Metamorphic rocks of the Murmansk domain (Kola Peninsula) as compared with the oldest rock associations of the northeastern Baltic shield,Canada, and Greenland     

N. E. Kozlov  E. V. Martynov  N. O. Sorokhtin  A. A. Ivanov  N. M. Kudryashov  N. E. Kozlova 《Geochemistry International》2008,46(6):608-613

Rock associations characterized by heterogeneous sets of petrogeochemical parameters were compared by quantifying the degree of their similarity-dissimilarity and searching for discrimination trends between them. Using procedures specially developed for this purpose, it was demonstrated for the first time that the lithotectonic complexes of the Murmansk domain are fundamentally different from those of typical granulite-gneiss terrains and resemble the granite-greenstone terrains of the Baltic shield, Greenland, and Canada. Based on the whole data set, the Murmansk domain can be considered as a deeply eroded Archean granite-greenstone terrain retaining only the tonalite-trondhjemite-gneiss basement with abundant supracrustal enclaves. A trend of the compositional difference between the older and younger rock associations is similar to that between the tholeiitic and boninitic volcanic series. It was suggested that the petrogeochemical “age” trend reflects the initial stage of the compositional evolution of the metamagmatic rocks of the region from metamorphic rocks similar to tholeiites at the early stages to the Paleoproterozoic boninite-like rocks, which are believed to be linked to the unique PGE-bearing province of the northeastern Baltic shield. This implies that the specific metallogenic features of the region emerged already in the Archean, which supported the suggestion on the long duration of geological processes in the Early Precambrian.  相似文献   

Collisional metamorphism as a result of thrusting in the Transangara region of the Yenisei Ridge     

I. I. Likhanov  P. S. Kozlov  N. V. Popov  V. V. Reverdatto  A. E. Vershinin 《Doklady Earth Sciences》2006,411(1):1313-1317

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Estimation of Aerosol Radiation Effects under Background and Smoke-haze Atmospheric Conditions over Siberia from Empirical Data     

M. V. Panchenko  T. B. Zhuravleva  V. S. Kozlov  I. M. Nasrtdinov  V. V. Pol’kin  S. A. Terpugova  D. G. Chernov 《Russian Meteorology and Hydrology》2016,41(2):104-111

The results of numerical simulation of downward solar radiation fluxes for background and smoke-contaminated atmospheric conditions are discussed. Vertical profiles of aerosol characteristics are obtained from the empirical model based on the data of aircraft sounding of profiles of angular scattering coefficients and content of absorbing particles in the lower troposphere. The background model was created using the results of measurements obtained under cloudless and mostly cloudless atmospheric conditions in 1999–2011. Optical parameters of smoke aerosol are determined from the data of aircraft measurements in the period of long-term wildfires in Siberia in the summer 2012. It is demonstrated that deficiency in diurnal values of total solar radiation at the surface level caused by the formation of the optically dense smoke layer as compared to background conditions, is more than 13 MJ/m².  相似文献   

Natural ring structures on the Baikal ice cover: Analysis of experimental data and mathematical modeling     

N.G. Granin  I.B. Mizandrontsev  V.V. Kozlov  E.A. Tsvetova  R.Yu. Gnatovskii  V.V. Blinov  I.A. Aslamov  K.M. Kucher  V.G. Ivanov  A.A. Zhdanov 《Russian Geology and Geophysics》2018,59(11):1514-1525

Hydrophysical studies and mathematical modeling of ring structures during ice cover on Lake Baikal have shown that their existence at the stage of ice cover degradation is due to anticyclonic currents. Such currents can be generated as a result of local upwelling, which we associate with the rise of methane hydrates from the top layer of bottom sediments and their dissociation. Analysis of satellite images shows that the radii of ice rings range from 1300 to 2400 m, which is close to the baroclinic Rossby radius. The measured ice thicknesses in the area of the rings are in agreement with model calculations. Deep water renewal in Lake Baikal can also be associated with the rise of hydrates.  相似文献   

Geochemical peculiarities of some rock-forming minerals during experimental modeling of shock metamorphism     

S. G. Skublov  V. I. Fel’dman  E. A. Kozlov 《Doklady Earth Sciences》2010,432(1):638-643

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The polygenous-polychronous nature of zircons and the problem of the age of the Barangulov gabbro-granite complex     

A. A. Krasnobaev  V. I. Kozlov  V. N. Puchkov  A. N. Larionov  A. G. Nekhorosheva  N. G. Berezhnaya 《Doklady Earth Sciences》2007,416(1):1070-1075

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Ethnic processes and trends in the ethnic composition of the population in the USSR     

Kozlov V. I. 《GeoJournal》1980,4(1):23-30

The paper deals with the processes of ethnic consolidation, ethnic and linguistic assimilation and inter-ethnic integration taking place in the USSR. The author shows the influence of consolidation and assimilation processes over the trends in the numerical strength of individual peoples and the resulting change in the country's ethnic composition as this is reflected in the Soviet population censuses of 1926, 1959, 1970, and 1979.  相似文献   

Variations of Natural Electrical Potentials in the Cryolithozone,Yakutsk     

Kozlov  V. I.  Baishev  D. G.  Pavlov  E. A. 《Izvestiya Physics of the Solid Earth》2022,58(3):435-442

Izvestiya, Physics of the Solid Earth - Abstract—This paper considers daily, seasonal, and interannual variations of natural potentials at two sites in the cryolithozone at the testing...  相似文献   

P–T evolution of ultrahigh temperature metamorphism: Evidence for a Late Paleoproterozoic intraplate extension at the southwestern margin of the Siberian Craton     

I. I. Likhanov  A. D. Nozhkin  V. V. Reverdatto  P. S. Kozlov  V. V. Khiller 《Doklady Earth Sciences》2015,465(1):1139-1142

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Photometric investigation of the Herbig Ae/Be star MWC 297. I. Quasisimultaneous UBVRIJHK observations     

Yu. K. Bergner  V. P. Kozlov  A. A. Krivtsov  A. S. Miroshnichenko  R. V. Yudin  N. Yu. Yutanov  K. G. Dzhakusheva  K. S. Kuratov  D. B. Mukanov 《Astrophysics》1988,28(3):313-320

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