Vol 24, No 1 (2024)

Articles

SEICHE DYNAMICS IN THE AZOV SEA CURRENT SYSTEM

Matishov G., Grigorenko K.

Abstract

The paper presents new results of an investigations of the cyclic currents of the Azov Sea. Using offshore and onshore surveys at buoy ADCP-stations the separation of the characteristic features of water transport in different areas of the Taganrog Bay was shown. Expeditionary observations showed that despite of the drift-gradient nature, the resulting current has the direction of the Don runoff current. Direct coastal measurements showed that the runoff current significantly predominates on the spits of the southern coast of Taganrog Bay. Seiche pulsations manifest themselves as a two to three-hour slowdown of the main flow at diurnal intervals. The division of the areas of the Taganrog Bay according to the trajectories of water movement is noticeable. The eastern part has a predominantly river regime of water circulation. In the central part the meridional component of seiche currents plays an important role in water mixing. The marine regime of water mixing prevails in the western part of the Taganrog bay. Test calculations show that the classical tidal analysis program T_TIDE is applicable with caution for the Sea of Azov. The visually observed diurnal and semi-diurnal sea level rises represent a superposition of waves of different natures. The results of the work correspond to the known patterns of energy exchange between the atmosphere and the ocean. Even weak winds lead to the development of wave processes at eigen frequencies close to tidal ones. Increasing winds contribute to the intensification of wave fluctuations and significant transfer of water during strong surges.
Russian Journal of Earth Sciences. 2024;24(1):ES1001
pages ES1001 views

ACCUMULATION OF TECHNOGENIC AND NATURAL RADIONUCLIDES IN THE DON DELTA SEDIMENTS

Matishov G., Ilyin G., Polshin V., Usyagina I.

Abstract

The study of current sedimentation processes and radioactive contamination in the total area of the Don Delta is the research goal. The presented paper contains data analysis of radioecological and lithologic studies on bottom sediments, sampled in the northern part of the Don Delta in 2022. Based on the research results obtained, the authors provide the characteristics of the current conditions of sedimentation and specific activity of artificial and natural radionuclides in fluvial deposits, as well as indicate that similar in characteristics sandy-silty aleurites and sandy aleurite-clayish silts with inclusions of plant and shell detritus compose the bottom sediments of numerous braided channels. The authors determined the zonal accumulation character of both 137Cs technogenic and 226Ra, 40K, and 232Th natural radionuclides which conditions their accumulation and content increase from the lower delta to the upper delta areas. The velocity of currents in the braided channels (bayous) and related sedimentation conditions of suspended matter, as well as the lithotype of the bottom ground determine the indicated regularity. We assume that unlike 137Cs the distribution of natural radionuclides (40K, 226Ra, and 232Th) mainly depends on the mineral content of sediments entering the delta with the river runoff. Relatively low indices – on average ca. 9 Bq/kg of dry weight (d.w.) – characterise the current range of 137Cs radioisotope concentrations in the sediments of the Northern Don Delta. Such a level of specific activity is of no danger to the regional ecosystem.
Russian Journal of Earth Sciences. 2024;24(1):ES1002
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HIGH RESOLUTION SEISMICITY SMOOTHING METHOD FOR SEISMIC HAZARD ASSESSMENT

Vorobieva I., Grekov E., Krushelnitskii K., Malyutin P., Shebalin P.

Abstract

A high resolution smoothing method is proposed for performing local estimates of the parameters of the Gutenberg-Richter law (GR). Using this method, the smoothing radius can be chosen large enough to ensure that the condition of applicability of GR law is met, while the distinguished areas of high activity align well with the distribution of epicenters and there is no “smearing” of narrow areas of really high seismic activity into wider zones, which are not actually active at the edges.
Russian Journal of Earth Sciences. 2024;24(1):ES1003
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CURRENT ISSUES PROBLEMS OF GEOINFORMATICS

Rozenberg I., Dulin S.

Abstract

Geoinformatics is a scientific discipline that focuses on natural, technical, and socioeconomic spatial systems studied through computer modeling of localized objects and phenomena. The main goals of geoinformatics as a science are visualization, localization, and decision-making regarding spatial transformations of the environment. The structure of geoinformatics includes such sections as geosystem modeling, spatial analysis, and applied geoinformatics itself. The development of technologies for collecting, storing, converting and exchanging spatial and temporal data has led to the rapid development of GIS technologies and the emergence of a wide variety of industrial GIS aimed at processing geodata in order to make informed decisions. Currently, geoinformatics in many industries is perceived as a geoinformation industry, which implies the presence of its own equipment, the development of commercial software products such as GIS, a staff of experienced expert analysts and the organization of marketing. The paper highlights three of the most pressing problems faced by researchers in the field of geoinformatics over the past two decades: interoperability, digital transformation, and geodata fusion. The characteristic features of these problems and some aspects of their solution are considered.
Russian Journal of Earth Sciences. 2024;24(1):ES1004
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INFORMATION SUPPORT FOR GEOMECHANICAL CALCULATIONS OF STABILITY OF THE UNDERMINED ROCK MASS WITH A COMPLEX TECTONIC STRUCTURE

Baryakh A.A., Sanfirov I.A., Dyakonov M.V., Lobanov S.Y., Nikiforova A.I.

Abstract

Using the example of the Tyubegatan potash deposit (Uzbekistan), a complex of geophysical and geomechanical safety assurance for mining operations in conditions of the complex tectonic structure of the undermined rock mass is considered. Geophysical research included ground-based seismic surveys using a profile system in combination with «light» standard electro- and gravimetric techniques. Based on the results of these works, a physical and geological model of the deposit areas was built with the weakened zones and faults localization. As part of the meaningful interpretation, the physical and geological model was transformed into a geomechanical calculation scheme, which reflected the main mining-geological and mining-technical condition of development and was based on a model of elastoplastic deformation of salt rocks. The geomechanical model was calibrated from radar interferometric surveys. The time factor was taken into account in accordance with the developed modification of the well-known method of variable deformation modules. The formation of plasticity zones in physical terms was identified with the formation of fracturing areas in the water protection layer, which determine the danger of violating its continuity. Numerical implementation of the geomechanical model using the finite element method made it possible to substantiate the optimal parameters of the chamber development system, ensuring the safety of the water protection layer, including fault zones.
Russian Journal of Earth Sciences. 2024;24(1):ES1005
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THE POLYMETALLIC DEPOSITS OF THE WESTERN EUROPEAN PLATE AND STRUCTURE OF THE EARTH'S CRUST ACCORDING TO GOCE GRAVITY DATA

Galyamov A., Volkov A., Lobanov K.

Abstract

For the first time, the results of modern studies of the earth's crust based on gravity data from the GOCE satellite Project are used for a comparative regional metallogenic analysis of the geodynamic settings of the formation of polymetallic deposits in Western Europe and the Mediterranean segment of the Tethys belt. It is shown that exhalative sulfide deposits (SEDEX) and cuprous sandstones and shales (SSC) are mainly located in the earth's crust with a predominant development of the lower “basalt” layer of the earth's crust. Pyrite copper and lead-zinc deposits in volcanogenic rocks (VMS), as well as some occurrences of the SEDEX type, are found in supra-subduction island-arc and accretionary crustal settings with a predominant development of the middle “granite” layer. Lead-zinc ores of the Mississippi type (MVT) are localized in deep pericratonic sedimentary basins with petroleum-bearing specialization on the shelf and continental slope, regardless of the stratification of the earth's crust. The results obtained can be used for regional forecasting and metallogenic constructions, prospecting and assessment of new deposits.
Russian Journal of Earth Sciences. 2024;24(1):ES1006
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STRUCTURAL TECTONIC SCHEME CREATION BASED ON SEISMIC-GRAVITY MODELS AND ISOSTASY USAGE: URAL CASE

Martyshko P., Ladovskii I., Byzov D., Cidaev A.

Abstract

Process of Earth’s density models creation leads to the solution of direct and inverse gravimetry problems. The inverse problem of gravimetry is a classic example of an ill-posed problem: in the common statement, its solution is not unique and unstably depends on input data. Therefore, it is necessary to determine solutions belonging substantial sets of correctness, choosing reasonable models of an initial approximation. In this paper the application of complex interpretation methods of seismic and gravitational data for the creation of three-dimensional models of crust and the upper mantle are presented. Original algorithms and programs were developed for implementation of these methods. They contain solution of non-linear (structural) inverse problem and the solution of the linear three-dimensional inverse problem taking note of the side sources. Coefficients of the “density-velocity” correlation formulas for a number of geo-traverses were defined. Also, we suggest a technique of tectonic maps construction, which is based on the lithostatic pressure calculation. Its idea can be applied to both two- and three-dimensional cases. In the 2D case we show the way to split the mantle to blocks with vertical boundaries. If lithostatic compensation hypothesis is adopted, the method also allows one to calculate density value for each block. Such separation of the mantle helps to diminish discrepancy between model and observed fields. In 3D case we suggest a method, which can be used to construct tectonic structure maps with information about approximate depth and height of each tectonic block.
Russian Journal of Earth Sciences. 2024;24(1):ES1007
pages ES1007 views

THE ROLE OF PLACER DEPOSITS IN ENSURING THE REPRODUCTION OF THE MINERAL RESOURCE BASE OF SCARCE TYPES OF STRATEGIC MINERAL RAW MATERIALS IN RUSSIA AT THE PRESENT STAGE

Bortnikov N.S., Volkov A.V., Lalomov A.V., Bochneva A.A., Ivanova Y.N., Lalomov D.A.

Abstract

Placer deposits had (and for a number of components still have) an important role in providing strategic types of mineral resource base for both Russia and the world as a whole. Placers have a number of advantages that make them in demand by the mining industry: relatively shallow (often accessible for open-pit mining) occurrence, disintegrated state of productive deposits, simplicity of enrichment processes (mainly gravitational systems), as well as the possibility of rapid involvement in exploitation, which significantly reduces payback period for investments. All this is even more relevant for modern Russia, when, in the shortest possible time, in conditions of a shortage of credit resources, it is necessary to implement a program of import substitution and provide the country with scarce types of strategic mineral raw materials, such as gold, platinum group metals, tin, rare metals, titanium, chromium, diamonds.
Russian Journal of Earth Sciences. 2024;24(1):ES1008
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A GLOBAL VIEW ON INTERNAL TIDES

Morozov E.

Abstract

This is a review paper on generation of internal tides in the global ocean based on literature data and publications of the author. Energy fluxes of semidiurnal internal tide generation over submarine ridges were estimated based on modeling and measurements on moorings in many regions of the ocean. Data from 4000 moorings during a period of 50 years are considered. Regions of intense generation of internal tides are indicated. They are related to several underwater oceanic ridges. Energy fluxes from submarine ridges greatly exceed those from the continental slopes because generally the currents of the barotropic tide are parallel to the coastline. If the barotropic tide currents are normal to the ridge, they generate strong internal tides. They account approximately for one fourth of the energy losses of the barotropic tide. Decay of internal tide during propagation was estimated based on the data from lines of moorings located normal to the ridges. Model simulations and moored measurements result in a global map of semidiurnal internal tide amplitudes
Russian Journal of Earth Sciences. 2024;24(1):ES1009
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A CLOSER COOPERATION BETWEEN SPACE AND SEISMOLOGY COMMUNITIES – A WAY TO AVOID ERRORS IN HUNTING FOR EARTHQUAKE PRECURSORS

Pilipenko V., Shiokawa K.

Abstract

The space physicists and the earthquake (EQ) prediction community exploit the same instruments – magnetometers, but for different tasks: space physicists try to comprehend the global electrodynamics of near-Earth space on various time scales, whereas the seismic community develops electromagnetic methods of short-term EQ prediction. The lack of deep collaboration between those communities may result sometimes in erroneous conclusions. In this critical review, we demonstrate some incorrect results caused by a neglect of specifics of geomagnetic field evolution during space weather activation. The considered examples comprise: Magnetic storms as a trigger of EQs; ULF waves as a global EQ precursor; Geomagnetic impulses before seismic shocks; Long-period geomagnetic disturbances generated by strong EQs; Discrimination of underground ULF sources by amplitude-phase gradients; Depression of ULF power as a short-term EQ precursor; and Detection of seimogenic emissions by satellites. To verify the reliability of the above widely disseminated results data from available arrays of fluxgate and search-coil magnetometers have been re-analyzed. In all considered events, the “anomalous” geomagnetic field behavior can be explained by global geomagnetic activity, and it is apparently not associated with seismic activity. This critical review does not claim that ULF electromagnetic field cannot be used as a sensitive indicator of the EQ preparation processes, but we suggest that both communities must cooperate their studies more tightly using data exchange, combined usage of magnetometer networks, organization of CDAW for unique events, etc.
Russian Journal of Earth Sciences. 2024;24(1):ES1010
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THE CYCLOSTRATIGRAPHY OF THE EASTERN PARATETHYS KONKIAN: ZELENSKY SECTION (TAMAN PENINSULA)

Rostovtseva Y.

Abstract

The Eastern Paratethys Konkian sedimentary successions of the Zelensky section (Taman peninsula, Russia) were investigated by cyclostratigraphy methods based on magnetic susceptibility measurements. Cyclostratigraphy is a new scientific direction in stratigraphy and sedimentology, the purpose of which is to identify astronomical cyclicity for the reconstruction geochronology using high-precision technologies. Time series analysis (Lomb-Scargle and REDFIT periodograms, wavelet) revealed statistically significant signals corresponding most likely to long-term insolation periodicities in studied sediments. In the deep-water Konkian sediments of the Zelensky section, the signal at 3.3 m corresponds to the 100-kyr eccentricity cycle. The astronomically tuned these sediments result in an average sedimentation rate of about 3.3 cm/kyr with the duration of accumulation of the Sartaganian and Veselyankian beds about 200 kyr. The obtained cyclostratigraphic results generally do not contradict the new data about the possible duration of the Konkian (Kartvelian, Sartaganian and Veselyankian beds) of about 750 kyr [Palcu et al., 2017].
Russian Journal of Earth Sciences. 2024;24(1):ES1011
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WORLD SEISMIC NETWORKS AND EARTHQUAKE CATALOGS

Gvishiani A.D., Dzeranov B.V., Skorkina A.A., Dzeboev B.A.

Abstract

This paper is devoted to the review of currently functioning seismological agencies, seismic monitoring networks created, developed and supported by them, as well as earthquake catalogs produced. Particular attention is focused on international and national seismological centers and seismic networks. A historical insight about the first observations made by seismic networks completes the picture. The basic parameters of the main seismic networks and the principles of functioning for seismological centers are considered. The key characteristics of seismic catalogs that determine the criteria for their quality are discussed. The system-analytical approach to solving the urgent problem of creating the most complete and representative earthquake catalogs with a unified magnitude scale by integrating data from international, national and regional catalogs in the studied region is presented.
Russian Journal of Earth Sciences. 2024;24(1):ES1012
pages ES1012 views

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