04.00.00 Geological-mineralogical sciences
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MICROBIOLOGICAL INFLUENCE ON UNDERGROUND PIPELINES IN UNDERFLOODED LOESSIAL SOILS
04.00.00 Geological-mineralogical sciences
Description
This article discusses Microbiological factor in processes of corrosion damage of metal underground pipelines in underflooded loessial soils. Aerobic corrosion and anaerobic corrosion is described
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METHODS OF PROTECTION AGAINST COASTAL LANDSLIDES
04.00.00 Geological-mineralogical sciences
Description
This article discusses the problem of protection of coastal areas of the Black and Azov seas. Landslides development mechanism is considered. Reasons for choosing a type and placement location of different landslide structures are given
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APPROACHES TO PERIODIZATION OF DESTRUCTION OF SOIL COVERING OF THE PLANET
04.00.00 Geological-mineralogical sciences
Description
The article deals with questions of sense and essence of changes which occurred with the soil covering of planet. Classification of these processes is given for the first time
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EXPLORATION OF TECTONIC PARAGENE-SISES, AND THEIR INFLUENCING ON THE HILLS CONSTITUTION
04.00.00 Geological-mineralogical sciences
Description
In this article, the tectonic framework of terrain of construction of a railway tunnel №6 is considered: mated automobile and railway Adler – Alpika – Ser-vice mountain-climate health resort. Endogenic allocation of a fracturing in a rocky block in directions and a density function on a block is learnt in details. The fracturing assaying on reference stages has demonstrated all spectrum of allocations of the basic linear flaws and the loosened bands
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04.00.00 Geological-mineralogical sciences
Description
This article discusses results of hydrogeological study including morphometric terrain analysis of irrigation systems of Syrt Plain. The author of this article tries to prove that irrigation of chestnut soil in Syrt Plain can be achieved without employing regular drainage systems by citing the example of long-term irrigation system employed by experimental station in the town of Ershov
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THE FILTRATION PROPERTIES FEATURES OF TECHNOGENIC DEPOSITS
04.00.00 Geological-mineralogical sciences
Description
The studies of synthetic sand deposits formed after working dredges deposits in river valleys, have established significant heterogeneity of filtration properties of elementary layers of sand of different grain size distribution. The features of the structure of the array of man-made structures provide a large capacity of absorption of suspended clay particles and the conditions for water purification by adsorption
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PHYSICAL AND MECHANICAL PROPERTIES OF GYPSUM AND GEOTECHNICAL CONDITIONS OF DEPOSIT BOGOMOLOVSKOYE
04.00.00 Geological-mineralogical sciences
Description
The article presents the evaluation of geotechnical conditions of gypsum Bogomolovskoye deposit, the Perm Region. It is shown, that the main influence on the conditions of the development of the field will have surface and underground karst
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INTEGRATED GEOECOLOGICAL ASSESSMENT OF MINING AND INDUSTRIAL AREAS OF THE NORTH URALS
04.00.00 Geological-mineralogical sciences
Description
In this article, the technique to an integrated geoecological assessment on an example of the mining and industrial region of Northern Ural is considered. The geoecological analysis shows that the main influence on the environment has mining and recent geodynamics
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REGIONAL FACTORS IN FORMING THE ENGINEERING AND GEOLOGICAL CONDITIONS OF THE PERM REGION
04.00.00 Geological-mineralogical sciences
Description
The article summarizes the main factors of regional engineering and geological conditions, and the results of zoning on the basis formation analysis and classification of engineering-geological conditions in the Perm region
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04.00.00 Geological-mineralogical sciences
Description
In West Karelia (Severny Prigranichny locality), an extension of the Hattu greenstone belt (Finland) was traced and diorite-tonalite and granodiorite complexes, similar in petrochemical characteristics to the Kuittila and Viluvaara complexes, and near-N-S-trending shear-zones, favourable for gold concentration, were revealed. Gold is most likely to occur in Kadilampi-type massives, in schistosity and silicification zones in them and in their haloes. Gold ore occurrences and mineralization points, such as Kadilampi, Kuslokki, Gornoye, Soluha, Kappala and some others, were located
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