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A. A. Krasnobaev P. M. Valizer V. N. Anfilogov S. A. Sergeev A. I. Rusin S. V. Busharina E. V. Medvedeva 《Doklady Earth Sciences》2016,469(1):674-679
Dating of zircon (SHRIMP) from dunite and harzburgite of the Karabash massif was carried out for the first time. Relics of ancient crystals (1940 ± 30 Ma in harzburgite, 1860 ± 16 Ma in dunite) provide evidence for the Paleoproterozoic age of the protolith. The morphological peculiarities of zircon crystals allow us to assume differentiation of the magmatic source 1720 m. y. ago. The major variety of zircons indicates stages of metamorphic evolution in the Neoproterozoic (530–560 Ma) and Early–Late Ordovician (440–480 Ma). 相似文献
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V. I. Ulomov T. I. Danilova N. S. Medvedeva T. P. Polyakova 《Izvestiya Physics of the Solid Earth》2006,42(7):551-566
The Scythian-Turan platform, together with the Alpine Iran-Caucasus-Anatolia and Hercynian Central Tien Shan orogenic structures adjacent to it, represents a coherent seismogeodynamic system responsible for regional seismicity features in the territory under consideration. Investigations of the spatiotemporal and energy evolution of seismogeodynamic processes along the main lineament structures of the orogen reveal characteristic features directly related to the prediction of seismic hazard in this region, as well as in southern European Russia. These characteristics primarily include kinematic features in the sequences of seismic events of various magnitudes and an ordered migration of seismic activation, enabling the more or less reliable determination of the occurrence time intervals (years) and areas of forthcoming large earthquakes (magnitudes of 7.0 ± 0.2, 7.5 ± 0.2, and 8.0 ± 0.2). 相似文献
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Kubryakov A. A. Lishaev P. N. Chepyzhenko A. I. Aleskerova A. A. Kubryakova E. A. Medvedeva A. V. Stanichny S. V. 《Oceanology》2021,61(2):159-172
Oceanology - High-resolution measurements by unmanned aerial vehicles (UAVs), satellite and in-situ data are used to study the optical structure of coastal submesoscale eddies and their influence... 相似文献
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A.?I.?SemenovEmail author I.?V.?Medvedeva V.?I.?Perminov 《Geomagnetism and Aeronomy》2018,58(2):273-280
The results of rocket and satellite measurements available in the literature of 5.3-μm nitric oxide emission in the upper atmosphere have been systematized and analyzed. Analytical dependences describing the height distribution of volumetric intensity of 5.3-μm emission of the NO molecule and its variations in a range of heights from 100 to 130 km as a function of the time of year, day, latitude, and solar activity have been obtained. 相似文献
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A.?I.?SemenovEmail author I.?V.?Medvedeva V.?I.?Perminov Yu.?A.?Zheleznov 《Geomagnetism and Aeronomy》2017,57(5):597-601
The results of rocket and satellite measurements of carbon dioxide emissions at a wavelength of 15 μm in the upper atmosphere have been systematized and analyzed. Analytical expressions describing the dependence of the altitude distribution of 15-μm CO2 emission intensity and its variation in the altitude range from 100 to 130 km on the season, latitude, and solar activity have been obtained. 相似文献
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Medvedeva M. A. Vozbrannaya A. E. Sirin A. A. Maslov A. A. 《Izvestiya Atmospheric and Oceanic Physics》2017,53(9):1072-1080
Izvestiya, Atmospheric and Oceanic Physics - The capabilities of several multispectral satellite data types to identify the status of peatlands affected by peat extraction and abandoned deposits... 相似文献
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S. A. Medvedeva 《Russian Journal of Pacific Geology》2016,10(4):299-316
The first data on the whole-rock chemical composition of Jurassic–Lower Cretaceous sedimentary rocks cropping out in the Soloni–Umal’ta river interfluve (Bureya sedimentary basin) are used for revealing the distribution of their rock-forming elements. It is shown that the clastic material originated mostly from acid igneous rocks, while their intermediate varieties, as well as quartz-rich sedimentary and metamorphic rocks, played a subordinate role. It is assumed that the bulk of the clastic material was transported from the west and southwest (Bureya massif) and a smaller share from the east. The most significant differences between the Lower–Middle Jurassic and Upper Jurassic–Lower Cretaceous rocks mark a break in sedimentation. 相似文献
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