{"title":"Modeling method for obtaining kinetic parameters of metamorphic reactions in texture-homogeneous rocks","authors":"I. Likhanov, И И Лиханов","doi":"10.31857/s0869-56524884420-424","DOIUrl":"https://doi.org/10.31857/s0869-56524884420-424","url":null,"abstract":"A new approach for deriving kinetic parameters of diffusion-controlled metamorphic reactions is described. It is based on comparison of models of temperature field evolution near a cylindrical intrusion and observable chemical changes in minerals at the contact aureole of the Kharlovo massif. The calculations yielded estimates of the effective rates of metamorphic reactions (~10-12 s-1) and the effective diffusion coefficient (5.29 10-16 cm2s-1 at T = 475 С). These values are consistent with experimentally and theoretically derived estimates of solid-state diffusion, including grain-boundary diffusion in mineral aggregates and segregations for the respective PT-parameters.","PeriodicalId":24047,"journal":{"name":"Доклады Академии наук","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2019-10-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"73411813","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}
M. Erbajeva, М А Ербаева, A. Shchetnikov, А А Щетников, A. Kazansky, А Ю Казанский, G. Matasova, Г Г Матасова, F. Khenzykhenova, Ф И Хензыхенова, I. A. Filinov, И А Филинов, O. D. Namzalova, О Намзалова Д-Ц., I. V. Nechaev, И О Нечаев
{"title":"New pleistocene key section Ulan-Zhalga of the Western Transbaikalia","authors":"M. Erbajeva, М А Ербаева, A. Shchetnikov, А А Щетников, A. Kazansky, А Ю Казанский, G. Matasova, Г Г Матасова, F. Khenzykhenova, Ф И Хензыхенова, I. A. Filinov, И А Филинов, O. D. Namzalova, О Намзалова Д-Ц., I. V. Nechaev, И О Нечаев","doi":"10.31857/s0869-56524883277-281","DOIUrl":"https://doi.org/10.31857/s0869-56524883277-281","url":null,"abstract":"The currant paper presents the preliminary results of the multidisciplinary study of the new Pleistocene section Ulan-Zhalga (51°29′40.75″ С, 107°20′18.11″ В) discovered in the Western Transbauikalaia in 2017. On the base of the paleontological, paleomagmetic, and lithological data the early, middle and late Pleistocene sediments were recognized in the section. The analysis of the rich small mammal fossils resulted in to trace the paleoenvironmental and climatic changes in the region during the Quaternary. The unique alternation of the 19 faunistic horizons and 11 fossil soils in the whole section, the high correlation of the paleomagnetic and paleontological data allow us to refer the studied section Ulan-Zhalga to addition new late Cenozoic Key section of the south Eastern Siberia. The new geological and paleontological data would be important for paleogeographical reconstruction and biostratigraphic analysis.","PeriodicalId":24047,"journal":{"name":"Доклады Академии наук","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2019-09-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"90971933","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":"Connection of crystal faceting with the mechanism of its formation","authors":"P. Fedorov, П П Федоров, V. V. Osiko, В В Осико","doi":"10.31857/s0869-56524883253-255","DOIUrl":"https://doi.org/10.31857/s0869-56524883253-255","url":null,"abstract":"The observed formation of nano- and microcrystals devoid of faceting in low-temperature processes of their formation can be associated with the implementation of a non-classical crystal growth mechanism by aggregation and oriented splicing of particles. The observation is illustrated on CaF2 examples.","PeriodicalId":24047,"journal":{"name":"Доклады Академии наук","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2019-09-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"88844264","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}
F. Maksimov, Ф Е Максимов, M. Pevzner, М М Певзнер, A. Petrov, А.Ю. Петров, S. Levchenko, С Б Левченко, V. Grigoriev, Василий Александрович Григорьев, N. Baranova, Н. Г. Баранова, V. Kuznetsov, В. Ю. Кузнецов
{"title":"Age of the «cross-laminated sandy» stratum from the reference section Yar Sredny (Central Kamchatka) according to the paired 230Th /238U and 14C dating of peat","authors":"F. Maksimov, Ф Е Максимов, M. Pevzner, М М Певзнер, A. Petrov, А.Ю. Петров, S. Levchenko, С Б Левченко, V. Grigoriev, Василий Александрович Григорьев, N. Baranova, Н. Г. Баранова, V. Kuznetsov, В. Ю. Кузнецов","doi":"10.31857/s0869-56524883288-293","DOIUrl":"https://doi.org/10.31857/s0869-56524883288-293","url":null,"abstract":"For the first time, numerical radioisotope age were obtained for the “cross-laminated sandy” stratum, which is widespread in Neopeopleistocene reference sections of loose sediments from Central Kamchatka. Two peat layers, incorporated in the “cross-laminated sandy” stratum of the Yar Sredny, were studied. The results of their paired 230Th/238U and 14C dating are in good agreement with each other. According to the dating results, it was determined that the “cross-laminated sandy” stratum was deposited, apparently, in the range of about 50-40 thousand years ago, i.e. in the Late Pleistocene (MIS-3), and not in the Middle Pleistocene, about 400-300 thousand years ago, as previously thought.","PeriodicalId":24047,"journal":{"name":"Доклады Академии наук","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2019-09-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"91339020","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":"Influence of the vibrations in the interfacial layer on the wettability of adhesized material interfacial formations in systems with d- and f-elements","authors":"E. Golubina, N. Kizim, A. Chekmarev","doi":"10.31857/s0869-56524883267-271","DOIUrl":"https://doi.org/10.31857/s0869-56524883267-271","url":null,"abstract":"The effect of local vibration at interfacial layer of a heterogeneous liquid system on the wettability of the material of interfacial formations based on the salt of the d- or f-element of di-(2-ethylhexyl)phosphoric acid adhered to glass has been investigated. It is shown that in the field of mechanical vibrations one can obtain a material with a given value of the wetting angle, which has hydrophobic properties. It is established that the influence of mechanical vibrations is due to changes in the hydrodynamic situation in the transition region and is the result of complex interactions mainly hydrodynamic and coagulation processes in the interfacial layer of the di-(2-ethylhexyl)phosphoric acid - solvent system / water solution of the d- or f-element salt. The dependence of the wettability of the material of interfacial formations adhered to glass on the parameters of the force field (vibration frequency, amplitude), the design features of the experimental setup, and the composition of the system is shown.","PeriodicalId":24047,"journal":{"name":"Доклады Академии наук","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2019-09-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"83921494","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. Fedotova, Анастасия Федотова, S. Bogdanova, С В Богданова, S. Claesson, С. Клаэссон, M. Anosova, М О Аносова, A. V. Postnikov, А.В. Постников, M. M. Fugzan, М. М. Фугзан, T. Kirnozova, Т. И. Кирнозова
{"title":"New data refer to palaeoproterozoic age of the Elabuga deformation zone metamorphism of the Volgo-Uralia, East European Craton","authors":"A. Fedotova, Анастасия Федотова, S. Bogdanova, С В Богданова, S. Claesson, С. Клаэссон, M. Anosova, М О Аносова, A. V. Postnikov, А.В. Постников, M. M. Fugzan, М. М. Фугзан, T. Kirnozova, Т. И. Кирнозова","doi":"10.31857/s0869-56524883307-312","DOIUrl":"https://doi.org/10.31857/s0869-56524883307-312","url":null,"abstract":"This paper presents age data of the Elabuga zone rocks metamorphism and of the detrital zircon of the Elabuga zone paragneisses and their correlation with the age of Middle-Volga megablock rocks. The Elabuga zone rocks and the Middle-Volga megablock rocks have similar geochemical characteristics and degree of metamorphism. Difference is as follows: Paleoproterozoic metamorphism is occurred at the studied Elabuga zone rocks and such metamorphism age is not presented at the Middle-Volga megablock rocks. The study of U-Pb isotopic system in external zones in the Elabuga deformation zone zircon crystals suggests that rocks were underwent by metamorphism of two stages 1.99 and 1.95 Ga ago.","PeriodicalId":24047,"journal":{"name":"Доклады Академии наук","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2019-09-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"88589520","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}
Y. Vasil'chuk, Ю.К. Васильчук, A. Kurchatova, А Н Курчатова, N. Budantseva, Н.А. Буданцева, V. Rogov, В. В. Рогов, J. Chizhova, Ю.Н. Чижова
{"title":"Variations of stable oxygen and hydrogen isotopes in the pingo ice core, south of the Gydan Peninsula","authors":"Y. Vasil'chuk, Ю.К. Васильчук, A. Kurchatova, А Н Курчатова, N. Budantseva, Н.А. Буданцева, V. Rogov, В. В. Рогов, J. Chizhova, Ю.Н. Чижова","doi":"10.31857/s0869-56524883323-328","DOIUrl":"https://doi.org/10.31857/s0869-56524883323-328","url":null,"abstract":"The vertical isotopic profile of the pingo Messoyakha-1 (coordinates: 68°30′32″ N, 79°59′53″ E) ice core, obtained in the south of the Gydan Peninsula in the Middle Messoyakha swell. There is no significant variations of the isotopic composition of pingo ice core: δ18О values vary from -14.98 to -16.60‰, δ2Н values vary from -117.9 to -12.8. This small scatter of values is probably the result of intense heaving and rather rapid formation of the pingo. Basing on the features of the pingo, it can be assumed that initially there was a lake of 0.5 km length and 0.3 km width in this site. Then, as a result of water draining to a nearby river, the lake began to dry out and alas, which occupies most of the primary lake area, was formed. Pingo arose during the freezing of the alas under its gradual drying.","PeriodicalId":24047,"journal":{"name":"Доклады Академии наук","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2019-09-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"77986714","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}
P. Bazhin, П М Бажин, A. Stolin, А М Столин, A. Konstantinov, А С Константинов, A. Chizhikov, А П Чижиков, A. Prokopets, А Д Прокопец, M. Alymov, М И Алымов
{"title":"Structural features of layered composite materials based on titanium borides by free SHS compression","authors":"P. Bazhin, П М Бажин, A. Stolin, А М Столин, A. Konstantinov, А С Константинов, A. Chizhikov, А П Чижиков, A. Prokopets, А Д Прокопец, M. Alymov, М И Алымов","doi":"10.31857/s0869-56524883263-266","DOIUrl":"https://doi.org/10.31857/s0869-56524883263-266","url":null,"abstract":"The work shows the structural features layered composite materials based on titanium boride on titanium alloy VT6 (Ti6Al4V) by the method of free SHS compression, which implements the combination of combustion processes and high-temperature shear deformation. The layered structure of the produced materials was established, the feature of the structure of the transition zone at the boundary of the ceramic composite - titanium alloy was studied in details.","PeriodicalId":24047,"journal":{"name":"Доклады Академии наук","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2019-09-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"88066819","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. Agatova, А Р Агатова, R. Nepop, Р К Непоп, L. Khazin, Л Б Хазин, A. Zhdanova, А. Н. Жданова, O. Uspenskaya, О.Н. Успенская, I. Ovchinnikov, И Ю Овчинников, P. Moska, П Моска
{"title":"New chronological (14C, OSL), paleontological and geochemical data on developing of ice-dammed lakes in Kurai basin (south-eastern part of the Russian Altai) during the MIS-2","authors":"A. Agatova, А Р Агатова, R. Nepop, Р К Непоп, L. Khazin, Л Б Хазин, A. Zhdanova, А. Н. Жданова, O. Uspenskaya, О.Н. Успенская, I. Ovchinnikov, И Ю Овчинников, P. Moska, П Моска","doi":"10.31857/s0869-56524883319-322","DOIUrl":"https://doi.org/10.31857/s0869-56524883319-322","url":null,"abstract":"One of the highly debatable issue of the Altai Pleistocene paleogeography is the chronology and extension of the last ice-dammed lakes. For the first time paleontological, mineralogical characteristics, and optically stimulated luminescence (OSL) ages for lacustrine deposits confirm accumulation of ice-dammed lake with depth at least 170 m in Kurai basin at the end of the Late Pleistocene - 16-19 ka. New data provide information about the ecology and evolution of this Sartan reservoir. Draining of this lake less affected the topography in comparison with earlier cataclysmic glacier-lakes outburst floods. Nevertheless, the lake controlled human settlement of the basin in the Late Paleolithic. Drying of this reservoir defined formation of the modern hydrological network, including flowing of the Chuya River along the steep gorge between the Maashey and Belgibash mouths. New data evidence for significant difference in evolution of the Kurai-Chuya system of intermountain depressions and Uimon basin at the end of the Late Pleistocene.","PeriodicalId":24047,"journal":{"name":"Доклады Академии наук","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2019-09-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"82818111","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}
V. Golubev, В И Голубев, A. V. Shevchenko, Андрей Владимирович Шевченко, I. Petrov, Игорь Петров
{"title":"Taking into account the fluid saturation of bottom sediments in marine seismic survey problem","authors":"V. Golubev, В И Голубев, A. V. Shevchenko, Андрей Владимирович Шевченко, I. Petrov, Игорь Петров","doi":"10.31857/s0869-56524883248-252","DOIUrl":"https://doi.org/10.31857/s0869-56524883248-252","url":null,"abstract":"The problem of the numerical simulation of the seismic response from the marine bottom is considered. Acoustic equations are used for the description of the water dynamic behavior. Bottom sediments are described with the porous fluid-filled medium. The Dorovsky model is used. The algorithm for solving all hyperbolic equation systems with the grid-characteristic method was proposed. The distinctive feature of this approach is the ability to set explicitly necessary contact conditions between media with different rheology.","PeriodicalId":24047,"journal":{"name":"Доклады Академии наук","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"2019-09-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"81886397","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}