Spetsius, Z. V. Bogush, I. N.
Published in
Doklady Earth Sciences
The first studies of diamonds in eclogitic xenoliths from the Komsomolskaya kimberlite pipe are described. Among round and oval-shaped xenoliths with diamond ingrowths, samples with a garnet content of 40–90% of the xenolith volume dominate. Two eclogite samples contain grains of accessory rutile; a kyanite sample is also revealed. Certain samples ...
Vakhrusheva, N. V. Ivanov, K. S.
Published in
Doklady Earth Sciences
Corundum-containing and corundum-free plagioclasites localized in chromite-bearing ultramafites of the Rai-Iz Massif were explored for the composition and age. The composition of rock-forming minerals was studied, and the geochemical characteristics of the rocks were ascertained. The isotope age of plagioclasites determined by zircons using the U–P...
Demina, L. L. Budko, D. F. Lisitzin, A. P. Novigatsky, A. N.
Published in
Doklady Earth Sciences
The contribution of different geochemical processes in the accumulation of metals in dispersed sedimentary matter collected by ADOO was estimated for the first time for the White Sea system. The contents of Al, Fe, Cr, Ni, Со, and Мо (from 60 to 90% of the total content) are mainly controlled by terrigenous processes. The group of geochemically mob...
Ivanov, V. A. Zalesny, V. B. Lukyanova, A. N. Bagaev, A. V.
Published in
Doklady Earth Sciences
The parameters of barotropic and baroclinic oscillations in the subinertial range have been obtained by numerical simulations of the Black Sea circulation using a model developed at the Marchuk Institute of Numerical Mathematics, Russian Academy of Sciences. The structures and periods of barotropic and baroclinic seiches are in good agreement with ...
Konovalov, Yu. I. Luchsheva, L. N. Kurnosov, V. B.
Published in
Doklady Earth Sciences
The results of studying Hg in an underwater hydrothermal system in the ocean using the Middle Valley of the Juan de Fuca ridge as an example are presented. A significant part of Hg is accumulated in the basalt fundament (Holes 858F, G), forming anomalously high concentrations (up to 29.30 ppm) in certain parts. The high Hg contents were established...
Maslov, A. V. Kovalev, S. G. Puchkov, V. N. Sergeeva, N. D.
Published in
Doklady Earth Sciences
The geodynamic origin of volcanic and sedimentary rocks of the Upper Precambrian Arsha Group of the western slope of the southern Urals is considered. It is shown that both rock types are riftogenic/plume in origin. The problem of the spatial and temporal correlation of the Arsha and Karatau groups requires further study.
Gorbatikov, A. V. Rogoghin, E. A. Stepanova, M. Yu. Kharazova, Yu. V. Sysolin, A. I. Rybin, A. A. Andreeva, N. V.
Published in
Doklady Earth Sciences
A geophysical section by the method of microseismic sounding is obtained along the profile that completely crosses the Elbrus volcano in the area of its eastern summit. The peculiarities of the deep structure and edifice of the Elbrus volcano are revealed.
Mokhov, I. I. Smirnov, D. A.
Published in
Doklady Earth Sciences
We have quantitatively estimated the contributions of anthropogenic forcing characterized by variations in the atmospheric content of greenhouse gases and of natural variability characterized by the Atlantic Multidecadal Oscillation to the trends of global surface air temperature from observations since the middle of the nineteenth century on the b...
Bushnev, D. A. Burdelnaya, N. S. Goncharov, I. V. Samoylenko, V. V. Veklich, M. A.
Published in
Doklady Earth Sciences
The molecular and isotopic composition of an extract from the rocks of the Bazhenov Formation in the southeast part of Western Siberia, oils that are genetically related to this formation, and products of hydrous pyrolysis of the organic matter of oil shale (Middle Volgian) of the East European Platform were studied. Common features and differences...
Pertsev, A. N. Bortnikov, N. S. Prokofiev, V. Yu. Aranovich, L. Ya. Ageeva, O. A. Beltenev, V. E. Zhilicheva, O. M. Kovalchuk, E. V.
Published in
Doklady Earth Sciences
New data on local mineral associations and the microheterogeneity of minerals and fluid inclusions in gabbro were obtained for the gabbro–peridotite oceanic core complex with a long-lived detachment fault controlling the hydrothermal activity. It is assumed that the hydrothermal hydrogen-bearing fluid with a NaCl content of >30 wt % is formed in th...