A. V. Tevelev, A. Borisenko, I. Sobolev, A. Kazansky, N. Pravikova, E. V. Kopte, E. A. Volodina, V. Chervyakovskiy
{"title":"The areas of manifestation of the Intravisean orogeny in the Eastern Zones of the Southern Urals (According to the detrital zircons U-Pb dating data from the Solnechnaya Formation of the Upper Visean)","authors":"A. V. Tevelev, A. Borisenko, I. Sobolev, A. Kazansky, N. Pravikova, E. V. Kopte, E. A. Volodina, V. Chervyakovskiy","doi":"10.33623/0579-9406-2022-5-47-56","DOIUrl":"https://doi.org/10.33623/0579-9406-2022-5-47-56","url":null,"abstract":"The aim of this work is to determine the provenance for the Upper Visean Solnechnay formation (The Southern Urals) using the U-Pb dating of detrital zircons. 138 zircon grains with discordance range of ± 10% were selected for the analysis. The vast majority of the zircons yielded the Ordovician and Cambrian ages. The main peak corresponds to the beginning of the Ordovician period (circa 480 Ma), and the secondary peaks correspond to the beginning of the Late Ordovician, the middle Cambrian, and the early Cambrian. The clastic material was derived from the East Ural megazone exclusively.","PeriodicalId":253271,"journal":{"name":"Moscow University Bulletin. Series 4. Geology","volume":"3 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-12-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"134634323","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":"Physical modeling of the interaction between the spreading ridge and the large Kerguelen igneous province","authors":"G. Agranov, E. Dubinin, A. Grokholsky","doi":"10.33623/0579-9406-2022-5-19-27","DOIUrl":"https://doi.org/10.33623/0579-9406-2022-5-19-27","url":null,"abstract":"The problem of the interaction of spreading ridges with large igneous provinces is widely discussed in the scientific literature. The most striking and well-preserved example of such interaction in the geological past is the “collision” of the Southeast Indian spreading ridge and the Kerguelen plateau, which occurred about 43 Maago. The consequence of this event was the division of a single Kerguelen plateau into two parts: in fact, the Kerguelen plateau and the Broken ridge. The conditions for the formation of these morphostructures were studied experimentally. The paper presents the results of modeling the interaction of a spreading ridge with a large igneous province. The experimental results correlate well with geological and geophysical data and with the proposed model for the development of this region.","PeriodicalId":253271,"journal":{"name":"Moscow University Bulletin. Series 4. Geology","volume":"77 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-12-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"131102438","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}
T. Lubkova, O. Lipatnikova, O. R. Filatova, I. V. Balykova
{"title":"X-ray fluorescence analysis of sulfate-ion in aqueous solutions by dried drop technique using a portable spectrometer","authors":"T. Lubkova, O. Lipatnikova, O. R. Filatova, I. V. Balykova","doi":"10.33623/0579-9406-2022-2-59-67","DOIUrl":"https://doi.org/10.33623/0579-9406-2022-2-59-67","url":null,"abstract":"In this paper authors propose the methodology of X-ray fluorescence determination of sulfate-ion in aqueous solutions with preconcentration by dried drop technique using portable energy dispersive spectrometer NITON FXL 959 GOLDD+. The represented measuring procedure has been tested in a wide range of sulfate-ion concentrations (10–4200 mg/l) during exploration the groundwater samples of the Over Jurassic Aquifer complex of the Moscow region and drainage water of the sulfide porphyry-copper mineralization of the Nakhodka ore field (Western Chukotka). Verification of the measuring procedure is based on results of the water investigation by ion chromatography and titration methods.","PeriodicalId":253271,"journal":{"name":"Moscow University Bulletin. Series 4. Geology","volume":"6 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-12-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"123884002","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}
L. Lyamina, N. Kharitonova, A. Rastorguev, G. Chelnokov, I. Bragin
{"title":"Conceptual model of the formation of nitrogen thermal waters in crystalline rock massifs (example of the Kuldur Spa)","authors":"L. Lyamina, N. Kharitonova, A. Rastorguev, G. Chelnokov, I. Bragin","doi":"10.33623/0579-9406-2022-2-78-90","DOIUrl":"https://doi.org/10.33623/0579-9406-2022-2-78-90","url":null,"abstract":"The study of the influence of hydrodynamic factors on the occurrence of nitrogen thermal waters in crystalline massifs, by the example of the Kuldur field, is presented in the article. The results of two-dimensional modeling (based on FEFLOW code) of several variants of formation and circulation of therms in the study area are considered. Model parameters included temperature (130–140 °C), calculated on the basis of geothermometers, and the residence time of waters in the rock massif (68 800–254 000 years), estimated by means of 14C and 4He dating. The modeling results show that exactly the filtration parameters of the granite massif are the main factor controlling the dynamics of fluid movement and, consequently, the relative age of thermal waters. It is also found that the filtration characteristics of the fault zone have a significant influence on the temperature of thermal water discharge.","PeriodicalId":253271,"journal":{"name":"Moscow University Bulletin. Series 4. Geology","volume":"67 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-12-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"127163357","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}
I. O. Krylov, I. I. Nikulin, A. A. Samsonov, D. Korshunov, D. I. Vildanov
{"title":"New data on the composition of plagioclase on the western flank of the Oktyabrsky deposit according to infrared spectroscopy","authors":"I. O. Krylov, I. I. Nikulin, A. A. Samsonov, D. Korshunov, D. I. Vildanov","doi":"10.33623/0579-9406-2022-2-27-39","DOIUrl":"https://doi.org/10.33623/0579-9406-2022-2-27-39","url":null,"abstract":"The plagioclases of the Kharaelakh intrusion on the western part of the Oktyabrsky deposit were analyzed by infrared spectroscopy. Analysis of 130 Fourier-IR absorption spectra of plagioclases with selective verification of their chemical composition by X-ray spectral microanalysis indicates a regular change in the isomorphic series from albite (1150, 1096 cm–1) to anorthite (1142, 1275 cm–1), depending on the degree of differentiation of rocks in the intrusion. According to Fourier-IR spectroscopy, albite is confined to olivine-containing and olivine gabbro-dolerites. Anorthite is evenly distributed in gabbro-dolerites, but predominates in leucocratic gabbro. Among the impurity elements in the structure of the mineral, Fe3+ is noted at peaks of 1580–1644 cm–1 in picrite gabbro-dolerites, where ore interspersed mineralization of chalcopyrite, pyrrhotite, and pentlandite is directly developed. In addition to iron impurities, aluminum, potassium, barium, and strontium are also characteristic impurities in plagioclases. The totality of the data used in the section of the intrusion increases the indicative value of plagioclases and can be recommended as an additional mineral criterion of ore content.","PeriodicalId":253271,"journal":{"name":"Moscow University Bulletin. Series 4. Geology","volume":"1 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-12-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"115594338","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":"Introduction of the Stanovsky ophiolites of Faddesky block of Northeasten Taimyr according to geological data and numerical modeling results","authors":"L. I. Demina, V. S. Zakharov, M. Promyslova","doi":"10.33623/0579-9406-2022-1-24-34","DOIUrl":"https://doi.org/10.33623/0579-9406-2022-1-24-34","url":null,"abstract":"The geological position, morphology of serpentinite bodies, limitation by faults, the presence of surrounding metamorphites as enclosing strata fragments within the Stanovsky ophiolite complex, the nature of metamorphism, high deformation of rocks of both ophiolites and contact zone strata, and the mineral parageneses of secondary transformations fully correspond to the signs of Stanovsky ophiolites introduction into the deeply metamorphosed Faddeevsky block strata of Northeastern Taimyr, and not their obduction. The modeling results showed that fragments of the oceanic crust introduced into the metamorphosed complexes of the continental crust during the collision can have a dual origin — from the primary oceanic crust, and from the newly formed crust of the back-arc basin. A detailed chemical composition analysis of the Stanovsky ophiolites indicates their formation in the suprasubduction setting of the back-arc basin, which justifies the possibility of the second scenario.","PeriodicalId":253271,"journal":{"name":"Moscow University Bulletin. Series 4. Geology","volume":"18 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-12-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"125100673","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. Starovoytov, M. Tokarev, Z. Zamotina, Y. E. Terehina
{"title":"Role of glacial and lithodynamic factors in the formation of the sedimentary cover structure of the Great Salma Strait (White sea)","authors":"A. Starovoytov, M. Tokarev, Z. Zamotina, Y. E. Terehina","doi":"10.33623/0579-9406-2022-1-62-70","DOIUrl":"https://doi.org/10.33623/0579-9406-2022-1-62-70","url":null,"abstract":"New data on the bottom relief in the waters adjacent to the Belomorskaya Biological Station of Moscow State University (Kandalaksha Bay), obtained with the help of a multipath echo sounder (MBE), allowed us to study the bottom relief in detail and clarify the structure of Quaternary sediments in this area, significantly detailing the previously obtained data of continuous seismoacoustic profi ling (CSP). In the western part of the studied water area, the de Geer moraines were first identifi ed in a complex of glacial deposits, which were formed during the retreat of the glacier in the late Pleistocene in an easterly direction towards the modern deep-water part of the White Sea. In the deep-water part of the water area, according to the data of the MBE and CSP, sediments were studied, the genesis of which is due to the intensive manifestation of gravitational processes at the end of the Late Pleistocene — Holocene. The new data obtained may indicate the existence of “dead” ice in the Belomorskaya Depression.","PeriodicalId":253271,"journal":{"name":"Moscow University Bulletin. Series 4. Geology","volume":"16 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-12-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"121880748","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":"To the construction of a general classification of continental ecological and geological systems","authors":"V. Korolev, V. Т. Trofimov","doi":"10.33623/0579-9406-2022-1-54-61","DOIUrl":"https://doi.org/10.33623/0579-9406-2022-1-54-61","url":null,"abstract":"The issues of constructing a general classification of continental natural and technogenic ecologicalgeological systems, which are the subject of research in modern ecological geology, are considered. A classification is proposed that takes into account the composition and characteristics of the components of ecological-geological systems.","PeriodicalId":253271,"journal":{"name":"Moscow University Bulletin. Series 4. Geology","volume":"120 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-12-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"115462149","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":"The Modern Crystallography: Is It Useful for the Earth’s Sciences?","authors":"D. Y. Pushcharovsky","doi":"10.33623/0579-9406-2023-1-3-23","DOIUrl":"https://doi.org/10.33623/0579-9406-2023-1-3-23","url":null,"abstract":"Formed in XVII century at the junction between mineralogy and mathematics subsequently crystallography is considered as the science which is closer to physics, chemistry, biology and even to medicine. Due to this fact, the community, associated with the Earth’s sciences, accepts it with some restraint. The importance of the most advanced crystallographic approaches, the results obtained and the new insights which contribute the further development of the new scientific ideas about the composition and the structure of the Earth and some terrestrial planets are considered.","PeriodicalId":253271,"journal":{"name":"Moscow University Bulletin. Series 4. Geology","volume":"1 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-12-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"128976326","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":"Oleg Alexandrovich Mazarovich — representative of one of the famous geological dynasties of Russia (on the 100th anniversary of his birth)","authors":"A. Mazarovich, T. Tveritinova, A. I. Gushchin","doi":"10.33623/0579-9406-2022-4-164-168","DOIUrl":"https://doi.org/10.33623/0579-9406-2022-4-164-168","url":null,"abstract":"The biography and scientific achievements of Oleg Alexandrovich Mazarovich, Professor of the Department of Historical and Regional and the Department of Geology of Russia of the Geological Faculty of Moscow State University, a representative of the Russian geological dynasty Mazarovich, are considered.","PeriodicalId":253271,"journal":{"name":"Moscow University Bulletin. Series 4. Geology","volume":"360 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-12-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"134405920","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}