Zapiski Rossiiskogo Mineralogicheskogo Obshchestva最新文献_第9页

Amino acid composition of gallstones and its connection with the mineral component 胆结石的氨基酸组成及其与矿物成分的关系

Zapiski Rossiiskogo Mineralogicheskogo Obshchestva Pub Date : 2019-09-09 DOI: 10.30695/zrmo/2019.1484.07

E. V. Mashina, Машина Екатерина Валерьевна, S. Shanina, Шанина Светлана Николаевна

引用次数: 3

Niz'yavrski alkaline massif: age, isotopic characteristics and rare-metal mineralization 尼兹亚夫斯基碱性地块:年龄、同位素特征与稀有金属成矿作用

Zapiski Rossiiskogo Mineralogicheskogo Obshchestva Pub Date : 2019-09-09 DOI: 10.30695/zrmo/2019.1484.01

M. N. Petrovskiy, Петровский Михаил Николаевич

引用次数: 0

Once again about the Curie dissymmetry principle 再谈居里不对称原理

Zapiski Rossiiskogo Mineralogicheskogo Obshchestva Pub Date : 2019-06-25 DOI: 10.30695/ZRMO/2019.1483.09

Y. Voytekhovsky, Войтеховский Юрий Леонидович

引用次数: 1

Wolframoixiolite in lithium-fluoric granites of the Arga-Ynnakh-Khaysky massif, Yakutia 雅库特Arga Ynnakh Khaysky地块锂氟花岗岩中的Wolframoixiolite

Zapiski Rossiiskogo Mineralogicheskogo Obshchestva Pub Date : 2019-06-25 DOI: 10.30695/ZRMO/2019.1483.03

V. Alekseev, Алексеев Виктор Иванович, Yu. B. Marin, Марин Юрий Борисович, O. Galankina, Галанкина Ольга Леонидовна

{"title":"Wolframoixiolite in lithium-fluoric granites of the Arga-Ynnakh-Khaysky massif, Yakutia","authors":"V. Alekseev, Алексеев Виктор Иванович, Yu. B. Marin, Марин Юрий Борисович, O. Galankina, Галанкина Ольга Леонидовна","doi":"10.30695/ZRMO/2019.1483.03","DOIUrl":"https://doi.org/10.30695/ZRMO/2019.1483.03","url":null,"abstract":"For the first time, lithium-fluoric granites and ongonites of the Arga-Ynnakh-Khaysky massif (East Yakutia) have been revealed to contain an accessory complex of tungsten-bearing tantalum-niobates ( columbite-(Fe), columbite-(Mn), tantalite-(Mn), minerals of microlite group, tantalic rutile ) including «wolframoixiolite». These rocks containing wolframoixiolite, their composition and typomorphic features are described: they are highly ferriferous, with major geochemical role of niobium and wide variations of tungsten and tantalum concentrations. Wolframoixiolite occurs there in paragenesis with tungsten-bearing columbite-(Mn), tantalum-niobium ferberite, lepidolite and topaz. Wolframoixiolite of the Arga-Ynnakh-Khaysky massif was formed on a late-magmatic stage of lithium-fluoric granites crystallization by polymorphic transformation of columbite-(Fe). The study of accessory mineralization in rare-metal granites of Eurasia allows, taking into account a new find, to draw a conclusion, that wolframoixiolite is typomorphic accessory mineral in lithium-fluoric granites and may be looked as the indicator of rare-metal-granite magmatism with accompanying tin-rare-metal ore mineralization.","PeriodicalId":36969,"journal":{"name":"Zapiski Rossiiskogo Mineralogicheskogo Obshchestva","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2019-06-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"45793605","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 1

High-temperature behavior of axinite-(Mn), kornerupine and leucosphenite 铝辉石-(Mn)、高锰矿和白钨矿的高温行为

Zapiski Rossiiskogo Mineralogicheskogo Obshchestva Pub Date : 2019-06-25 DOI: 10.30695/ZRMO/2019.1483.06

M. Krzhizhanovskaya, Кржижановская Мария Георгиевна, V. A. Firsova, Фирсова Вера Александровна, R. Bubnova, Бубнова Римма Сергеевна, S. Britvin, Бритвин Сергей Николаевич, Olga G. Bubnova, Бубнова Ольга Геннадьевна, I. Pekov, Пеков Игорь Викторович

{"title":"High-temperature behavior of axinite-(Mn), kornerupine and leucosphenite","authors":"M. Krzhizhanovskaya, Кржижановская Мария Георгиевна, V. A. Firsova, Фирсова Вера Александровна, R. Bubnova, Бубнова Римма Сергеевна, S. Britvin, Бритвин Сергей Николаевич, Olga G. Bubnova, Бубнова Ольга Геннадьевна, I. Pekov, Пеков Игорь Викторович","doi":"10.30695/ZRMO/2019.1483.06","DOIUrl":"https://doi.org/10.30695/ZRMO/2019.1483.06","url":null,"abstract":"In situ high-temperature powder X-ray diffraction (HTPXRD) and differential scanning calorimetry (DSC) of three natural borosilicates have been performed in the temperature range of 25—1200 °С. Axinite-(Mn) melts incongruently at 900 °С forming anorthite and bustamite. Leucosphenite decomposes at 850 °С to fresnoite and cristobalite. According to DSC data, kornerupine decomposes at 1177 °С and sapphirine, indialite, and spinel were observed as the products of kornerupine heating. The calculation and orientation of thermal expansion tensor have been performed using HTPXRD data. The study showed that the borosilicates expand weakly and almost isotropically. The average volumetric thermal expansion coefficients are 21.3, 22.7, and 32.9 ∙ 10 –6 °C –1 for axinite-(Mn), kornerupine, and leucosphenite, respectively. Leucosphenite has a maximum volumetric expansion most likely due to the pronounced layered character of the crystal structure. The least symmetric structure of axinite-(Mn) has the maximal anisotropy of thermal expansion in the temperature range of 600—900 °C.","PeriodicalId":36969,"journal":{"name":"Zapiski Rossiiskogo Mineralogicheskogo Obshchestva","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2019-06-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"44827692","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Симметрийная статистика минеральных видов в различных термодинамических обстановках 不同热力学环境中矿物物种对称统计

Zapiski Rossiiskogo Mineralogicheskogo Obshchestva Pub Date : 2019-06-25 DOI: 10.30695/zrmo/2019.1483.00

Филатов Станислав Константинович

{"title":"Симметрийная статистика минеральных видов в различных термодинамических обстановках","authors":"Филатов Станислав Константинович","doi":"10.30695/zrmo/2019.1483.00","DOIUrl":"https://doi.org/10.30695/zrmo/2019.1483.00","url":null,"abstract":"Обобщаются сведения о симметрии минералов в различных земных оболочках как функции от температуры, давления и совместного воздействия этих параметров. Показывается, что распределение минеральных видов по симметрийной иерархии, в частности существование моноклинного максимума и триклинного минимума в симметрийной статистике окружающего нас мира минералов и неорганических соединений, определяется прежде всего двумя разнонаправленными факторами — динамичностью решетки (количеством не фиксированных симметрией параметров элементарной ячейки) и экономичностью кристаллического строения (максимальной кратностью атомных позиций, допускаемой данной точечной группой). С ростом температуры симметрия вещества обычно повышается, с ростом давления — понижается при перманентном сжатии структуры и повышается при ее реконструкции. Совместное возрастание температуры и давления при погружении в глубь Земли вызывает устойчивое повышение средней симметрии горной породы от единиц до максимальной величины 48 индекса Доливо-Добровольского. Многопараметричность симметрийной статистики минералов позволяет оставить без комментариев некоторые флуктуации зависимости до их проверки временем.","PeriodicalId":36969,"journal":{"name":"Zapiski Rossiiskogo Mineralogicheskogo Obshchestva","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2019-06-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69567370","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 1

Rare earth minerals in ores of the malmyzhskoe gold-copper-porphyry deposit (Khabarovsky krai) malmyzhskoe金铜斑岩矿床（哈巴罗夫斯克-克拉伊）矿石中的稀土矿物

Zapiski Rossiiskogo Mineralogicheskogo Obshchestva Pub Date : 2019-03-05 DOI: 10.30695/ZRMO/2019.1481.05

D. Bukhanova, Д С Буханова, V. Chubarov, В М Чубаров

引用次数: 1

Russian mineralogical society as a socio-historical phenomenon (Russian mineralogical society in the XIX—first half of the XX century) 作为社会历史现象的俄罗斯矿物学社会(二十世纪十九至上半叶的俄罗斯矿物学社会)

Zapiski Rossiiskogo Mineralogicheskogo Obshchestva Pub Date : 2019-03-05 DOI: 10.30695/ZRMO/2019.1481.02

T. В. Ilinskaya, Т Б Ильинская

{"title":"Russian mineralogical society as a socio-historical phenomenon (Russian mineralogical society in the XIX—first half of the XX century)","authors":"T. В. Ilinskaya, Т Б Ильинская","doi":"10.30695/ZRMO/2019.1481.02","DOIUrl":"https://doi.org/10.30695/ZRMO/2019.1481.02","url":null,"abstract":"The article is an analysis of materials on the history of science (primarily mineralogy), which make it possible to understand the role of scientific societies in the development of the creativity of scientists. The author of this article was primarily interested in the personal, «human» dimension of the problem. The materials for solving this problem were the memoirs and epistolary of scientists, as well as historiographic materials accompanying the activities of the Russian Mineralogical Society in the period from the 19 th to the middle of the 20 th century. The recent 200 th anniversary of the RMS was a vivid testimony to the viability of the Society, and therefore the focus of the author of the proposed article was that of the «centripetal forces» that allowed the RMS to be preserved, while many other scientific societies disintegrated. In the course of the analysis of the above materials, the following motives are outlined that determine the work of the scientist within the scientific community: scope for personal initiative, the possibility of consolidating efforts, material support for research. Additional incentives for membership in the RMS were revealed: the Society as a post-graduate school, the Society as a guarantor of the traditions of scientific ethics. In addition, the double genesis of the RMS was revealed, which was a continuation of the European line of mineralogy development and at the same time a new direction in domestic science, which eventually becomes the leading one.","PeriodicalId":36969,"journal":{"name":"Zapiski Rossiiskogo Mineralogicheskogo Obshchestva","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2019-03-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"46106568","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Modern mineral formation in the thermal lake Fumarolnoe (Uson caldera, Kamchatka) is the key to paleoreconstruction 热湖Fumarolnoe（堪察加半岛Uson破火山口）的现代矿物形成是古重建的关键

Zapiski Rossiiskogo Mineralogicheskogo Obshchestva Pub Date : 2019-03-05 DOI: 10.30695/ZRMO/2019.1481.00

I. Kirichenko, Игорь Кириченко, E. Lazareva, Е. В. Лазарева, S. Zhmodik, С М Жмодик, N. L. Dobrezov, Н Л Добрецов, D. Belyanin, Д К Белянин, L. V. Miroshnichenko, Л В Мирошниченко

{"title":"Modern mineral formation in the thermal lake Fumarolnoe (Uson caldera, Kamchatka) is the key to paleoreconstruction","authors":"I. Kirichenko, Игорь Кириченко, E. Lazareva, Е. В. Лазарева, S. Zhmodik, С М Жмодик, N. L. Dobrezov, Н Л Добрецов, D. Belyanin, Д К Белянин, L. V. Miroshnichenko, Л В Мирошниченко","doi":"10.30695/ZRMO/2019.1481.00","DOIUrl":"https://doi.org/10.30695/ZRMO/2019.1481.00","url":null,"abstract":"Paleoreconstruction of events involved in the bottom sedimentation has been carried out on the base of mineral composition of a section of bottom sediments in the Lake IV (the Lake Fumarolnoe). The lower levels are composed there mainly of smectite in association with gypsum and jarosite; they are overlapped by smectite-kaolinite depositions with the large amount of diatom algae shells and the fraboidal pyrite. There is also a layer of sinter opal-pyrite structures and calcite. It is assumed that initially the lake IV was a mud pit with sulfide-bearing solutions, then, after the lowering of water level and the partial exposure of bottom sediments of the surface, the substance has been oxidized. The subsequent phreatic explosion has provided the covering of oxidized substance by the matter of lower layers of the pit. The further situation corresponded to the source, with the cyano-bacterial community developing around the griffin, and it was replaced by the site of a shallow-water lake similar to the contemporary one. The studied sedimentary formation includes two layers of pyroclastic material originated from neighbouring eruptions.","PeriodicalId":36969,"journal":{"name":"Zapiski Rossiiskogo Mineralogicheskogo Obshchestva","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2019-03-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"43284374","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Platinum-metal mineralization of the Yuzhnosopchinsky-1 locality (Monchegorsk ore district, Kola peninsula) Yuzhnosopchinsky-1地区（科拉半岛Monchegorsk矿区）的铂金属矿化

Zapiski Rossiiskogo Mineralogicheskogo Obshchestva Pub Date : 2019-03-05 DOI: 10.30695/ZRMO/2019.1481.03

Y. A. Miroshnikova, Я А Мирошникова, A. Chernyavsky, Александр Чернявский, A. V. Bazay, А В Базай

引用次数: 2