical Museum, A.E. Fersman.



Generalov M.E. In the wake of the Danish Italian. Collection Antonio Cetti (Antonio Cetti) in the Mineralogical Museum. A.E. Fersman, pp. 27-34

New data are published about Antonio Cetti and his mineralogical collection, acquired for the Kunstkamera in 1806 and later merged into the collection of the Mineralogical Museum named after A.E. Fersman. The information obtained helped to clarify the possible period of its formation, to connect samples to this collection for which authorship was not indicated or inaccurate in the documents of the museum.
Keywords: history of the mineralogical collection, collector of natural science collections, Antonio Chetti, Kunstkamera, Mineralogical Museum, A.E. Fersman.



Issue 2

Plechov P.Yu., Pekov I.V., Belakovsky D.I., Pautov L.A., Kasatkin A.V., Agakhanov A.A., Moiseev M.M., Karpenko V.Yu., Nekrylov N .A., Gritsenko Yu.D., Garanin V.K. Diversity of minerals and their paragenesis: scientific results of the Ferman Mineralogical Museum of RAS in 2018, pp. 36-57

The article is a summary of the main scientific results of the employees of the Fersman Mineralogical Museum of RAS (MinMuseum RAS) for 2018. Brief descriptions of 31 new mineral species are given: horseradish, rhabdoborite- (V), rhabdoborite- (W), manaevite- (Ce), paraberceliitis, whitework, zubkovit, achirofanit, aleutite, elasmochloite, canauerite, udinite, arsenudinite, akoperite, akoperit, (La), Radekškodaite- (La), Glaskovite, ferrierite, Dalnegorskite, red matte, Antophagastite, Pliniusite, Jarjemskyite, Alekskhomyakovite, Milanriderite, Kruenite, Falgarite, Badakhshanite- (Y), Nataliya-Kulikit, Avdey Perdeit.
The current results of the mineralogical study of the Arkhangelsk diamondiferous province, the Pamir pegmatites, the fumaroles of the Tolbachinsky dol and coal fire sublimates of Ravat, the rare-earth mineralization of the Mochalin Log and the thallium mineralization of the Vorontsov deposit in the Urals are summarized.
The results of studying olivine of magnesian skarn and rare finds for igneous rocks of extreme magnesian olivine (Fo> 96) and olivine containing up to 0.48 wt.% P2O5 are presented. In olivine of magnesian skarns, a substantial titanium content was first recorded. The data on the composition of chromium spinelide inclusions in olivine from the volcanic rocks of Kamchatka are summarized.
Keywords: MinMuseum RAS, report on scientific work for 2018, 31 new minerals, new data on the mineralogy of natural objects, variations in the composition of rock-forming minerals.



Issue 3

Sandalov F.D., Koshlyakova N.N., Pekov I.V., Yapaskurt V.O., Khanin D.A., Sidorov E.G. Cassiterite from fumarole exhalations of the Tolbachik volcano (Kamchatka): chemical composition and morphogenetic features, pp. 60-70

In the present work, cassiterite of fumarole genesis was first characterized. It was found in the deposits of the active fumarole Arsenatnaya (Second slag cone of the Northern breakthrough of the Great Fissure Tolbachinsky eruption 1975–76, Tolbachinsky dol, Tolbachik volcanic massif, Kamchatka), where it is closely associated with “salt” minerals - sylvin, halite - and alkaline sulfates of the group aphthalitis, as well as with anhydrous arsenates of Ca, Mg, Na, Fe and Cu. Cassiterite here is represented by “fluffy” soft radial-radiant aggregates of fine-needle to hairy crystals in the cavities, which is a consequence of rapid crystallization from the gas phase. It also forms a sagenite lattice on hematite, which was recorded for cassiterite for the first time.
Keywords: cassiterite, tin in hematite, isomorphism, exhalation mineral formation, fumarole, Tolbachik volcano, Kamchatka.



 Pekov I.V. In development of some issues of museum science in the field of mineralogy. IV. On extraordinary mineralogical objects and their significance, pp. 71-79

The article is devoted to questions of the importance of mineralogical objects - the locations of minerals - in the scientific, museum-collection and environmental aspects. Extraordinary mineralogical objects are discussed, their importance scientifically and generally culturally, criteria for classifying a mineralogical object as extraordinary, the principles of ranking them by significance and a classification scheme proposed for this, taking into account, among other things, the nature of the mineralogical material originating from this object.
Keywords: mineralogical museum, mineralogical collection, mineralogical object, location of minerals, geographical information in mineralogy, natural monument.



Kasatkin A.V., Skoda R. Find of Kirkyite at the Berezovsky gold ore deposit (Middle Urals), pp. 80-85

A rare lead sulfovismuthite-sulfoarsenite Kirkyite Pb10Bi3As3S19 was installed by us in a sample from the Berezovsky gold ore deposit (Sverdlovsk region, Middle Urals), stored in the systematic collection of the Mineralogical Museum named after AE Fersman RAS under the number 71444. The mineral forms inclusions up to 50 microns in size in kozalite. The empirical formula of the Kirkite Pb9.92 (Bi2.91Sb0.18) is Σ3.09As2.97S19.01. The parameters of the monoclinic unit cell are: a = 8.582 (18), b = 26.12 (4), c = 8.80 (2) Å, β = 119.8 (2) °, V = 1711 (6) ų. Kirkiit was found for the first time in the Russian Federation.
Keywords: kirkiit, kozalit, Berezovskoye gold deposit, Middle Urals, the first mineral discovery in Russia.



Nenasheva S.N., Borisova E.A., Pavlova T.M. The article is dedicated to the oldest employee of the Mineralogical Museum named after A.E. Fersman, Marianna Borisovna Chistyakova (1929–2015), who worked at the museum for more than 60 years and was the custodian of funds and expositions of the collection of precious and ornamental stones.
Keywords: Fersman Mineralogical Museum of RAS, a collection of ornamental and precious stones, a museum exposition, stone-cutting products, MB Chistyakova.



Issue4

Pautov L.A., Mirakov M.A., Makhmadsharif S., Karpenko V.Yu., Fayziev A.R. Finding of native tellurium in sublimates of a natural underground fire in the tract Kukhi-Malik at the Fan-Yagnob coal deposit (Tajikistan), pp. 95-99

The discovery of native tellurium in sublimates of high-temperature fumaroles in a natural underground coal fire in the tract Kukhi-Malik near the village of Rawat in the Fan-Yagnob coal deposit in the Sogd region of Tajikistan is described. Tellurium is represented by well-formed prismatic crystals (0.1 mm), on which the faces m {10¯10}, ¯e {01¯12}, r {10¯11} are most developed, and a number of unidentified forms are less common with {0001}. In association with tellurium are Fe and K sulfates, Tl and K sulfate, and anglesite. Tellurium crystals are zonal; the central part is enriched in selenium (up to 10 wt.%). The physical properties and main reflections of the X-ray powder diffraction pattern are presented.
Keywords: native tellurium, selenium-containing tellurium, an isomorphic series of selenium - tellurium, minerals of sublimates, fumaroles, coal fire, Tajikistan, Fan-Yagnob deposit, Ravat, Kuhi-Malik.



Borisova E.A., Plechov P.Yu. To the 110th anniversary of the periodical publication of the Mineralogical Museum named after A.E. Fersman Russian Academy of Sciences, pp. 100-113

In 2017, 110 years have passed since the publication of the first issue of the periodical of the museum, now bearing the name of Academician A.E. Fersman. The article gives a brief overview of the issues of the journal for the first decade of its existence (the period from 1907 to 1917–1918).
Keywords: Fersman Mineralogical Museum of RAS, New Data on Minerals, History of the Mineralogical Journal.



Mirakov M.A., Pautov L.A., Karpenko V.Yu., Fayziev A.R., Makhmadsharif S Pauflerit β-VO (SO4) in the sublimates of a natural underground fire in the tract Kuhi-Malik (Rawat) at Fan- Yagnob coal deposit, Tajikistan, pp. 114-121

A description of the finding of β-VO (SO4) pauflerite in the sublimates of high-temperature gas emissions from a natural coal fire in the Kukhi-Malik tract near the village of Ravat, Fan-Yagnob coal deposit, Tajikistan, in brecciated siltstones. Pauflerite crystals are elongated-prismatic, measuring 40–100 microns; simple forms: b {010}, m {101} (most developed), e 110}, p {111}, δ {212}. Doubles are observed in (010) (?). The mineral is transparent, green, fragile. Glitter glass. Powflerite is optically biaxial, 2V close to 90º. The dispersion of the optical axes is very weak, v> r. The plane of the optical axes is perpendicular to the elongation of the crystals; np = 1.733 (2), nm = 1.778 (3), ng calc. = 1.823 (4). Pleochroism: by Ng - green color, by Nm and Np - light green. Absorption scheme Ng> Nm> Np. Composition (cf. 3 ann., Electron probe data, wt.%): VO2 49.87, SO3 50.01, amount 99.88. The empirical formula is V0.97O (S1.02O4). The parameters of the rhombic unit cell (Ǻ): a = 7.392 (3), b = 6.272 (2), c = 7.064 (3). For the first time, a powder x-ray and drawings of powderedite crystals are shown. According to the presence of the mineral phases V, Cd, Mo, Tl, Bi, Sn, In, Sb, Se, Te, As, the sublimates of a coal fire at the Fan-Yagnobskoye deposit are close to the sublimates of the volcanic fumaroles of Kamchatka, Kuril, Italy, due to the common extraction mechanisms the gases of these elements from the host rocks, their transfer and deposition in the unloading zones.
Keywords: pauflerite, vanadium, vanadil, sulfate, minerals of sublimates, fumaroles, coal fire, Tajikistan, Fan-Yagnob deposit, Ravat, Kuhi-Malik.