{"id":8481,"date":"2023-07-14T15:48:08","date_gmt":"2023-07-14T12:48:08","guid":{"rendered":"http:\/\/rion-journal.com\/?p=8481"},"modified":"2023-07-14T15:48:08","modified_gmt":"2023-07-14T12:48:08","slug":"7-2023","status":"publish","type":"post","link":"http:\/\/rion-journal.com\/en\/2023\/07\/14\/7-2023\/","title":{"rendered":"7-2023"},"content":{"rendered":"<p><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-medium wp-image-8474\" src=\"http:\/\/rion-journal.com\/wp-content\/uploads\/2023\/07\/nedra-07_2023-1-212x300.jpg\" alt=\"\" width=\"212\" height=\"300\" srcset=\"http:\/\/rion-journal.com\/wp-content\/uploads\/2023\/07\/nedra-07_2023-1-212x300.jpg 212w, http:\/\/rion-journal.com\/wp-content\/uploads\/2023\/07\/nedra-07_2023-1-106x150.jpg 106w, http:\/\/rion-journal.com\/wp-content\/uploads\/2023\/07\/nedra-07_2023-1.jpg 591w\" sizes=\"auto, (max-width: 212px) 100vw, 212px\" \/><\/p>\n<table>\n<tbody>\n<tr>\n<td width=\"667\">\n<h3>CONTENTS \u2116 07\/2023<\/h3>\n<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<p>DOI: 10.53085\/0034-026X_2023_07_03<\/p>\n<p>\u0423\u0414\u041a 550.8<\/p>\n<p>Shashorin B.N. (VIMS) \/\/ <a href=\"mailto:shashorin.boris@yadex.ru\">shashorin.boris@yadex.ru<\/a><\/p>\n<p>Makarov A.I. (VIMS) \/\/ <a href=\"mailto:vims@df.ru\">vims@df.ru<\/a><\/p>\n<p>Suchkov A.V. (VIMS) \/\/ <a href=\"mailto:alexsandir@mail.ru\">alexsandir@mail.ru<\/a><\/p>\n<p><strong>MAGMATIC FRONT OF CONTINENTAL CRUST DECOMPRESSION AS ONE OF THE FACTORS OF METALLOGENIC CONTROL IN THE GEOLOGICAL PREDICTION OF POTENTIALLY ORE-BEARING FORMATIONS (ON THE EXAMPLE OF W-Sn- AND Au-U-ORE REGIONS OF NORTHERN KAZAKHSTAN)<\/strong><\/p>\n<p>The geological stages of the formation of ore-bearing structures of Northern Kazakhstan, the depth-density and seismic inhomogeneities of the Earth\u2019s crust of the Kokchetav Precambrian massif and its nearest folded frame are characterized. The position is shown regarding the depth-density and seismic inhomogeneities of the Earth\u2019s crust of W-Sn- and Au-ore nodes, fields, deposits; their localization on the density barrier of ore deposition. An innovative technique for studying the deep structure of the subsurface and geological forecasting of potentially ore-bearing environments is recommended, based on mapping the magmatic front of continental crust decompression ascending from the depths and sections of its (front) wedging into near-surface dense masses.<\/p>\n<p><strong>Keywords:<\/strong> the magmatic front of the continental crust decompression, the density barrier of ore deposition, potentially ore-bearing environments of the \u00abore node-ore field\u00bb rank.<\/p>\n<p>&nbsp;<\/p>\n<p>\u0420.3-12<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<p>DOI: 10.53085\/0034-026X_2023_07_13<\/p>\n<p>\u0423\u0414\u041a 553.2.4.43.44<\/p>\n<p>Velizade S.F. (Institute of Geology and Geophysics of Azerbayjan National Academy of Sciences (ANAS), Baku) \/\/ <a href=\"mailto:velizade.43@mail.ru\">velizade.43@mail.ru<\/a><\/p>\n<p><strong>SOURCES OF ORE MATTER IN PYRITE DEPOSITS OF THE GREATER CAUCASUS SOUTH SLOPE (AZERBAyJAN AREA)<\/strong><\/p>\n<p><strong>\u00a0<\/strong>This article considers possible sources of ore matter of pyrite deposit, transfer mode and reasons for mineral-forming components deposition are highlighted during ore formation process in studied region. It is shown besides deep sources crust sources both of magmatic and non-magmatic nature participated in ore genesis.<\/p>\n<p><strong>Keywords:<\/strong> source, ore matter, pyrite, mantee, oregenesis.<\/p>\n<p>&nbsp;<\/p>\n<p>\u0420.13-19<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<p>DOI: 10.53085\/0034-026X_2023_07_19<\/p>\n<p>\u0423\u0414\u041a 553.06<\/p>\n<p>Redin Yu.O. (Sobolev Institute of Geology and Mineralogy Siberian Branch Russian Academy of Sciences (IGM SB RAS)) \/\/ <a href=\"mailto:redin@igm.nsc.ru\">redin@igm.nsc.ru<\/a><\/p>\n<p>Malyutina A.V. (Sobolev Institute of Geology and Mineralogy Siberian Branch Russian Academy of Sciences (IGM SB RAS)) \/\/ <a href=\"mailto:malyutina@igm.nsc.ru\">malyutina@igm.nsc.ru<\/a><\/p>\n<p>Redina A.A. (Sobolev Institute of Geology and Mineralogy Siberian Branch Russian Academy of Sciences (IGM SB RAS)) \/\/ <a href=\"mailto:redina@igm.nsc.ru\">redina@igm.nsc.ru<\/a><\/p>\n<p>Dultsev V.F. (Sobolev Institute of Geology and Mineralogy Siberian Branch Russian Academy of Sciences (IGM SB RAS)) \/\/ <a href=\"mailto:dultsev@igm.nsc.ru\">dultsev@igm.nsc.ru<\/a><\/p>\n<p><strong>GEOCHEMICAL COMPOSITION OF MAGNETITE FROM ORES OF LARGE Au-Cu-Fe-SKARN (SKARN-PORPHYRY) DEPOSITS OF THE EASTERN TRANSBAIKALIA \u2014 AS AN INDICATOR OF THE DEPOSITS GENETIC AFFILIATION<\/strong><\/p>\n<p>In this article, the mineral composition and geochemical features of magnetite from ores of large gold-copper-iron-skarn deposits in the Eastern Transbaikalia were studied using modern methods. The richest ore bodies with magnetite mineralization are associated with retrograde skarns, where magnetite is associated mainly with actinolite\/tremolite, phlogopite, garnet, and other skarn minerals. The first obtained data on the microelement composition of magnetite made it possible to establish indicator characteristics (values) for skarn and skarn-porphyry types of mineralization.<\/p>\n<p><strong>Keywords:<\/strong> magnetite, typochemistry, skarn deposits, porphyry skarn deposits, Eastern Transbaikalia.<\/p>\n<p>&nbsp;<\/p>\n<p>\u0420.19-25<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<p>DOI: 10.53085\/0034-026X_2023_07_26<\/p>\n<p>\u0423\u0414\u041a 622.775<\/p>\n<p>Beysekeev E.Sh. (NAC \u00abKazatomprom\u00bb, Astana, Republic of Kazakhstan) \/\/ <a href=\"mailto:yermek_f-81@mail.ru\">yermek_f-81@mail.ru<\/a><\/p>\n<p>Yazikov E.G. (Tomsk Polytechnic University) \/\/ <a href=\"mailto:yazikoveg@tpu.ru\">yazikoveg@tpu.ru<\/a><\/p>\n<p><strong>ROCK PERMEABILITY FACTORS AND THE APPLICATION OF INDUCTION LOGGING UNDER THE CONDITIONS OF URANIUM DEPOSITS OF BED OXIDATION ZONES FOR ORE MINING (ON THE EXAMPLE OF CHU-SARYSUY PROVINCE)<\/strong><\/p>\n<p><strong>\u00a0<\/strong>The article presents the prospects for the use of induction logging, taking into account rock permeability factors, to assess the active thickness of ore-bearing rocks in hydrogenous uranium deposits (using the example of the Inkai Chu-Sarysu province). The article substantiates the effectiveness of induction logging as a standard method for monitoring the hydrodynamics of leaching solutions. The use of the method at the stage of development of hydrogenous deposits makes it possible to accurately determine the change in the active power of the technological unit, which increases the efficiency of mining ore deposits.<\/p>\n<p><strong>Keywords:<\/strong> reservoir permeability, in-situ leaching method, active power, induction logging, hydrogenous uranium deposits, block active power control.<\/p>\n<p>&nbsp;<\/p>\n<p>\u0420. 26-32<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<p>DOI: 10.53085\/0034-026X_2023_07_33<\/p>\n<p>\u0423\u0414\u041a 553.776<\/p>\n<p>Kuzmenko P.S. (VIMS) \/\/ <a href=\"mailto:kuzmenko@vims-geo.ru\">kuzmenko@vims-geo.ru<\/a><\/p>\n<p>Chmerev V.S. (VIMS) \/\/ <a href=\"mailto:v_chmerev@vims-geo.ru\">v_chmerev@vims-geo.ru<\/a><\/p>\n<p>Mikheeva E.D. (VIMS) \/\/ <a href=\"mailto:galsuta@rambler.ru\">galsuta@rambler.ru<\/a><\/p>\n<p><strong>CONDITIONS OF FORMATION AND PATTERNS OF DISTRIBUTION OF LITHIUM-BEARING BRINES ON THE TERRITORY OF THE RUSSIAN FEDERATION<\/strong><\/p>\n<p>The work is aimed at substantiating a new geological and industrial type \u2014 deposits of underground lithium-bearing brines (brines \u2014 complex (Li, Rb, Cz, Br, I, Mg)) forecasting and allocation of prospecting areas for lithium hydromineral raw materials.<\/p>\n<p><strong>Keywords:<\/strong> lithium, hydromineral raw materials, brines, multicomponent brines, associated waters of oil fields, halogen formations.<\/p>\n<p>&nbsp;<\/p>\n<p>\u0420. 33-46<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<p>DOI: 10.53085\/0034-026X_2023_07_46<\/p>\n<p>\u0423\u0414\u041a 339.13:661.834<\/p>\n<p>Boyarko G.Yu. (TPU, Tomsk) \/\/ <a href=\"mailto:gub@tpu.ru\">gub@tpu.ru<\/a><\/p>\n<p>Khatkov V.Yu. (Gazprom, St. Petersburg) \/\/ <a href=\"mailto:V.Khatkov@adm.gazprom.ru\">V.Khatkov@adm.gazprom.ru<\/a><\/p>\n<p>Bolsunovskaya L.M. (TPU, Tomsk) \/\/ <a href=\"mailto:bolsunovskl@tpu.ru\">bolsunovskl@tpu.ru<\/a><\/p>\n<p>Dibrov A.M. (TGASU, Tomsk) \/\/ <a href=\"mailto:dibrov5@yandex.ru\">dibrov5@yandex.ru<\/a><\/p>\n<p>Dibrova Yu.A. (TPU, Tomsk) \/\/ <a href=\"mailto:juliadib@yandex.ru\">juliadib@yandex.ru<\/a><\/p>\n<p><strong>RUSSIA LITHIUM PRODUCTS: SUPPLY AND DEMAND ISSUES<\/strong><\/p>\n<p>The state of the Russian lithium industry is very complex due to the complete absence of national production of lithium raw materials. A commercial transit import-export process flow of lithium products from the conversion of imported lithium carbonates into oxides for export was formed. Due to political sanctions in 2022, there was a decrease in the import volume, processing and lithium products\u2019 export, which complicated the work of the Russian lithium industry. Reconstruction of the national production of strategic lithium raw materials for the purpose of its import substitution is possible by putting into operation its hydro-mineral and mineral (spodumene) deposits.<\/p>\n<p><strong>Keywords:<\/strong> strategic raw materials, import dependence, lithium carbonates, import, lithium hydroxides, export, national projects.<\/p>\n<p>&nbsp;<\/p>\n<p>\u0420. 46-53<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<p>DOI: 10.53085\/0034-026X_2023_07_54<\/p>\n<p>\u0423\u0414\u041a 504.43, 504.064.2.001.18<\/p>\n<p>Zubkov A.A. (Joint stock company \u00abSiberian Chemical Combine\u00bb) \/\/ <a href=\"mailto:geomon97@mail.ru\">geomon97@mail.ru<\/a><\/p>\n<p>Zavediy T.Yu.\u00a0 (Joint stock company \u00abSiberian Chemical Combine\u00bb) \/\/ <a href=\"mailto:taras-zavedy@yandex.ru\">taras-zavedy@yandex.ru<\/a><\/p>\n<p>Kokorev O.N. (The Federal State Unitary Enterprise \u00abNational operator for radioactive waste management\u00bb the branch \u00abSeverskiy\u00bb) \/\/ <a href=\"mailto:kokorev.podzemgazprom@yandex.ru\">kokorev.podzemgazprom@yandex.ru<\/a><\/p>\n<p><strong>EVALUATION OF THE MIGRATION ABILITY OF TECHNOGENIC GAMMA-EMITTING RADIONUCLIDES BY GAMMA SPECTROMETRY IN OPERATIONAL <\/strong><strong>HORIZONS OF LIQUID RADIOACTIVE WASTE DEEP GEOLOGICAL REPOSITORIES OF THE BRANCH \u00abSEVERSKIY\u00bb OF THE FEDERAL STATE UNITARY ENTERPRISE \u00abNATIONAL OPERATOR FOR RADIOACTIVE WASTE MANAGEMENT\u00bb<\/strong><\/p>\n<p><strong>\u00a0<\/strong>The results of studies of the sorption properties of sedimentary rocks in relation to technogenic gamma-emitting radionuclides of fragmentation and activation origin by means of a comprehensive data analysis are presented. An assessment of the migration ability of technogenic gamma-emitting radionuclides is given. The research results were obtained by methods of geophysics and hydrogeochemistry as part of monitoring the state of the subsoil and underground structures (geotechnological monitoring).<\/p>\n<p><strong>Keywords:<\/strong> migration ability of technogenic gamma-emitting radionuclides, gamma spectrometry, geotechnological monitoring, sorption.<\/p>\n<p>&nbsp;<\/p>\n<p>\u0420. 54- 58<\/td>\n<\/tr>\n<tr>\n<td width=\"667\">\n<p>DOI: 10.53085\/0034-026X_2023_07_59<\/p>\n<p>\u0423\u0414\u041a 55:930.2 (575.1)<\/p>\n<p>Bakhtierzoda O.B. (Mirzo Ulugbek NUUz, Tashkent) \/\/ <a href=\"mailto:oybakht@gmail.com\">oybakht@gmail.com<\/a><\/p>\n<p><strong>ABOUT THE PROSPECTS OF GEOLOGICAL EXPLORATION IN UZBEKISTAN: UNPUBLISHED PAGES OF THE FIELD DIARIES OF ACADEMICIAN I.H. HAMRABAEVA<\/strong><\/p>\n<p>The article presents materials from previously unpublished dairy notes by the world famous Uzbek scientist \u2014 academician I.H. Khamrabaev implementation will solve not only the problems of industrial exploration, but also environmental.<\/p>\n<p><strong>\u00a0<\/strong><strong>Keywords:<\/strong> academician I.H. Khamrabaev, scientific legacy, unpublished notes, space geology, prospecting for rare materials, forecasting of earthquake.<\/p>\n<p>&nbsp;<\/p>\n<p>\u0420. 59-62<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<p><\/p>","protected":false},"excerpt":{"rendered":"<p>CONTENTS \u2116 07\/2023 DOI: 10.53085\/0034-026X_2023_07_03 \u0423\u0414\u041a 550.8 Shashorin B.N. (VIMS) \/\/ shashorin.boris@yadex.ru Makarov A.I. (VIMS) \/\/ vims@df.ru Suchkov A.V. (VIMS) \/\/ alexsandir@mail.ru MAGMATIC FRONT OF CONTINENTAL CRUST DECOMPRESSION AS ONE OF THE FACTORS OF METALLOGENIC CONTROL IN THE GEOLOGICAL PREDICTION OF POTENTIALLY ORE-BEARING FORMATIONS (ON THE EXAMPLE OF W-Sn- AND Au-U-ORE REGIONS OF NORTHERN KAZAKHSTAN) [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":8480,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[33],"tags":[],"class_list":["post-8481","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-33"],"acf":[],"_links":{"self":[{"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/posts\/8481","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=8481"}],"version-history":[{"count":3,"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/posts\/8481\/revisions"}],"predecessor-version":[{"id":8486,"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/posts\/8481\/revisions\/8486"}],"wp:featuredmedia":[{"embeddable":true,"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/media\/8480"}],"wp:attachment":[{"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/media?parent=8481"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/categories?post=8481"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/tags?post=8481"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}