24 research outputs found
ΠΠΎΡΡΠΎΠ»ΠΎΠ³ΠΈΡ, ΡΡΡΠΎΠ΅Π½ΠΈΠ΅ ΠΈ ΡΠΎΡΡΠ°Π² ΡΠΈΡΠΊΠΎΠ½Π° ΠΈΠ· ΠΌΠ΅ΡΠ°ΠΏΠ΅ΡΡΠ°Π½ΠΈΠΊΠΎΠ² Π°Π»ΡΠΊΠ΅ΡΠ²ΠΎΠΆΡΠΊΠΎΠΉ ΡΠΎΠ»ΡΠΈ (ΠΡΠΈΠΏΠΎΠ»ΡΡΠ½ΡΠΉ Π£ΡΠ°Π»)
Description of the features of morphology, internal structure, and analysis results of Th/U and Zr/Hf ratios in zircons from sandstones of the gold-bearing Alkesvozhskaya sequence, located at the basement of the Paleozoic section in the Subpolar Urals, is presented. It has been established that most of the studied zircons are primary igneous grains of the first weathering cycle. The detrital zircon source was probably in formations close in age, underlying or located nearby felsic and basic volcanics of igneous complexes of different stages of formation of Timanides-protouralides, associated granitoids, and intrusive mafic formations. Small part of well-rounded zircon Pre-Riphean grains can be redeposited from the Riphean metasedimentary formations, which, in turn, inherited it from the rocks of the ancient basement of the East European PlatformΠΡΠΈΠ²Π΅Π΄Π΅Π½Ρ ΠΎΠΏΠΈΡΠ°Π½ΠΈΠ΅ ΠΎΡΠΎΠ±Π΅Π½Π½ΠΎΡΡΠ΅ΠΉ ΠΌΠΎΡΡΠΎΠ»ΠΎΠ³ΠΈΠΈ, Π²Π½ΡΡΡΠ΅Π½Π½Π΅Π³ΠΎ ΡΡΡΠΎΠ΅Π½ΠΈΡ ΠΈ Π°Π½Π°Π»ΠΈΠ· ΠΎΡΠ½ΠΎΡΠ΅Π½ΠΈΠΉ Th/U ΠΈ Zr/Hf Π² ΡΠΈΡΠΊΠΎΠ½Π°Ρ
ΠΈΠ· ΠΏΠ΅ΡΡΠ°Π½ΠΈΠΊΠΎΠ² Π·ΠΎΠ»ΠΎΡΠΎΠ½ΠΎΡΠ½ΠΎΠΉ Π°Π»ΡΠΊΠ΅ΡΠ²ΠΎΠΆΡΠΊΠΎΠΉ ΡΠΎΠ»ΡΠΈ, ΡΠ°ΡΠΏΠΎΠ»ΠΎΠΆΠ΅Π½Π½ΠΎΠΉ Π² ΠΎΡΠ½ΠΎΠ²Π°Π½ΠΈΠΈ ΠΏΠ°Π»Π΅ΠΎΠ·ΠΎΠΉΡΠΊΠΎΠ³ΠΎ ΡΠ°Π·ΡΠ΅Π·Π° Π½Π° ΠΡΠΈΠΏΠΎΠ»ΡΡΠ½ΠΎΠΌ Π£ΡΠ°Π»Π΅. Π£ΡΡΠ°Π½ΠΎΠ²Π»Π΅Π½ΠΎ, ΡΡΠΎ Π±ΠΎΠ»ΡΡΠΈΠ½ΡΡΠ²ΠΎ ΠΈΠ·ΡΡΠ΅Π½Π½ΡΡ
ΡΠΈΡΠΊΠΎΠ½ΠΎΠ² ΡΠ²Π»ΡΡΡΡΡ ΠΏΠ΅ΡΠ²ΠΈΡΠ½ΠΎ-ΠΌΠ°Π³ΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΠΌΠΈ Π·Π΅ΡΠ½Π°ΠΌΠΈ ΠΏΠ΅ΡΠ²ΠΎΠ³ΠΎ ΡΠΈΠΊΠ»Π° Π²ΡΠ²Π΅ΡΡΠΈΠ²Π°Π½ΠΈΡ. ΠΡΡΠΎΡΠ½ΠΈΠΊΠΎΠΌ ΠΎΠ±Π»ΠΎΠΌΠΎΡΠ½ΠΎΠ³ΠΎ ΡΠΈΡΠΊΠΎΠ½Π°, Π²Π΅ΡΠΎΡΡΠ½ΠΎ, ΡΠ²Π»ΡΠ»ΠΈΡΡ Π±Π»ΠΈΠ·ΠΊΠΈΠ΅ ΠΏΠΎ Π²ΡΠ΅ΠΌΠ΅Π½ΠΈ ΠΎΠ±ΡΠ°Π·ΠΎΠ²Π°Π½ΠΈΡ ΠΏΠΎΠ΄ΡΡΠΈΠ»Π°ΡΡΠΈΠ΅ ΠΈΠ»ΠΈ ΡΠ°ΡΠΏΠΎΠ»ΠΎΠΆΠ΅Π½Π½ΡΠ΅ ΠΏΠΎΠ±Π»ΠΈΠ·ΠΎΡΡΠΈ ΠΊΠΈΡΠ»ΡΠ΅ ΠΈ ΠΎΡΠ½ΠΎΠ²Π½ΡΠ΅ Π²ΡΠ»ΠΊΠ°Π½ΠΈΡΡ ΠΌΠ°Π³ΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΊΠΎΠΌΠΏΠ»Π΅ΠΊΡΠΎΠ² ΡΠ°Π·Π»ΠΈΡΠ½ΡΡ
ΡΡΠ°Π΄ΠΈΠΉ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΡΠΈΠΌΠ°Π½ΠΈΠ΄-ΠΏΡΠΎΡΠΎΡΡΠ°Π»ΠΈΠ΄, Π°ΡΡΠΎΡΠΈΠΈΡΡΡΡΠΈΠ΅ Ρ Π½ΠΈΠΌΠΈ Π³ΡΠ°Π½ΠΈΡΠΎΠΈΠ΄Ρ ΠΈ ΠΈΠ½ΡΡΠ·ΠΈΠ²Π½ΡΠ΅ ΠΎΠ±ΡΠ°Π·ΠΎΠ²Π°Π½ΠΈΡ ΠΎΡΠ½ΠΎΠ²Π½ΠΎΠ³ΠΎ ΡΠΎΡΡΠ°Π²Π°. ΠΠ΅Π·Π½Π°ΡΠΈΡΠ΅Π»ΡΠ½Π°Ρ ΡΠ°ΡΡΡ Ρ
ΠΎΡΠΎΡΠΎ ΠΎΠΊΠ°ΡΠ°Π½Π½ΡΡ
Π·Π΅ΡΠ΅Π½ ΡΠΈΡΠΊΠΎΠ½Π° Ρ Π΄ΠΎΡΠΈΡΠ΅ΠΉΡΠΊΠΈΠΌΠΈ Π΄Π°ΡΠΈΡΠΎΠ²ΠΊΠ°ΠΌΠΈ ΠΌΠΎΠΆΠ΅Ρ Π±ΡΡΡ ΠΏΠ΅ΡΠ΅ΠΎΡΠ»ΠΎΠΆΠ΅Π½Π° ΠΈΠ· ΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΌΠ΅ΡΠ°ΠΎΡΠ°Π΄ΠΎΡΠ½ΡΡ
ΠΎΠ±ΡΠ°Π·ΠΎΠ²Π°Π½ΠΈΠΉ, Π² ΡΠ²ΠΎΡ ΠΎΡΠ΅ΡΠ΅Π΄Ρ ΡΠ½Π°ΡΠ»Π΅Π΄ΠΎΠ²Π°Π²ΡΠΈΡ
Π΅Π³ΠΎ ΠΈΠ· ΠΏΠΎΡΠΎΠ΄ Π΄ΡΠ΅Π²Π½Π΅Π³ΠΎ ΡΡΠ½Π΄Π°ΠΌΠ΅Π½ΡΠ° ΠΠΎΡΡΠΎΡΠ½ΠΎ-ΠΠ²ΡΠΎΠΏΠ΅ΠΉΡΠΊΠΎΠΉ ΠΏΠ»Π°ΡΡΠΎΡΠΌΡ
Π‘Π°ΠΌΠΎΡΠΎΠ΄Π½Π°Ρ ΠΏΠ»Π°ΡΠΈΠ½Π° Π² Ρ ΠΎΠ½Π΄ΡΠΈΡΠ΅
The article presents the first results of the study of native platinum extracted from chondrite. The native platinum forms microinclusions in carbonaceous matter andchromites, which are found in ordinary chondrite. Native platinum forms micrograins and aggregates of cubic microcrystals, most of which are free from impurities. The composition of platinum-containing chromites corresponds to terrestrial analogues of ultrabasic mantle rocks. Assumption about the magmatic origin of platinum-containing carbon is made.ΠΡΠΈΠ²Π΅Π΄Π΅Π½Ρ ΠΏΠ΅ΡΠ²ΡΠ΅ ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΡ ΠΈΠ·ΡΡΠ΅Π½ΠΈΡ ΡΠ°ΠΌΠΎΡΠΎΠ΄Π½ΠΎΠΉ ΠΏΠ»Π°ΡΠΈΠ½Ρ, ΠΌΠΈΠΊΡΠΎΠ²ΠΊΠ»ΡΡΠ΅Π½ΠΈΡ ΠΊΠΎΡΠΎΡΠΎΠΉ ΠΎΠ±Π½Π°ΡΡΠΆΠ΅Π½Ρ Π² ΡΠ³Π»Π΅ΡΠΎΠ΄ΠΈΡΡΠΎΠΌ Π²Π΅ΡΠ΅ΡΡΠ²Π΅ ΠΈ Ρ
ΡΠΎΠΌΠΈΡΠ°Ρ
ΠΈΠ· ΠΎΠ±ΡΠΊΠ½ΠΎΠ²Π΅Π½Π½ΠΎΠ³ΠΎ Ρ
ΠΎΠ½Π΄ΡΠΈΡΠ°. Π‘Π°ΠΌΠΎΡΠΎΠ΄Π½Π°Ρ ΠΏΠ»Π°ΡΠΈΠ½Π° ΠΎΠ±ΡΠ°Π·ΡΠ΅Ρ ΠΌΠ΅Π»ΠΊΠΈΠ΅ Π·Π΅ΡΠ½Π° ΠΈ ΡΡΠΎΡΡΠΊΠΈ ΠΊΡΠ±ΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΌΠΈΠΊΡΠΎΠΊΡΠΈΡΡΠ°Π»Π»ΠΎΠ², Π±ΠΎΠ»ΡΡΠΈΠ½ΡΡΠ²ΠΎ ΠΊΠΎΡΠΎΡΡΡ
ΡΠ²ΠΎΠ±ΠΎΠ΄Π½Ρ ΠΎΡ ΠΏΡΠΈΠΌΠ΅ΡΠ΅ΠΉ. ΠΠΏΡΠ΅Π΄Π΅Π»Π΅Π½ ΡΠΎΡΡΠ°Π² ΡΠΎΠ΄Π΅ΡΠΆΠ°ΡΠΈΡ
ΠΏΠ»Π°ΡΠΈΠ½Ρ Ρ
ΡΠΎΠΌΡΠΏΠΈΠ½Π΅Π»ΠΈΠ΄ΠΎΠ² ΠΈ ΡΡΡΠ°Π½ΠΎΠ²Π»Π΅Π½ΠΎ, ΡΡΠΎ ΠΎΠ½ ΡΠΎΠΎΡΠ²Π΅ΡΡΡΠ²ΡΠ΅Ρ Π·Π΅ΠΌΠ½ΡΠΌ Π°Π½Π°Π»ΠΎΠ³Π°ΠΌ ΠΈΠ· ΡΠ»ΡΡΡΠ°ΠΎΡΠ½ΠΎΠ²Π½ΡΡ
ΠΏΠΎΡΠΎΠ΄ ΠΌΠ°Π½ΡΠΈΠΉΠ½ΠΎΠ³ΠΎ ΠΏΡΠΎΠΈΡΡ
ΠΎΠΆΠ΄Π΅Π½ΠΈΡ. Π‘Π΄Π΅Π»Π°Π½ΠΎ ΠΏΡΠ΅Π΄ΠΏΠΎΠ»ΠΎΠΆΠ΅Π½ΠΈΠ΅ ΠΎ ΠΌΠ°Π³ΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΎΠΌ ΠΏΡΠΎΠΈΡΡ
ΠΎΠΆΠ΄Π΅Π½ΠΈΠΈ ΡΠΎΠ΄Π΅ΡΠΆΠ°ΡΠ΅Π³ΠΎ ΠΏΠ»Π°ΡΠΈΠ½Ρ ΡΠ³Π»Π΅ΡΠΎΠ΄Π°
CORECLUST: identification of the conserved CRM grammar together with prediction of gene regulation
Identification of transcriptional regulatory regions and tracing their internal organization are important for understanding the eukaryotic cell machinery. Cis-regulatory modules (CRMs) of higher eukaryotes are believed to possess a regulatory βgrammarβ, or preferred arrangement of binding sites, that is crucial for proper regulation and thus tends to be evolutionarily conserved. Here, we present a method CORECLUST (COnservative REgulatory CLUster STructure) that predicts CRMs based on a set of positional weight matrices. Given regulatory regions of orthologous and/or co-regulated genes, CORECLUST constructs a CRM model by revealing the conserved rules that describe the relative location of binding sites. The constructed model may be consequently used for the genome-wide prediction of similar CRMs, and thus detection of co-regulated genes, and for the investigation of the regulatory grammar of the system. Compared with related methods, CORECLUST shows better performance at identification of CRMs conferring muscle-specific gene expression in vertebrates and early-developmental CRMs in Drosophila
Phase Equilibrium and Interdiffusion in Blends of Polystyrene with Polyacrylates
The solubility and interdiffusion of polystyrene (PS) with polymethyl acrylate (PMA), polyethyl acrylate (PEA), polybutyl acrylate (PBA), and polyethylhexyl acrylate (PEHA) have been studied by the optical interferometry method. Phase state diagrams are plotted. It is shown that they are characterized by the upper critical solution temperatures (UCST), which are localized in the temperature range above 450 K. Pair interaction parameters and their temperature dependences are determined and analyzed. Extrapolation of the temperature dependence of the interaction parameter was used to construct the dome of binodal curves and determine the spinodal curves in the framework of the FloryβHuggins theory. The diffusion coefficients of polystyrene into polyacrylates and polyacrylates into polystyrene are calculated. The dependences of the interdiffusion coefficients on the concentration, temperature, polystyrene molecular weight, and the number of carbons in the side chain of polyacrylate are analyzed. The numerical values of the interdiffusion coefficients of PS-1 into polyacrylates at 433 K change as β8.5 β β6.7 β β6.4 in the homologous series PMA β PEA β PBA. The coefficients of friction are calculated and the effect of change in the matrix structure on the diffusion of polystyrene in them is estimated
Life-purpose orientations of todayβs university students of a multicultural region
You The article presents an empirical study of the life-purpose orientations of thirdand fourth-year students of various directions of undergraduate training: βPsychologyβ, βEnvironmental sciencesβ, βEconomicsβ, βLawβ of the Volga Humanitarian Institute (branch) of Volgograd State University. The study used the Life-Purpose Orientations Test (LPO technique) of D.A. Leontiev as the main technique. The results of respondents in this sample correspond to the average level of indicators on all scales. In addition, students were offered the authorβs questionnaire βWhat is valuable to you?β An analysis of the answers led to the conclusion that spiritual values are a priority for almost all students and βFamilyβ is the most significant value
Simulation of Binodal and Spinodal Curves of Phase State Diagrams for Binary Polymer Systems
A new approach is proposed for simulating binodal and spinodal curves of phase diagrams for binary polymer systems. It is shown that the Flory–Huggins theory makes it possible to predict phase behavior in a wide range of temperatures and concentrations based on limited data on the components’ solubility. The approbation data of the technique are presented in the example of PS–PB and PS–PMMA systems, for which generalized phase diagrams are constructed
Organization of IT-Based Socio-Pedagogical Research by Students of Pedagogical University
Π ΡΠ°Π±ΠΎΡΠ΅ ΠΎΠΏΠΈΡΠ°Π½ ΠΎΠΏΡΡ ΠΎΡΠ³Π°Π½ΠΈΠ·Π°ΡΠΈΠΈ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°ΡΠ΅Π»ΡΡΠΊΠΎΠΉ ΡΠ°Π±ΠΎΡΡ ΡΡΡΠ΄Π΅Π½ΡΠΎΠ² ΠΏΠ΅Π΄Π°Π³ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΠΏΠ΅ΡΠΈΠ°Π»ΡΠ½ΠΎΡΡΠ΅ΠΉ ΠΏΡΠΈ ΠΈΠ·ΡΡΠ΅Π½ΠΈΠΈ Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊ ΠΈ ΡΡΠ»ΠΎΠ²ΠΈΠΉ ΡΡΠ΅Π±Π½ΠΎΠ³ΠΎ ΠΏΡΠΎΡΠ΅ΡΡΠ° Π½Π° Π±Π°Π·Π΅ on-line ΠΎΠΏΡΠΎΡΠΎΠ². ΠΡΠΎΠ°Π½Π°Π»ΠΈΠ·ΠΈΡΠΎΠ²Π°Π½Ρ ΠΎΡΠ½ΠΎΠ²Π½ΡΠ΅ Π²ΠΈΠ΄Ρ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°ΡΠ΅Π»ΡΡΠΊΠΎΠΉ Π΄Π΅ΡΡΠ΅Π»ΡΠ½ΠΎΡΡΠΈ, ΡΠ΅ΡΡΡΡΡ ΠΈΡ
ΠΏΠΎΠ΄Π΄Π΅ΡΠΆΠΊΠΈ ΠΈ ΠΏΡΠ°ΠΊΡΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΡ.The paper deals the experience of organizing research work of students of pedagogical specialties in studying the characteristics and conditions of the educational process by on-line surveys. It was analyzed the main types of research activities, their support resources and practical results
Π₯Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊΠΈ ΠΌΠ΅ΡΠ°ΠΏΠ΅ΡΡΠ°Π½ΠΈΠΊΠΎΠ² ΡΠ²Π΅ΡΠ»ΠΈΠ½ΡΠΊΠΎΠΉ ΡΠ²ΠΈΡΡ β ΡΡΠ±ΡΡΡΠ°ΡΠ° ΡΠ΅Π»ΠΎΡΠ½ΡΡ ΡΡΠ΄Π½ΡΡ ΠΌΠ΅ΡΠ°ΡΠΎΠΌΠ°ΡΠΈΡΠΎΠ² (ΠΠΊΡΡΠ±ΡΡΡΠΊΠΎΠ΅ ΡΡΠ΄Π½ΠΎΠ΅ ΠΏΠΎΠ»Π΅, Π‘ΡΠ΅Π΄Π½ΠΈΠΉ Π’ΠΈΠΌΠ°Π½)
The paper considers the characteristics of the meta sandstones of the Svetlinskaya Suite developed within the Oktyabrskoe ore field at the Chetlas Stone (Middle Timan) and serving as a substrate for ore alkaline metasomatites. The main source of detrital material for fine-grained feldspar-quartz metasandstones during their formation were the meta-sedimentary and, to a lesser extent, acidic igneous rocks, including those altered in the weathering crust. The formation of metapsammites took place under relatively stable tectonic conditions of the passive continental margin.Π Π°ΡΡΠΌΠΎΡΡΠ΅Π½Ρ Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊΠΈ ΠΌΠ΅ΡΠ°ΠΏΠ΅ΡΡΠ°Π½ΠΈΠΊΠΎΠ² ΡΠ²Π΅ΡΠ»ΠΈΠ½ΡΠΊΠΎΠΉ ΡΠ²ΠΈΡΡ, ΡΠ°Π·Π²ΠΈΡΡΡ
Π² ΠΏΡΠ΅Π΄Π΅Π»Π°Ρ
ΠΠΊΡΡΠ±ΡΡΡΠΊΠΎΠ³ΠΎ ΡΡΠ΄Π½ΠΎΠ³ΠΎ ΠΏΠΎΠ»Ρ Π½Π° Π§Π΅ΡΠ»Π°ΡΡΠΊΠΎΠΌ ΠΠ°ΠΌΠ½Π΅ (Π‘ΡΠ΅Π΄Π½ΠΈΠΉ Π’ΠΈΠΌΠ°Π½) ΠΈ ΡΠ»ΡΠΆΠ°ΡΠΈΡ
ΡΡΠ±ΡΡΡΠ°ΡΠΎΠΌ ΡΡΠ΄Π½ΡΡ
ΡΠ΅Π»ΠΎΡΠ½ΡΡ
ΠΌΠ΅ΡΠ°ΡΠΎΠΌΠ°ΡΠΈΡΠΎΠ². ΠΡΠ½ΠΎΠ²Π½ΡΠΌ ΠΈΡΡΠΎΡΠ½ΠΈΠΊΠΎΠΌ ΠΎΠ±Π»ΠΎΠΌΠΎΡΠ½ΠΎΠ³ΠΎ ΠΌΠ°ΡΠ΅ΡΠΈΠ°Π»Π° ΠΏΡΠΈ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΠΈ ΠΏΠΎΠ»Π΅Π²ΠΎΡΠΏΠ°Ρ-ΠΊΠ²Π°ΡΡΠ΅Π²ΡΡ
ΠΌΠ΅Π»ΠΊΠΎΠ·Π΅ΡΠ½ΠΈΡΡΡΡ
ΠΌΠ΅ΡΠ°ΠΏΠ΅ΡΡΠ°Π½ΠΈΠΊΠΎΠ² Π±ΡΠ»ΠΈ ΠΌΠ΅ΡΠ°ΠΎΡΠ°Π΄ΠΎΡΠ½ΡΠ΅ ΠΈ, Π² ΠΌΠ΅Π½ΡΡΠ΅ΠΉ ΡΡΠ΅ΠΏΠ΅Π½ΠΈ, ΠΊΠΈΡΠ»ΡΠ΅ ΠΌΠ°Π³ΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΏΠΎΡΠΎΠ΄Ρ, Π² ΡΠΎΠΌ ΡΠΈΡΠ»Π΅ ΠΈΠ·ΠΌΠ΅Π½Π΅Π½Π½ΡΠ΅ Π² ΠΊΠΎΡΠ΅ Π²ΡΠ²Π΅ΡΡΠΈΠ²Π°Π½ΠΈΡ. ΠΠ±ΡΠ°Π·ΠΎΠ²Π°Π½ΠΈΠ΅ ΠΏΠ΅ΡΡΠ°Π½ΠΈΠΊΠΎΠ² ΠΏΡΠΎΡ
ΠΎΠ΄ΠΈΠ»ΠΎ Π² ΠΎΡΠ½ΠΎΡΠΈΡΠ΅Π»ΡΠ½ΠΎ ΡΡΠ°Π±ΠΈΠ»ΡΠ½ΡΡ
ΡΠ΅ΠΊΡΠΎΠ½ΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΡΠ»ΠΎΠ²ΠΈΡΡ
ΠΏΠ°ΡΡΠΈΠ²Π½ΠΎΠΉ ΠΊΠΎΠ½ΡΠΈΠ½Π΅Π½ΡΠ°Π»ΡΠ½ΠΎΠΉ ΠΎΠΊΡΠ°ΠΈΠ½Ρ