{"id":6993,"date":"2019-06-06T10:47:55","date_gmt":"2019-06-06T07:47:55","guid":{"rendered":"http:\/\/rion-journal.com\/?p=6993"},"modified":"2019-06-06T10:47:55","modified_gmt":"2019-06-06T07:47:55","slug":"5-2019","status":"publish","type":"post","link":"http:\/\/rion-journal.com\/en\/2019\/06\/06\/5-2019\/","title":{"rendered":"(\u0440\u0443\u0441\u0441\u043a\u0438\u0439) 5-2019"},"content":{"rendered":"<p><a href=\"http:\/\/rion-journal.com\/wp-content\/uploads\/2019\/06\/Nedra-05_19-1.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-medium wp-image-6991\" src=\"http:\/\/rion-journal.com\/wp-content\/uploads\/2019\/06\/Nedra-05_19-1-212x300.jpg\" alt=\"\" width=\"212\" height=\"300\" srcset=\"http:\/\/rion-journal.com\/wp-content\/uploads\/2019\/06\/Nedra-05_19-1-212x300.jpg 212w, http:\/\/rion-journal.com\/wp-content\/uploads\/2019\/06\/Nedra-05_19-1-106x150.jpg 106w, http:\/\/rion-journal.com\/wp-content\/uploads\/2019\/06\/Nedra-05_19-1.jpg 591w\" sizes=\"auto, (max-width: 212px) 100vw, 212px\" \/><\/a><\/p>\n<table>\n<tbody>\n<tr>\n<td width=\"667\">\n<h3>CONTENTS \u2116 5\/2019<\/h3>\n<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<h3>GEOLOGY &amp; METHODICS OF PROSPECT &amp; EXPLORATION OF DEPOSITS<\/h3>\n<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<p>\u0423\u0414\u041a 55(092)+55(091)<\/p>\n<p><strong>Aksenov S.A.<\/strong> (Rosnedra) \/\/ <a href=\"mailto:saksenov@rosnedra.gov.ru\">saksenov@rosnedra.gov.ru<\/a><\/p>\n<p><strong>Bavlov V.N.<\/strong> (NAEN) \u00bb) \/\/ <a href=\"mailto:npnaen@mail.ru\">info@naen.ru<\/a><\/p>\n<p><strong>Mashkovtsev G.A<\/strong>. (VIMS) \/\/ <a href=\"mailto:vims@df.ru\">vims@df.ru<\/a><\/p>\n<p><strong>Pechenkin I.G.<\/strong> (VIMS) \/\/ <a href=\"mailto:pechenkin@vims-geo.ru\">pechenkin@vims-geo.ru<\/a><\/p>\n<p><strong>EVGENIY ALEKSANDROVICH KOZLOVSKIY \u2013 OUTSTANDING HEAD OF THE GEOLOGICAL BRANCH<\/strong><\/p>\n<p>The article shows the life course of E.A. Kozlovskiy &#8211; an outstanding public figure, a gifted scientist, a long-term leader of the geological industry, and an organizer of new trends in the creation of a fatherland mineral resource base.<\/p>\n<p><strong>Keywords:<\/strong> mineral deposits (MD), mineral resource base, method of exploration of MD, geological and economic assessment of MD.<\/p>\n<p>\u0420. 4-7<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<p>\u0423\u0414\u041a 551.7+553.04 (571.6)<\/p>\n<p><strong>Shashorin B.N.<\/strong> (VIMS) \/\/ <a href=\"mailto:shashorin.boris@yadex.ru\">shashorin.boris@yadex.ru<\/a><\/p>\n<p><strong>Makarov A.I.<\/strong> (VIMS) \/\/ vims@vims-geo.ru<\/p>\n<p><strong>Matveeva E.V.<\/strong> (VIMS) \/\/ matveeva@vims-geo.ru<\/p>\n<p><strong>Vydrich D.E.<\/strong> (VIMS) \/\/ <a href=\"mailto:devrich@mail.ru\">devrich@mail.ru<\/a><\/p>\n<p><strong>ORE-CONTROLLING FACTORS AND ESTIMATION OF WOLFRAMTONES INDIVIDUAL TERRITORIES CENTRAL SIKHOTE-ALIN<\/strong><\/p>\n<p>Ore-controlling factors determining the space-time position of W-ore objects in the folded-block structure of Sikhote-Alin are characterized, as well as the most important search criteria and features used to assess the prospects of tungsten content and localization of search areas. The results of spectral-correlation analysis of gravity and magnetic data sheet L-53-VI (fields Dg and D\u0422 scale 1:200 000), which allowed to reproduce (outline) in the values of the densities (g\/cm3) and conventional units of magnetization of rocks potentially ore-bearing volume of the subsoil in the area of sheet L-53-VI and to allocate, within its limits, the situation close to their geological and geophysical characteristics to the reference ore areas and knots of Primorsky Krai (East, Lermontov RU). Within the limits of sheet L-53-VI the prospecting sites of the grade &#8220;ore node-field&#8221;, perspective on revealing of skarn-sheelite-sulfide deposits with rich ores (from 0,3% to 5,5-7,06%, WO3 and more) are designated and contoured.<\/p>\n<p><strong>Keywords: <\/strong>collisional-orogenic granites I-S genetic types, turbidite-flysch and olistostromic strata of J-K1 with inclusions of upper Paleozoic limestones, areas of decompressed masses with high and abnormally high values of magnetic properties.<\/p>\n<p>\u0420. 8-18<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<p>\u0423\u0414\u041a 549.514.51<\/p>\n<p><strong>K<\/strong><strong>abanova L.Y\u0430<\/strong><strong>.<\/strong> (Institute of mineralogy of the Ural division of RAS) \/\/ kablar@mineralogy.ru<\/p>\n<p><strong>I<\/strong><strong>gumentseva M.A.<\/strong> (Institute of mineralogy of the Ural division of RAS) \/\/ maria@mineralogy.ru<\/p>\n<p><strong>N<\/strong><strong>ikandrova N.K.<\/strong> (Institute of mineralogy of the Ural division of RAS) \/\/ nikandrova@ilmeny.ac.ru<\/p>\n<p><strong>A<\/strong><strong>nfilogov V.N.<\/strong> (Institute of mineralogy of the Ural division of RAS) \/\/ anfilogov@mineralogy.ru<\/p>\n<p><strong><a href=\"https:\/\/elibrary.ru\/author_items.asp?authorid=859110\">Ryzhkov<\/a><\/strong><strong> V.M. <\/strong>(Institute of mineralogy of the Ural division of RAS) \/\/ ryzhkov@mail.ru<\/p>\n<p><strong>GEOLOGY AND PETROGRAPHY OF DEPOSITS OF VEIN QUARTZ \u00abPESCHANOE\u00bb (SOUTH URAL)<\/strong><\/p>\n<p>The article presents actual data on the geological position of quartz veins formed during the process of filling open cracks in the granite massif. Change the granites, developed places in the mylonites and blastomylonites and the presence of quartz grains distinct traces of brittle and plastic deformations indicate <a href=\"https:\/\/www.babla.ru\/%D0%B0%D0%BD%D0%B3%D0%BB%D0%B8%D0%B9%D1%81%D0%BA%D0%B8%D0%B9-%D1%80%D1%83%D1%81%D1%81%D0%BA%D0%B8%D0%B9\/cataclastic-metamorphism\">cataclastic<\/a> metamorphism after the formation of quartz veins. The study of quartz aggregates and investigation of gas-fluid inclusions in grains of white, milky white and grey quartz allowed us to determine the temperature range of eutectic at cryothermometric data and the maximum temperature of homogenization 356 \u00ba\u0421 and minimum 241 \u00ba\u0421\u2013257 \u00ba\u0421. These data indicate that the hydrothermal formation of quartz veins at the temperature of 300 \u00baC\u2013360 \u00ba\u0421. Recrystallization of quartz in the process of the volumetric strain occurred at temperatures 200 \u00ba\u0421\u2013270 \u00ba\u0421.<\/p>\n<p><strong>Keywords:<\/strong> quartz, granite, blastomylonits, gas-fluid inclusions, the temperature of homogenization.<\/p>\n<p>\u0420. 18-24<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<p>\u0423\u0414\u041a 550.84: 523.21<\/p>\n<p><strong>Sokolov <\/strong><strong>S.<\/strong><strong>V.<\/strong> (VSEGEI) \/\/ <a href=\"mailto:Sergey_Sokolov@vsegei.ru\">Sergey_Sokolov@vsegei.ru<\/a><\/p>\n<p><strong>METHODS OF QUANTITATIVE RESOURCE ASSESSMENT ACCORDING TO THE GEOCHEMICAL DATA <\/strong><strong>FROM<\/strong><strong> POTENTIALLY ORE AREAS AT THE STAGE OF REGIONAL STUDY OF <\/strong><strong>THE <\/strong><strong>SUBSOIL<\/strong><\/p>\n<p>Methods of forecast resources assessment reflected in the current normative methodological documents are considered in terms of the critical approach. The method proposed by the authors, unlike the one, taken from the instruction, provides for the assessment of resources for higher-ranks ore objects, taking into account the share of commercial metal as well as on the basis of the theoretically grounded and practically widely tested system of parameters selecting as well as selecting of characteristics for anomalies and predicted mineralization. Resource assessments obtained with use of the method proposed are much more adequate to the prospecting and exploration data than the one, taken from the instruction.<\/p>\n<p><strong>Keywords:<\/strong> anomalous geochemical field, speculative resources of P<sub>3<\/sub> category.<\/p>\n<p>\u0420. 24-32<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<p>\u0423\u0414\u041a 552.553<\/p>\n<p><strong>Arkhangelskaya V.V.<\/strong> (VIMS)<\/p>\n<p><strong>KOND\u0415R MASSIF. HISTORY OF OPENING AND STUDYING<\/strong><\/p>\n<p>In article details of discovery of studying of the zone and concentric polymagmatic Kondyorsky massif are considered. Breeds of the massif compose Mount Konder. Characteristic of the Kondyorsky platinum field is given.<\/p>\n<p><strong>Keywords<\/strong>: Kondyorsky massif, mount \u041aonder, Kondersky platinum deposit.<\/p>\n<p>\u0420. 32-38<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<h3>GEOPHYSICS<\/h3>\n<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<p>\u0423\u0414\u041a 3311.02<\/p>\n<p><strong>Allahverdiev K.R.<\/strong> (National Academy of Aviation of the Republic of Azerbaijan) \/\/ kerim.allahverdi@gmail.com<\/p>\n<p><strong>Akhmedov E.A.<\/strong> (National Academy of Aviation of the Republic of Azerbaijan) \/\/ eynur1957@mail.ru<\/p>\n<p><strong>Gumbatov F.Yu.<\/strong> (Institute of \u00abRadiation problems\u00bb of the national Academy of Sciences of the Republic of Azerbaijan) \/\/ hfamil@mail.ru<\/p>\n<p><strong>GAMMA\u2013SPECTROMETRIC ANALYSIS OF THE RADIONUCLIDE COMPOSITION OF THE DASH-SALAKHLINSKY BENTONITE CLAY AND THE ROLE OF DIFFUSION PROCESSES IN RADIONUCLIDE MIGRATION<\/strong><\/p>\n<p>This article deals with the analysis of the radionuclide composition of dash-Salakhlin bentonite clay and the role of diffusion processes in the migration of these radionuclides. With this purpose g-spectrometric method of analysis were used. It is shown that very high radioactivity of bentonite clay is associated with a high content of <sup>40<\/sup>K, <sup>226<\/sup>Ra, <sup>232<\/sup>Th in its composition and is caused by active exogenous and endogenous migration processes.<\/p>\n<p><strong>Keywords:<\/strong> radioactiviti, radionuclide, migration, diffuzion, sorption, sedimentary rosk, bentonitic clay.<\/p>\n<p>\u0420. 38-41<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<h3>HYDROGEOLOGY &amp; GEOLOGICAL ENGINEERING<\/h3>\n<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<p>\u0423\u0414\u041a 551.24; 551.432<\/p>\n<p><strong>Karfidova E.A.<\/strong> (Environmental Geosciences Institute RAS) \/\/ e.karfidova@yandex.ru<\/p>\n<p><strong>Kravchenko I.M.<\/strong> (Environmental Geosciences Institute RAS) \/\/ kravchenkoilyamax@yandex.ru<\/p>\n<p><strong>Makeev V.M.<\/strong> (Environmental Geosciences Institute RAS) \/\/ vmakeev@mail.ru<\/p>\n<p><strong>DEVELOPMENT OF METHODS OF EVALUATION OF SURFACE RUNOFF ON AN EXAMPLE OF THE TERRITORY OF VERKHNEKAMSK DEPOSIT OF POTASSIUM AND MAGNESIUM SALTS<\/strong><\/p>\n<p>During the research for the first time a model of the surface runoff net of river Usolka, located within the central part of the Verkhnekamsk deposit of potassium and magnesium salts (VDPMS) was created. The model considers streams of different orders, closed local relief depressions, catchment basins and their morphometric and hydrological indices. The proposed methods allow to identify zones of increased moisture, which is accompanied by increased infiltration of surface water into the rocks, that leads to the development of suffusion and karst processes.<\/p>\n<p><strong>Keywords<\/strong>: geomorphology, surface runoff, suffusion, karst, deposit, safety.<\/p>\n<p>\u0420. 42-49<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<h3>TECHNIQUES &amp; TECHNOLOGY<\/h3>\n<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<p>\u0423\u0414\u041a 338.33:553.04<\/p>\n<p><strong>Krasnov <\/strong><strong>O.<\/strong><strong>S. <\/strong>(VNIGRI) \/\/ <a href=\"mailto:Okrasnov@vnigri.ru\">Okrasnov@vnigri.ru<\/a><\/p>\n<p><strong>Salikhov V.A.<\/strong> (FGBEU VO \u00abKemerovo State University\u00bb, Novokuznetsk) \/\/ <a href=\"mailto:Salihov-VA@yandex.ru\">Salihov-VA@yandex.ru<\/a><\/p>\n<p><strong>Korol L.N.<\/strong> (FGBEU VO \u00abKemerovo State University\u00bb, Novokuznetsk) \/\/ <a href=\"mailto:korol.lenya@yandex.ru\">korol.lenya@yandex.ru<\/a><\/p>\n<p><strong>METHODOLOGICAL AND METHODICAL ASPECTS OF THE DEVELOPMENT OF ECONOMICALLY EFFECTIVE AND ECOLOGICALLY SAFE TECHNOLOGIES OF PROCESSING OF MINERAL RAW MATERIALS AND WASTE<\/strong><\/p>\n<p>Due to the lack of a mineral resource base of strategically important rare metals in the Russian Federation, methodological and methodological approaches have been proposed for the development of cost-effective and environmentally friendly technologies for the extraction of these metals from mineral raw materials and industrial wastes. The main parameters of the geological and economic assessment of objects that are promising for the extraction of rare metals are given. The criteria for evaluating the effectiveness of the technologies being developed are substantiated. Tasks are grounded and a sequential phased scheme for the development of innovative technologies is proposed.<\/p>\n<p><strong>Keywords:<\/strong> rare metals, parameters, criteria, methods, technologies.<\/p>\n<p>\u0420. 50-53<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<p>\u0423\u0414\u041a (696.6+628.9 622.143) (075.8)<\/p>\n<p><strong>Bashkurov <\/strong><strong>A.<\/strong><strong>Yu.<\/strong> (MGRI-RGGRU) \/\/ <a href=\"mailto:Bashkurov_A@inbox.ru\">Bashkurov_A@inbox.ru<\/a><\/p>\n<p><strong>THE CHOICE OF OPTIMAL COMPOSITION OF LIGHT WEIGHT CEMENT SLURRY FOR<\/strong><\/p>\n<p>In conditions of market economy the mining industry is a topical problem of the quality of well construction, especially getting in the annulus of a hard cement, which will ensure planned production figures. You need to light backfill cement the required performance properties of the available, cheap materials. Of considerable interest as additives to facilitate represent luminosilicate hollow microspheres. The aim of this work is to determine the optimal composition of the lightweight cement slurry for cementing wells and analyze the effect of various reagents on the quality of education of the cement lining, that is, improving the quality of cementing.<\/p>\n<p><strong>Keywords:<\/strong> aluminosilicate microspheres cementation.<\/p>\n<p>\u0420. 53-56<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<h3>MANAGEMENT &amp; ECONOMICS<\/h3>\n<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<p>\u0423\u0414\u041a 553.04:669.168+622.7+338.5<\/p>\n<p><strong>Mashkovtsev<\/strong> <strong>G<\/strong><strong>.<\/strong><strong>A<\/strong><strong>.<\/strong> (VIMS) \/\/ vims@vims-geo.ru<\/p>\n<p><strong>Bakanova T.V. <\/strong>(VIMS) \/\/ bakanova@vims-geo.ru<\/p>\n<p><strong>Rudnev A.V.<\/strong> (Rosnedra) \/\/ arudnev@rosnedra\/gov.ru<\/p>\n<p><strong>MINERAL RAW MATERIALS FOR FERROALLOY INDUSTRY<\/strong><\/p>\n<p>The article is devoted to the problem of mineral resources supplies of the domestic ferroalloy industry. It examines the state of production, export-import of ferroalloys and its mineral resource base. The heavy deficit of reserves of rich manganese and chromium ores covered by expensive imports is shown. Recommendations on import substitution of scarce raw materials through development and implementation of effective technologies of poor and persistent ores processing at the previously explored deposits, and also revealing and development of new economically acceptable deposits are offered.<\/p>\n<p><strong>Keywords:<\/strong> ferroalloys, mineral raw materials, ore-dressing technologies, visible consumption, export, import of concentrates and ferroalloys.<\/p>\n<p>\u0420. 57-66<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<p><a name=\"_Toc428099602\"><\/a><a name=\"_Toc506137673\"><\/a><a name=\"_Toc509816968\"><\/a><\/p>","protected":false},"excerpt":{"rendered":"<p>CONTENTS \u2116 5\/2019 GEOLOGY &amp; METHODICS OF PROSPECT &amp; EXPLORATION OF DEPOSITS \u0423\u0414\u041a 55(092)+55(091) Aksenov S.A. (Rosnedra) \/\/ saksenov@rosnedra.gov.ru Bavlov V.N. (NAEN) \u00bb) \/\/ info@naen.ru Mashkovtsev G.A. (VIMS) \/\/ vims@df.ru Pechenkin I.G. (VIMS) \/\/ pechenkin@vims-geo.ru EVGENIY ALEKSANDROVICH KOZLOVSKIY \u2013 OUTSTANDING HEAD OF THE GEOLOGICAL BRANCH The article shows the life course of E.A. Kozlovskiy &#8211; [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":6991,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[27],"tags":[],"class_list":["post-6993","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-27"],"acf":[],"_links":{"self":[{"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/posts\/6993","targetHints":{"allow":["GET"]}}],"collection":[{"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/comments?post=6993"}],"version-history":[{"count":0,"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/posts\/6993\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/media\/6991"}],"wp:attachment":[{"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/media?parent=6993"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/categories?post=6993"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/tags?post=6993"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}