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Soboleva S. V. Evstigneeva T. E. Boeva N. M. Bortnikov N. S. 《Doklady Earth Sciences》2020,491(2):210-213
Doklady Earth Sciences - A structural model of the rare mineral yushkinite [(Mg0.60Al0.30V0.10)Σ1.0(OH)2] [V0.875S2] is studied using the data of electron microdiffraction and the X-ray powder... 相似文献
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Mamedov V. I. Chausov A. A. Okonov E. A. Makarova M. A. Boeva N. M. 《Geology of Ore Deposits》2020,62(2):163-176
Geology of Ore Deposits - The recognition of the Fouta Djallon–Mandingo territory as an independent bauxite province is substantiated. It is confined to the morphostructure of the same name... 相似文献
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N. S. Bortnikov A. D. Savko V. M. Novikov N. M. Boeva S. V. Soboleva E. A. Zhegallo D. I. Dmitriev A. V. Krainov A. P. Zhukhlistov E. B. Bushueva 《Lithology and Mineral Resources》2016,51(6):425-438
This paper reports the results of our recent studies and generalizes previously known data on the geology, mineralogy, geochemistry, and genesis of the Russia’s largest Latnenskoe refractory clay deposit. It is shown that conditions of its localization were defined by regional and local factors. The regional factors controlled the distribution of the clay raw material in the region, while the local factors were responsible for the genesis and composition of refractory clays of the Latnenskoe deposit. Our studies showed that the formation of refractory clays is not only related to terrigenous but also to authigenic processes of sedimentation. The terrigenous component of clays was formed by the erosion of kaolin weathering crusts of the Voronezh anteclise crystalline basement and Paleozoic sedimentary hydromica–kaolinite rocks. Authigenic processes were significantly contributed by organic matter, which determined the environmental pH and Eh parameters. It is established that the mineral matter of clays of the deposit is represented by three morphological modifications (crystalline, amorphous, and biomorphic), which were formed subsequently and (or) simultaneously and could be transformed into each other. Application of a complex of modern precision methods allowed us to reveal a previously unknown biomorphic modification of kaolinite, the major rock-forming mineral, as well as mixed-layer kaolinite-smectite in the clays. It is shown that the distribution of major and trace elements and the sulfur isotope composition in different technological types of clay depend mainly on the facies conditions of their formation. Technological properties of clay raw material are considered. 相似文献
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N. S. Bortnikov V. M. Novikov A. D. Savko N. M. Boeva E. A. Zhegallo E. B. Bushueva A. V. Krainov D. A. Dmitriev 《Lithology and Mineral Resources》2013,48(5):384-397
This paper reports the results of precision structural-morphological study of kaolinite from clayey rocks taken in various areas of the Voronezh anteclise subjected to different stages of lithogenesis: primary kaolins of the weathering crust, proluvial-talus and lacustrine secondary kaolins, as well as lacustrine-swampy fireproof and deltaic-lagoonal refractory clays. The clayey material was transported over more than 300 km. The formation of the fireproof and refractory kaolin deposits in the Voronezh anteclise was related to the Devonian and Early Cretaceous stages of the geological evolution of the region. In terms of spatiotemporal and facies features, the studied genetic series of the kaolin clay deposits is unique. It was established that the sequential structural-morphological evolution o kaolinite in the considered deposits was caused by its mechanical disintegration during transport and redeposition. Interrelation between organic and mineral matters in the fireproof clays was revealed for the first time. Experimental studies of the behavior of kaolinite during sequential grinding and heating confirmed the main reasons for its natural degradation. The formation of virtually monomineral kaolin clays was provoked by the “flow-through” diagenesis, which is similar to weathering in trend. Evolution of mineral matter of the considered genetic series in kaolinite clay deposits was accompanied by the increase of δ18O values and their dispersion. Peculiarities identified in the behavior of kaolinite and related oxygen isotope characteristics of different-aged denudation and redeposition products of the Devonian weathering crust can play an indicator role in studying different stages of the lithogenesis of clayey rocks. 相似文献
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Doklady Earth Sciences - For the first time, a series of long-term taphonomic experiments (1–5 years) has shown iron deposition during the formation of fossils of soft-bodied animals. Based... 相似文献
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Mamedov V. I. Shipilova E. S. Boeva N. M. Slukin A. D. Makarova M. A. Vnuchkov D. A. Bortnikov N. S. 《Doklady Earth Sciences》2020,490(1):8-12
Doklady Earth Sciences - Investigation of the comprehensive geological material on the lateritic weathering rocks (Futa Jallon-Mandingo, Africa) led to original identification of a specific horizon... 相似文献
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N. S. Bortnikov V. M. Novikov N. M. Boeva T. S. Gendler E. A. Zhegallo A. P. Zhukhlistov S. V. Soboleva 《Doklady Earth Sciences》2014,457(2):986-990
Studies of the mineral substance in the weathering crust (CW) of the basalts of Vietnam have shown that these basalts might be considered as a natural laboratory for the formation of mineral bionanostructures of specific crystal morphology and thermal and magnetic properties. It is suggested that the crystallization of goethite in the cuirass and underlying bauxites of the CW of Vietnam resulted from the coagulation of colloidal particles and of hydrated iron oxide under the impact of bacterial colonies, which determined the specific features. 相似文献
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R. Zamanov S. Boeva G. Latev K. A. Stoyanov S. V. Tsvetkova 《Astronomische Nachrichten》2015,336(2):189-195
We performed simultaneous observations in 3 bands (U BV) of the flickering variability of the recurrent novae RS Oph and T CrB at quiescence. Using new and published data, we compare the colours of the flickering in cataclysmic variables and symbiotic recurrent novae. We find a difference between the colours of the flickering source in these two types of accreting white dwarfs. The detected difference is highly significant with p ‐values ≈2 x 10–6 for the distributions of (U – B)0 colour and p ≈ 3 x 10–5 on an (U – B) versus (B – V) diagram. The possible physical reasons are briefly discussed. The data are available upon request from the authors. (© 2015 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim) 相似文献