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Al. V. Tevelev I. A. Prudnikov Ark. V. Tevelev A. O. Khotylev E. A. Volodina 《Moscow University Geology Bulletin》2018,73(3):238-246
The structural features and mechanism of the formation of the Sim trough within the Uralian Foredeep, as well as the development of the entire Karatau–Suleiman block, are considered. This wedge-shaped block was subject to lateral extrusion to the north along conjugated strike-slip fault zones under a general latitudinal compression. This factor determined the local meridional compression and latitudinal extension of the block. In the central part of the block, the latitudinal extension was compensated by gradual subsidence, which resulted in the formation of the Sim trough. 相似文献
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Khotylev A. O. Mayorov A. A. Khudoley A. K. Ershova V. B. Kalmykov G. A. Khubanov V. B. Chervyakovskaya M. V. 《Geotectonics》2021,55(2):219-239
Geotectonics - In our research we summarized data obtained on the composition, structure, and geochemical characteristics of the granitoid plutons of the eastern part of the Krasnoleninsky arch of... 相似文献
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Al. V. Tevelev Ark. V. Tevelev V. A. Fedorchuk A. O. Khotylev I. A. Kosheleva 《Moscow University Geology Bulletin》2017,72(2):95-105
This work presents the results of studying zones bounded by the Archean and Early Proterozoic Taratash block, which breaks the meridional structure of the Urals, pinching its structural zones at the latitude of the town of Miass. The mesostructures of rupture zones, microtextures of tectonites, anisotropy of the magnetic susceptibility, and seismic-wave propagation rate in blastomylonites were studied. The kinematic history of the Taratash block consists of two phases: (1) exhumation in the Middle Riphean under conditions of crustal extension; and (2) the formation of an indenter in the Late Paleozoic under conditions of compression. 相似文献
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A. M. Nikishin A. O. Khotylev A. Yu. Bychkov L. F. Kopaevich E. I. Petrov V. O. Yapaskurt 《Moscow University Geology Bulletin》2013,68(3):141-154
Deposits in southwestern Crimea that contain Late Albian, Middle Senomanian, and Middle Campanian volcanic material are described and dated. Supposedly volcanic edifices are identified in the Black Sea (the Shatsky Swell) based on seismic data. The Albian, Senomanian, and Campanian volcanic belts are reconstructed for the entire Black Sea Region. The suggestion is made that the Black Sea Basin formed as a back-arc basin that started from rifting in the Albian and finished with spreading of the oceanic crust in the Senomanian-Early Santonian. 相似文献
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Ark. V. Tevelev I. A. Prudnikov A. O. Khotylev Al. V. Tevelev 《Moscow University Geology Bulletin》2015,70(6):399-408
The relationship between the tectonic structure of the Ai–Ufa interfluve (Southern Urals), its morphology, the recent deformations, and the distribution of clastic material in the fluvial basins were studied. Geological interpretations are suggested for the problematic local areas of the drainage basins, whose structure and evolution are distinct from the model scenarios. The sedimentary regime of the river valleys is controlled, first of all, by their configuration and orientation of the valley segments relative to the tectonic zones, as well as by the amount of clastic material that is delivered by tributaries, the climate history of the fluvial basin, and its recent tectonic activity. 相似文献
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Al. V. Tevelev I. A. Kosheleva A. O. Khotylev Ark. V. Tevelev I. A. Prudnikov 《Moscow University Geology Bulletin》2014,69(5):289-298
The Ai volcanic complex is a part of the Ai Formation, which begins the stratotypical Riphean section in the South Urals and lies on the Archean Taratash metamorphic complex. New geochemical and isotope data were obtained for the volcanic rocks. The dominant porphyritic plagioclase and pyroxene trachibasalts associated with dacites are characterized by higher contents of alkalis and titanium, which is typical of rift volcanism. However, other geochemical data, e.g., decreased Ni contents, are beyond of this scheme. The U-Pb (SHRIMP) age of zircons from dacites is 1415 ± 11 Ma. 相似文献
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Al. V. Tevelev Ark. V. Tevelev I. A. Prudnikov A. O. Khotylev E. E. Baraboshkin S. S. Popov 《Moscow University Geology Bulletin》2016,71(4):290-295
The structural features of the Upper Paleozoic flysch formations in the central part of the Cis-Uralian Foredeep were studied. Three types of structural paragenesises typical of thrust zones were distinguished. Among them are west vergent inclined folds and overfolds that pass into recumbent folds near a fault plane, structured tectonic melange, local thrusts, schistosity zones, and flat slipping planes. The various structural elements extend from northwest to northeast, due to the structural heterogeneity of the allochthon, approximately parallel to the strike of the Karantrav thrust. 相似文献
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V. V. Krupskaya G. A. Kalmykov O. V. Khotylev M. Yu. Revva 《Lithology and Mineral Resources》2006,41(3):222-229
Filtration-capacity properties of terrigenous reservoir rocks significantly depend on catagenetic transformations of clay minerals. Results of our research revealed the authigenic nature and formation stages of kaolinite and chlorite. The volume and shape of pore space define the morphology of clay particles. Depending on the pore volume, kaolinite crystallizes either as thick tabular aggregates or as fan-shaped intergrowths. The formation of authigenic clays in pores of terrigenous reservoirs decreases filtration-capacity properties of rocks with low permeability and, conversely, increases filtration-capacity properties of rocks with high primary permeability and large pore volume. 相似文献
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