Geology and Mineral Resources of Siberia最新文献_第4页

THE KOUNRADSKY MINE TAILINGS CEMENTING LAYER THAT PREVENTS DEFLATION: MINERAL COMPOSITION, GEOCHEMICAL FEATURES 孔拉茨基尾矿防缩胶结层:矿物组成、地球化学特征

Geology and Mineral Resources of Siberia Pub Date : 2023-01-01 DOI: 10.20403/2078-0575-2023-2-68-80

E. Lazareva, V. V. Litvinov, D. A. Aytekenova, I. N. Myagkaya, I. Kirichenko

{"title":"THE KOUNRADSKY MINE TAILINGS CEMENTING LAYER THAT PREVENTS DEFLATION: MINERAL COMPOSITION, GEOCHEMICAL FEATURES","authors":"E. Lazareva, V. V. Litvinov, D. A. Aytekenova, I. N. Myagkaya, I. Kirichenko","doi":"10.20403/2078-0575-2023-2-68-80","DOIUrl":"https://doi.org/10.20403/2078-0575-2023-2-68-80","url":null,"abstract":"The paper is devoted to the study of composition of the surface matter of the man-made mineral formation (MMMF), namely, tailings of the Kounradsky mine (Konyrat, Karaganda region, the Republic of Kazakhstan), and the comparison of its geochemical characteristics with the composition of aerosols. The deposit is located in an arid area of steppe zone, which is characterized by wind-formed processes, therefore, an assessment of the degree of exposure of tailing substance to them is one of the important geoecological tasks. Most of the surface of the MMMF tailings of the Kounradsky mine is composed of coarse-grained material. At the sampling points the fraction content greater 1 mm amounted to 58.7–82.5%. The moisture content for the sampling period ranged from 1.9% to 4%. It is shown that the process of an oxidation leaching of sulphide-containing substance of MMMF led to the formation of acid sulphate detached waters, which dry out quickly in dry climates, that brings about the formation of sulphate efflorescences on the surface of tailings and cementing layer. It has been determined that cement is a complex and consists of newly formed kaolinite and/or illite, jarosite, gypsum and water-soluble sulphates of Fe, Ca, Al, Mg, Na and Cu. Comparison of geochemical characteristics of aerosols collected directly at tailings and at the background point with geochemical characteristics of MMMF of the Kounradsky mine shows that today tailings are not a source of air pollutants. The source of high concentrations of Pb, Cu, Zn, As, Se, Ad, Cd in aerosols recorded at one of the points is industrial enterprises of Balkhash.","PeriodicalId":52268,"journal":{"name":"Geology and Mineral Resources of Siberia","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"68427445","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

TYPES OF GOLD-POLYMETAL MINERALIZATION IN PRECAMBRIAN ROCKS OF THE NIMNYR TERRANE OF THE ALDAN-STANOVOY SHIELD (SOUTH OF THE NORTH ASIAN CRATON) 北亚克拉通南缘阿尔丹—斯坦诺沃伊盾宁尼尔地体前寒武纪岩石金多金属成矿类型

Geology and Mineral Resources of Siberia Pub Date : 2023-01-01 DOI: 10.20403/2078-0575-2023-1-50-60

A. A. Kravchenko, G. Anisimova, V. Berezkin, N. Popov, E. Loskutov, A. Zhuravlev, Z. Nikiforova

{"title":"TYPES OF GOLD-POLYMETAL MINERALIZATION IN PRECAMBRIAN ROCKS OF THE NIMNYR TERRANE OF THE ALDAN-STANOVOY SHIELD (SOUTH OF THE NORTH ASIAN CRATON)","authors":"A. A. Kravchenko, G. Anisimova, V. Berezkin, N. Popov, E. Loskutov, A. Zhuravlev, Z. Nikiforova","doi":"10.20403/2078-0575-2023-1-50-60","DOIUrl":"https://doi.org/10.20403/2078-0575-2023-1-50-60","url":null,"abstract":"The study of material composition of the Early Precambrian continental earth crust contributes to the identification of its metallogeny. Deposits of graphite, phlogopite, and iron have been discovered in the Paleoproterozoic granulite complexes of the Aldan-Stanovoy Shield on the southern margin of the North Asian Craton, and the first gold deposit has recently been discovered. Deposits are confined to the extended boundary of the infra- and supracrustal complexes within which multistage deformations, intense metasomatosis and metamorphism of various facies are observed. Modern methods of microanalysis allow scientists to significantly supplement data on the mineral composition of deposits, characterize conditions of their formation and make a comparison. The paper considers the geological structure of granulite complexes of the central part of the Aldan-Stanovoy Shield and ore mineralization in graphite-bearing quartzites, phlogopite-containing skarns, gold-bearing crystalline shales and diaphthorites. Ore and wallrock mineral associations have been identified. The comparison was made with well-studied ore deposits near the border of the Karelian Craton. The types of mineralization and directions of comparative metallogenic analysis are discussed.","PeriodicalId":52268,"journal":{"name":"Geology and Mineral Resources of Siberia","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"68426108","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

KARA GOLD ORE CLUSTER (EASTERN TRANSBAIKALIA): GEOCHEMICAL FEATURES OF ORES, THE RELATIONSHIP OF MAGMATISM WITH MINERALIZATION 卡拉金矿群(东跨贝加尔湖):矿石地球化学特征及岩浆作用与成矿关系

Geology and Mineral Resources of Siberia Pub Date : 2023-01-01 DOI: 10.20403/2078-0575-2023-1-61-67

B. Abramov

{"title":"KARA GOLD ORE CLUSTER (EASTERN TRANSBAIKALIA): GEOCHEMICAL FEATURES OF ORES, THE RELATIONSHIP OF MAGMATISM WITH MINERALIZATION","authors":"B. Abramov","doi":"10.20403/2078-0575-2023-1-61-67","DOIUrl":"https://doi.org/10.20403/2078-0575-2023-1-61-67","url":null,"abstract":"Dykes of the Amudzhikano-Sretenskiy complex (J3–K1) including hybrid porphyries are widely developed in the area of the Kara gold ore cluster. The parameters of the lanthanides distribution in them are close to those of ores of the quartz-tourmaline-pyrite association, indicating probable single sources of their formation. In hybrid porphyries, ΣTR is 52.24–123.35; in ores of the quartz-tourmaline-pyrite association ΣTR is 52.82–133.78. In hybrid porphyries, Eu/Sm is 0.18–0.65; in ores of the quartz-tourmaline-pyrite association Eu/Sm is 0.18–0.47. The degree of differentiation of magmatic chambers according to Eu/Eu* is 0.61-2.26 in dikes of hybrid porphyries; Eu/Eu* is 0.78–1.49 in ores of quartz-tourmaline-pyrite association. The represented data indicate that their magmatic chambers of dikes of hybrid porphyries and quartz-tourmaline-pyrite ores were not differentiated and, consequently, had a deep source. According to the geochemical composition, part of the Amudzhikano-Sretenskiy complex granite values corresponds to ore-bearing granites with goldmolybdenum mineralization. Ores of the actinolite-magnetite association are characterized by the highest gold contents among productive stages of gold mineralization. Close correlation relationships of Au with Zn, W, Mo were established in ores of the actinolite-magnetite association; in ores of the quartz-tourmaline-pyrite association – with Mo, Pb; in ores of the quartz-arsenopyrite association – with Pb, Mo, As, Ag.","PeriodicalId":52268,"journal":{"name":"Geology and Mineral Resources of Siberia","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"68426127","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

RESULTS OF PALYNOLOGICAL AND PALEOCARPOLOGICAL ANALYSES OF THE LATE NEOPLEISTOCENE INTERGLACIAL AND PERIGLACIAL DEPOSITS (EAST TYVA HIGHLANDS, SERLIGKHEM INTERMOUNTAIN BASIN) 晚新新世间冰期和冰缘沉积物(东tyva高地、serligkhem山间盆地)孢粉学和古人类学分析结果

Geology and Mineral Resources of Siberia Pub Date : 2023-01-01 DOI: 10.20403/2078-0575-2023-2-3-9

M. Mikharevich, S. G. Prudnikov

{"title":"RESULTS OF PALYNOLOGICAL AND PALEOCARPOLOGICAL ANALYSES OF THE LATE NEOPLEISTOCENE INTERGLACIAL AND PERIGLACIAL DEPOSITS (EAST TYVA HIGHLANDS, SERLIGKHEM INTERMOUNTAIN BASIN)","authors":"M. Mikharevich, S. G. Prudnikov","doi":"10.20403/2078-0575-2023-2-3-9","DOIUrl":"https://doi.org/10.20403/2078-0575-2023-2-3-9","url":null,"abstract":"The last Late Pleistocene glaciation deposits of the tongue-like basin, as well as an interglacial alluvium overlapped by glaciofluvial have been studied on the basis of application of palynological and paleocarpological methods of analysis in the basin of the middle course of the Yenisei River. The tongue-like basin deposits were compared with those previously studied by researchers in headwaters of the Kharal River (Azas glacial complex), formed according to OSL dates in the interval of the end of MIS-3–MIS-2. Fluvioglacial overlapping an interglacial alluvium is compared with the same glacial complex. A rather large scattering of absolute dates, some of which fall within the last Neopleistocene thermochron, palynological and paleocarpological complexes from glacial deposits characterizing the stage of glaciation degradation, raise the question of independence of the second Late Neopleistocene one. Further geochronological study of the interglacial alluvium section is proposed to clarify the lower time boundary of the Azas shield glacier.","PeriodicalId":52268,"journal":{"name":"Geology and Mineral Resources of Siberia","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"68426718","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

THERE HAVE NOT BEEN UNIVERSAL CATASTROPHES ON EARTH AND THERE WILL NOT BE 地球上没有普遍的灾难，将来也不会有

Geology and Mineral Resources of Siberia Pub Date : 2023-01-01 DOI: 10.20403/2078-0575-2023-1-85-92

V. L. Khomichev

引用次数: 0

ANALYTICAL SOLUTIONS TO THE PROBLEMS OF COMPENSATION OF NEAR-SURFACE HETEROGENEITY IN SEISMIC EXPLORATION USING SEISMIC REFLECTION METHOD 地震反射法补偿地震勘探中近地表非均质性问题的解析解

Geology and Mineral Resources of Siberia Pub Date : 2023-01-01 DOI: 10.20403/2078-0575-2023-1-36-43

A. Sysoev

{"title":"ANALYTICAL SOLUTIONS TO THE PROBLEMS OF COMPENSATION OF NEAR-SURFACE HETEROGENEITY IN SEISMIC EXPLORATION USING SEISMIC REFLECTION METHOD","authors":"A. Sysoev","doi":"10.20403/2078-0575-2023-1-36-43","DOIUrl":"https://doi.org/10.20403/2078-0575-2023-1-36-43","url":null,"abstract":"The solution of the problem of compensation of the near-surface heterogeneity (NSH) is an obligatory component of the digital processing technology of CDP data. The main result in the theory of solving this problem was determined by the equation of the normal traveltime curve of the common mid point with an additive component describing static corrections at the points of shotpoint and geophone. The substantiation of methods for compensation of heterogeneity based on the structure of high-speed model of the NSH is carried out in the present paper. Three variants of the NSH model corresponding to the zone of low velocities, heterogeneity of underlying bedrock deposits and variable relief of daytime surface are considered. The research subject is analytical methods for solving the problem of field continuation aimed at eliminating the influence of NSH on the kinematic parameters of wave field: method of static corrections and parametric method. Applications of methods are determined by the ratio of near-surface section velocities and underlying deposits. The requirements to the methodology of field observations and digital data processing ensuring the uniqueness of problem solution are considered for the compensation problem of heterogeneity of low-velocity zone.","PeriodicalId":52268,"journal":{"name":"Geology and Mineral Resources of Siberia","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"68426198","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

GEOCHEMISTRY OF RARE EARTH ELEMENTS IN ALLANITE OF THE DANILOVSKOYE MANIFESTATION OF THE GORNYI ALTAI 高尔尼阿尔泰达尼洛夫斯科耶表现allanite中稀土元素地球化学

Geology and Mineral Resources of Siberia Pub Date : 2023-01-01 DOI: 10.20403/2078-0575-2023-1-68-75

A. Gusev

{"title":"GEOCHEMISTRY OF RARE EARTH ELEMENTS IN ALLANITE OF THE DANILOVSKOYE MANIFESTATION OF THE GORNYI ALTAI","authors":"A. Gusev","doi":"10.20403/2078-0575-2023-1-68-75","DOIUrl":"https://doi.org/10.20403/2078-0575-2023-1-68-75","url":null,"abstract":"Data are given on the geochemical pecularities and composition of allanite of the Danilovskoye pegmatite manifestation belonging to the Nb > Ta-Y-F (NYF) family and allanite (orthite)-monazite type enriched with light rare earth elements (REE). Allanite occurs in the large-block part and micropegmatite fringe of zonal pegmatites and it is closely associated with hydroxyl-containing minerals- muscovite, zoisite. Total concentrations of rare earth elements in mineral vary from 182163 to 189046 g/t. It is also characterized by increased contents of Ti, Y, Th, U, Mn. High ratios (La/Yb)N (from 278 to 375.7) indicate a highly diff erentiated type of REE distribution. The tetradic effect of the W-type REE fractionation in allanite is due to abnormal conditions of its crystallization at the transition stage to water enrichment of fluids and an increased alkaline regime of the mineral formation medium. This process contributed to manifestation of the effect of nonсonformity to charge-radius behavior of chemical elements during crystallization of allanite. Abundant mineral secretions contributed to its accumulation in placers of some rivers together with monazite.","PeriodicalId":52268,"journal":{"name":"Geology and Mineral Resources of Siberia","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"68426177","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

FORMS OF MIGRATION OF CHEMICAL ELEMENTS IN RADON WATERS IN THE SOUTH OF SIBERIA 西伯利亚南部氡水中化学元素的迁移形式

Geology and Mineral Resources of Siberia Pub Date : 2023-01-01 DOI: 10.20403/2078-0575-2023-2-81-90

A. N. Nikitenkov, D. A. Novikov, T. V. Korneeva

{"title":"FORMS OF MIGRATION OF CHEMICAL ELEMENTS IN RADON WATERS IN THE SOUTH OF SIBERIA","authors":"A. N. Nikitenkov, D. A. Novikov, T. V. Korneeva","doi":"10.20403/2078-0575-2023-2-81-90","DOIUrl":"https://doi.org/10.20403/2078-0575-2023-2-81-90","url":null,"abstract":"The paper presents the first results of thermodynamic modeling of the chemical elements migration forms in radon waters of southern Siberia. It was determined that Ca, Mg, Na, K, Mn, as well as, Fe (at nearneutral pH) migrates in the form of free ions, the proportion of which in most cases is more than 90%. Among the complex forms of migration of trace elements, as well as U and Th, associates prevail with a participation of dominant anions HCO3 –, CO3 2–, compounds with Cl– ions are less common. Hydroxide and oxide coordination compounds play a significant role in the migration of Al, as well as Si, U and Th (reaching tens of % of gross content). In oxidizing environment, uranium migrates predominantly in the form of carbonate compounds, in a reducing environment – in the form of oxides and hydroxide ions. The proportion of samples with hydroxide forms decreases with an increase in pH value by more than 8.5, and the proportion of oxide forms increases. Thorium in the studied radon waters migrates mainly in the form of carbonate compounds, namely in the form of (ThCO3(OH)3)–, which accounts for more than 90% in most samples. Its decrease to values of about 60% is typical for slightly acidic waters with a pH of less than 6.5.","PeriodicalId":52268,"journal":{"name":"Geology and Mineral Resources of Siberia","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"68427065","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

CONSTRUCTION OF THE HIGH-VELOCITY MODEL OF THE EARTH’S UPPER CRUST OF THE EURASIAN AND OKHOTSK SEA PLATES CONJUNCTION ZONE ALONG THE NORTH-EASTERN SEGMENT OF THE 3-DV PROFILE BASED ON THE RESULTS OF DIGITAL PROCESSING OF COMPRESSIONAL- AND SHEAR-WAVE REFRACTIONS 基于纵波和横波折射数字处理结果的3-dv剖面东北段欧亚-鄂霍次克海板块接合带上地壳高速模型的构建

Geology and Mineral Resources of Siberia Pub Date : 2023-01-01 DOI: 10.20403/2078-0575-2023-1-21-35

P. O. Polyanskiy, A. F. Emanov, A. S. Salnikov

{"title":"CONSTRUCTION OF THE HIGH-VELOCITY MODEL OF THE EARTH’S UPPER CRUST OF THE EURASIAN AND OKHOTSK SEA PLATES CONJUNCTION ZONE ALONG THE NORTH-EASTERN SEGMENT OF THE 3-DV PROFILE BASED ON THE RESULTS OF DIGITAL PROCESSING OF COMPRESSIONAL- AND SHEAR-WAVE REFRACTIONS","authors":"P. O. Polyanskiy, A. F. Emanov, A. S. Salnikov","doi":"10.20403/2078-0575-2023-1-21-35","DOIUrl":"https://doi.org/10.20403/2078-0575-2023-1-21-35","url":null,"abstract":"An automated algorithm for monitoring the areas of refraction event tracking along the profile based on the dynamic conversion method is developed. Time sections of compressional - and shear-wave refractions recorded by the CDP shooting geometry on the North-Eastern segment of the 3DV survey base line are constructed. A high-speed model of the upper part of the Earth’s crust is constructed to depths of ≈2 km in the conjunction zone of the Okhotsk and Eurasian lithospheric plates. According to increased values of the velocity ratio of P- and S- waves, it is found that refracting boundaries in the Ayan-Yuryakh block are sections of rocks with various lithological composition in sedimentary cover. The zone of reduced values of P-wave velocity and the VP /Vs ratio associated with a high fragmentation of rocks is identified on the high-velocity profile of the Chay-Yurya fault zone, both above and below the refracting boundary. The velocity values of P- and S-waves (6.0–6.1 km/s and 3.6–3.7 km/s, respectively,) and reduced values of the Vp /Vs ratio (≈1.65) concerned with intrusions of acid rocks were recorded in the southern part of the Inyali-Debin block within t he depth range of 1–1.5 km.","PeriodicalId":52268,"journal":{"name":"Geology and Mineral Resources of Siberia","volume":"2020 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"136218141","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

THE ROLE OF ANCIENT KARST IN THE FORMATION OF URANIUM DEPOSIT (GORNAYA SHORIYA) 古岩溶在铀矿床形成中的作用(gornaya shoriya)

Geology and Mineral Resources of Siberia Pub Date : 2022-12-01 DOI: 10.20403/2078-0575-2022-4-85-94

E. Golovina, A. V. Grebneva

{"title":"THE ROLE OF ANCIENT KARST IN THE FORMATION OF URANIUM DEPOSIT (GORNAYA SHORIYA)","authors":"E. Golovina, A. V. Grebneva","doi":"10.20403/2078-0575-2022-4-85-94","DOIUrl":"https://doi.org/10.20403/2078-0575-2022-4-85-94","url":null,"abstract":"At the present time, drinking groundwater that is reliably protected from contamination should be considered as a priority source of utility and drinking water supply to the population. These waters undoubtedly belong to strategic types of natural resources, since they are essentially the only source of drinking water supply during emergencies, and the possibility of their use significantly affects the national security of the country. The current geopolitical situation around the Russian Federation dictates the need to consider the issue of managing transboundary resources of groundwater in the context of international legislative conventions and treaties in a new format, allocating groundwater to a separate block of strategic resources, the extraction of which occurs in frontier territories. The paper presents the analysis of the groundwater extraction quantitative evoluation at the largest water intake facilities of the Kaliningrad Region located on a transboundary territory using the balance calculation method. The method of balance approach, based on calculations of the so-called intake of water resources from the territory of neighboring state, allows for adjusting the activities of the intakes themselves and their further design taking into account boundary factors when approving maximum level decreases at observation points.","PeriodicalId":52268,"journal":{"name":"Geology and Mineral Resources of Siberia","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2022-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"47048815","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