{"title":"СHEMOSTRATIGRAPHY OF THE CARBONATE DEPOSITS OF THE KINTEREP FORMATION IN NORTHWESTERN SALAIR: FIRST DATA","authors":"N. Vetrova, E. Vetrov, E. Letnikova","doi":"10.20403/2078-0575-2022-2-10-23","DOIUrl":"https://doi.org/10.20403/2078-0575-2022-2-10-23","url":null,"abstract":"The results of geochemical, isotope-geochemical (Sr, C, O) surveys of the Kinterep Formation carbonate deposits of Northwestern Salair and U-Pb dating (LA-ICP-MS) of zircons were given. Carbonate rocks represented by pure limestones are characterized by normal values of δ18OSMOW from 19.8 to 23.8 ‰ and δ13 CPDB from –0.7 to +0.9, the isotopic composition of Sr (87Sr/86Sr ratio) varies in a narrow range from 0.708486 to 0.708582.Using Sr and C isotope chemostratigraphy and U-Pb dating of zircons, age limits (525-510 Ma) were determined for the formation time of carbonate deposits of the Kinterep Formation. The first data of isotope chemostratigraphy in combination with the results of geochronological studies made it possible to compare the limestones of the Kinterep Formation of Northwestern Salair with carbonate sections of Siberia and Central Asia.","PeriodicalId":52268,"journal":{"name":"Geology and Mineral Resources of Siberia","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2022-06-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"42262731","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}
{"title":"EXPERIENCE OF USING GEOTHERMAL ENERGY OF THE NEAR-SURFACE MASSIF OF ANCIENT GRANITOIDS FOR HEAT SUPPLY PURPOSES (SOUTH OF WEST SIBERIA)","authors":"A. Shevchenko, O. Skrobot","doi":"10.20403/2078-0575-2022-2-100-106","DOIUrl":"https://doi.org/10.20403/2078-0575-2022-2-100-106","url":null,"abstract":"An example of transition of the heating- and hot-water supply system to a low-temperature geothermal energy source from the Paleozoic granitoid massif is given for a secondary school building in Novosibirsk. The necessity for change the source of heat supply arose in 2018 due to wear and tear of the coal boiler house old equipment, which has provided the school with heat since it was built in 1964. At the time of the geothermal project implementation, there were already several cases of successful use of underground heat-producing probes arranged in specially drilled geothermal wells for heating public facilities in neighboring Siberian cities (Tomsk, Barnaul). However, loose sedimentary rocks there served for the source of heat energy, that greatly simplified and accelerated the tasks implementation. The described experience of heating – and hot-water supply of building due to the low energy from a shallow lying massif of ancient rocky grounds with intrusive genesis is unique for Russia and can serve as a platform for the implementation of geothermal projects in regions with complicated ground conditions and moderately cold climate.","PeriodicalId":52268,"journal":{"name":"Geology and Mineral Resources of Siberia","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2022-06-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"44282439","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}
{"title":"MOBILE FRACTION OF ELEMENTS IN TECHNOSOLS OF TAILINGS STORAGE FACILITY OF THE NERCHINSK POLYMETALLIC COMPLEX","authors":"B. V. Dampilova, S. G. Doroshkevich","doi":"10.20403/2078-0575-2022-2-62-67","DOIUrl":"https://doi.org/10.20403/2078-0575-2022-2-62-67","url":null,"abstract":"Contamination of soils adjacent to the tailings storage facility of the Nerchinsk Polymetallic Complex (East Transbaikalia) is caused by the behaviour of Aeolian processes in a dry sharply continental climate. The studied territory is characterized by a high gross content (mg/kg) of zinc up to 5000, arsenic up to 1400, lead up to 600, cadmium up to 36, antimony up to 30. The method of sequential extraction in static mode was used to determine the ion-exchange water- and acid-soluble, reducible, oxidizable, residual forms of elements. The elements of physical-chemical mobility and bioavailability are arranged in the following series according to their decreasing sequence Zn>Mn>Pb>Ni>Cu>As>Fe. The rhizosphere (root zone) of plants is characterized by the content of oxidized forms of copper, zinc, lead and hard-to-reach forms of arsenic, iron, nickel exceeding that in technosols.","PeriodicalId":52268,"journal":{"name":"Geology and Mineral Resources of Siberia","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2022-06-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"46222943","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}
{"title":"NEW FINDINGS OF BIODEGRADED NAPHTHIDES IN ROCKS OF THE VENDIAN KHATYSPYT FORMATION OF THE OLENEK UPLIFT","authors":"D. S. Melnik","doi":"10.20403/2078-0575-2022-2-48-56","DOIUrl":"https://doi.org/10.20403/2078-0575-2022-2-48-56","url":null,"abstract":"The geochemistry of organic matter (OM) and rocks from new sections of the Vendian Khatyspyt Formation on the Olenek uplift has been studied. The analysis of bitumens revealed signs of deep biodegradation of saturated hydrocarbons (HCs), demethylated terpanes in six samples. The present work is aimed at identifying the composition features of the OM components from rocks, containing biodegraded bitumens and assessing the Khatyspyt Formation rocks as potentially source ones. It was found that the rocks are enriched with OM, which accumulated under reducing conditions with possible sulphurous contamination of near–bottom waters, the water column was stratified. Its maturity on the Olenek Uplift corresponds to the initial stages of mesocatagenesis (the early oil window), it could generate naphthides. Comparative molecular analysis of saturated HCs showed that the source of biodegraded bitumens was represented by the dispersed OM of the Khatyspyt Formation. The peculiarities of HCs distribution indicate several stages of primary migration of bitumens. It is assumed that not only potentially oil source rocks can be distributed in the Khatyspyt Formation, but also rocks that are re-enriched with naphthides.","PeriodicalId":52268,"journal":{"name":"Geology and Mineral Resources of Siberia","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2022-06-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"43968694","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}
{"title":"CALCULATIONS OF DATUM STATICS IN REFLECTION METHOD WITH CONSIDERATION TO THE POSITION OF THE CHARGE RELATIVE TO THE BASE OF LOWVELOCITY LAYER","authors":"A. P. Sysoev, A. A. Shamordin","doi":"10.20403/2078-0575-2022-2-57-61","DOIUrl":"https://doi.org/10.20403/2078-0575-2022-2-57-61","url":null,"abstract":"While processing ground-based seismic operations by the reflection method using an explosive excitation source, the standard method of compensation technique for the inhomogeneity of the low velocity layer (LVL) is based on the use of blastholes parameters: shot depth, TSP and velocity of underlying stratum, determined by the apparent velocity of refracted wave. The necessary condition for the applicability of this method is the arrangement of the charge below the base of the LVL. Therefore, to substatiate this method, it is necessary to evaluate the position of the charge relative to the roof of the LWL for each source. If the necessary condition for calculating statics computations is not met, it is necessary to solve the problem of estimating the LVL’s thickness and velocity. The presented work contains the problem of analyzing the position of the charge relative to the LVL’s position and estimating the layer parameters which is solving on the basis of joint analysis of the parameters of wells and wave refracted on the LVL base. The solution of the problem is illustrated by the example of real data processing.","PeriodicalId":52268,"journal":{"name":"Geology and Mineral Resources of Siberia","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2022-06-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"48134202","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}
{"title":"GENESIS OF GRANITOID (GABBRO-GRANITE) PLUTONS AND ASSOCIATED MINERALIZATION","authors":"V. L. Khomichev","doi":"10.20403/2078-0575-2022-2-78-87","DOIUrl":"https://doi.org/10.20403/2078-0575-2022-2-78-87","url":null,"abstract":"Deep geological and geophysical modeling by a large number of granitoid plutons for the first time showed a completely different nature than was commonly believed. As a result, ideas about the connection of mineralization with them have changed dramatically. Many petrological contradictions and puzzles were solved logically and scientifically grounded. The complete and comprehensive review of the problem from the beginning (source of the initial magma) to the end (formation of the granite ore-magmatic system) is given. Three stages of the volatiles and ore matter concentration in the history of the plutons formation were established: the first (planetary) - during the intrachamber differentiation of the initial basalt magma with an isolation of granitoid melting; the second (regional) - during the formation of a residual leukogranite chamber the third, main (local) - during the intrusion of ore-generating apophyses from the chamber.","PeriodicalId":52268,"journal":{"name":"Geology and Mineral Resources of Siberia","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2022-06-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"45714913","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}
{"title":"SILVER MINERALIZATION OF THE KHOROGOCHI MOTHER LODE (STANOVAYA GRANITE-GREENSTONE AREA, UPPER AMUR REGION)","authors":"P. P. Safronov, N. V. Moiseenko","doi":"10.20403/2078-0575-2022-1-80-91","DOIUrl":"https://doi.org/10.20403/2078-0575-2022-1-80-91","url":null,"abstract":"The morphology and chemical composition of minerals of the Khorogochi silver ore occurrence (Upper Amur region) were studied by the analytical scanning electron microscopy. The mineral association is represented by high-grade native silver, basically silver minerals (silver sulphide, sulphoantimonites and silver sulfoarsenides), Ag-containing (fahl ore and galenite), as well as a number of associated minerals (pyrite, chalcopyrite, sphalerite, loellingite, ankerite, hydromica-smectite, etc.). Based on the revealed chemical composition of silver minerals and associated minerals, the features of their spatial relationship, as well as experimental data known from the literature on the resistance of silver-containing systems, the formation temperatures of silver mineralization, which fit into the range of 300–100 oC, and the order of crystallization of its constituent minerals were estimated – from multicomponent compositions with a low silver content (Agtennantite-tetrahedrite, proustite) to compositions with a high content of noble metal (stephanite, polybasite, pearceite, acanthite, native silver). The ore body of silver mineralization in the ore-placer cluster Khorogochi-2 is spatially dissociated from the ore sources of gold-silver mineralization.","PeriodicalId":52268,"journal":{"name":"Geology and Mineral Resources of Siberia","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2022-03-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"48556922","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}
A. P. Obolkin, V. S. Sintnikov, M. I. Sleptsova, R. F. Sevostyanova
{"title":"STUDY OF POSSIBLE MANIFESTATION OF THE SOUTH ANYUY SUTURE IN THE SEISMIC WAVE FIELD AT THE BASE OF THE TASTAKH TROUGH IN THE NORTHEASTERN YAKUTIA","authors":"A. P. Obolkin, V. S. Sintnikov, M. I. Sleptsova, R. F. Sevostyanova","doi":"10.20403/2078-0575-2022-1-57-62","DOIUrl":"https://doi.org/10.20403/2078-0575-2022-1-57-62","url":null,"abstract":"The material analysis of the СDP seismic survey works in the Tastakh trough of the northeastern Yakutia carried out in 1989–1993 was conducted, reinterpretation of data was made. At the trough base, a rift–type seismofacial complex characterizing the proposed western segment of the South Anyuy suture was distinguished.","PeriodicalId":52268,"journal":{"name":"Geology and Mineral Resources of Siberia","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2022-03-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"46855791","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}
S. I. Golyshev, P. Sobolev, N. L. Padalko, S. I. Dykhan, P. F. Yavorov, M. I. Prazdnichnykh, E. V. Chernikov
{"title":"ISOTOPIC AND GEOCHEMICAL SURVEY OF POTENTIALLY OIL-AND-GAS SOURCE DEPOSITS OF THE RIPHEAN IN THE SOUTH-EAST OF THE SIBERIAN PLATFORM","authors":"S. I. Golyshev, P. Sobolev, N. L. Padalko, S. I. Dykhan, P. F. Yavorov, M. I. Prazdnichnykh, E. V. Chernikov","doi":"10.20403/2078-0575-2022-1-48-56","DOIUrl":"https://doi.org/10.20403/2078-0575-2022-1-48-56","url":null,"abstract":"Based on the study of the carbon and oxygen isotopic composition of the carbonate constituent of rocks (CCR) and carbon of dispersed organic matter (DOM), the facies conditions of sedimentation of the Middle Riphean Totinskaya and Malginskaya formations and Lakhandinian series of the Upper Riphean in the southeast of the Siberian Platform were revealed. The main isotopic criteria of the Middle Riphean domanicoid formation within the Aldan-Maya sedimentary basin of the Siberian Platform have been determined. The exogenous and endogenous factors necessary for the formation of domanicoid deposits of the Malginskaya Formation are considered. A mechanism leading to the formation of abnormally low 13C content in the Middle and Upper Riphean sediments with a range of –33.0...–35.0 ‰ is proposed. On the basis of isotopic data potentially-enable source-bed horizons within the Aldan-Maya depression are examined.","PeriodicalId":52268,"journal":{"name":"Geology and Mineral Resources of Siberia","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2022-03-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"41739567","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}
{"title":"NEW DATA ON BIOSTRATIGRAPHY AND FORAMINIFERA OF THE TURONIAN STAGE OF WEST SIBERIA","authors":"V. Podobina","doi":"10.20403/2078-0575-2022-1-3-13","DOIUrl":"https://doi.org/10.20403/2078-0575-2022-1-3-13","url":null,"abstract":"The northern paleobiogeographic region of West Siberia is characterized by studied new sections of the Turonian – the Upper stage of the Middle series of the Cretaceous System. Two widespread foraminifera complexes have been determined in the section of the Kuznetsovsky Horizon, attributed to the Turonian: the lower one with Gaudryinopsis angustus and the upper one with Pseudoclavulina hastata. New data on the upper half of the Kuznetsovsky Horizon with the second of these foraminifera complexes offered an opportunity to clarify the position of the boundary layers of the Middle Cretaceous with the Upper (Coniac-Maastricht) series of the Cretaceous System.","PeriodicalId":52268,"journal":{"name":"Geology and Mineral Resources of Siberia","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2022-03-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"49126923","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}