Наведено результати вивчення структурних особливостей Старошепелицької ділянки Чорнобильської зони відчуження (ЗВ), яка відібрана як полігон для дослідження геодинамічних зон. Комплексно проаналізовано результати структурного дешифрування матеріалів дистанційних зйомок (МДЗ), а також детальних геофізичних (геоелектричних, сейсмоакустичних, магнітометричних) досліджень. Одержано нові дані, які значно доповнили геолого-геофізичну модель структури ділянки. Виявлено, що мережа елементарних лінеаментів і їх зон у цілому простежується вздовж складно побудованих геодинамічних субвертикальних зон напружено-деформаційного стану гірських порід, що індицирує наявність локальних диз'юнктивних порушень. Даним зонам відповідають неоднорідності геофізичних полів.

Приведены результаты изучения структурных особенностей Старошепелицкого участка Чернобыльской зоны отчуждения, который отобран в качестве полигона по исследованию геодинамических зон. Комплексно проанализированы результаты структурного дешифрирования материалов дистанционных съемок, а также детальных геофизических (геоэлектрических, сейсмоакустических, магнитометрических) исследований. Получены новые данные, которые значительно дополняют геолого-геофизическую модель структуры участка. Установлено, что сеть элементарных линеаментов и их зон в целом прослеживается вдоль сложно построенных геодинамических субвертикальных зон напряженно-деформационного состояния горных пород, таким образом индицируя наличие локальных дизъюнктивных нарушений. Указанным зонам соответствуют неоднородности геофизических полей.

The results of structure feature investigation on the Staroshepelychy district of the Chornobyl Exclusion Zone are highlighed. The district was selected as an example for the study of the test sites with geodynamic zones. The results of structural decoding of remote sensing data as well as results of geophysical (geoelectrical, seismoacoustic, magnetometric) survey have been analyzed integrally. New data completing a geological-geophysical model of the district have been received. It is determined that the network elementary lineaments and their zones trace generally along the compound built geodynamic subvertical zones of the stressed-deformational state of rock that induces the local ruptures existence. The heterogeneities of geophysical fields are corresponded to the zones.

Викладено результати вимірювань льодової потужності льодовика Домашній, що розташований на острові Галіндез, та льодовиків Малий Уіггенс і Великий Уіггенс - на Антарктичному півострові, виконаних за допомогою методів радіолокації й електрорезонансного зондування.

The results of geoelectric and seismic-acoustic investigations on the two ravine area in Odessa region are given. The depths of lying of main water horizon and separate water lenses are determined. The zones of vertical migration of underground water are installed. The organization of the dumps in investigation regions in not possible with ecological standpoint.

During the seasonal works of the 9-th Ukrainian Antarctic Expedition the thickness of the ice cap situated near the Academic Vernadsky station on the Galindez Island was measured. This problem was solved by the vertical electric-resonance sounding method that is widely used in solving different ecological, geologic-geophysical and geologic-engineering problems. Results of these works were used to set up: a sketch-map and 3-D diagram of the ice cap thickness on Galindez Island; vertical sections of the glacier mass along five profiles; sketch-map and 3-D diagrams of the Galindez Island surface both with the ice cap and without it. Researches the carried out show that the vertical electric-resonance sounding method can be effectively used for the West Antarctica studying of the ice cap structure.

The results of geological geophysical and reconnaissance geoelectrical investigations in the oil and gas perspective areas in the west ern part of the Kherson region are presented. The field observations data enable to select the geoelectrical field anomaly with which the hydrocarbons deposit can be bound.

The results of geoelectric and seismic-acoustic investigations on the Sophya Kyivska Cathedral territory in Kyiv are given. The foundation thickness and depth of the Cathedral and Bell Tower were determined. The zones with increased ground moistening were mapped. The geological-geophysical and acoustic cross-sections along some lines were constructed. The crystalline basement depth was determined by the electric-resonance method. The received data show that geoelectric and seismic-acoustic methods may be used for the historical and architectural preserve territory and building monitoring.

The results of geoelectric and seismic-acoustic investigations on the Zverynitskiye Caves territory in Kyiv are given. The areas of the underground passages possible continuation were determined. The zones with increased ground moistening were mapped.

The new results of the geoelectric investigations within the Karsak dome structure in Western Kazakhstan are given. The received data show that the geoelectric methods allow to find and to map the over-salt and sub-salt layers of anomaly polarized stratum, in which the hydrocarbons can be present.

The results of collation of geoelectric investigation data on the Western Kazakhstan oilfield in view of seismic and boring data are given. It is shown that geoelectic "oil-and-gas deposit" type anomalies coincides in plan on 60 % and resemble more the stated sidebars of the oil-and-gas fields. It is recommended to conduct the reconnaissance geoelectric studies ahead of seismic work in view of the main direction determination for the hydrocarbons search.

Some results of the investigations within exploratory block R-9 with using the technology of direct searching for hydrocarbon deposits are given. The studies carried out demonstrate high efficiency of this technology, allowing studying the significant area of the territory for a short time.

A method of electroresonance sounding is described. It is based on studying the processes of natural polarization of medium and spectral features of natural electric field over investigation objects. The method allows to define the location depths of the stratigraphic cross-section complexes and separate anomalous objects. The electric-resonance method efficiency is demonstrated by the results of its practical application at the ecological, engineering-geological and geological-geophysical problems solving.

The results of geoelectric investigation on the perspective in view of the oil and gaz Ludin area, which is situated within Volyn-Podolsk plate, are given. It is shown that "oil-and-gas deposit" type anomalies are mapped clearly by geoelectric methods. It is recommended to conduct the geoelectric studies together with another geophysical investigation with the aim to determine places for the exploration bore holes pawning.

The results of detailed geoelectric investigation on the M. I. Kalinin coal mine in Donetck with the reason of finding and contouring the area with raised concourse of the gas in coal layers and containing rocks are given. Three anomalous zones with raised gas content were mapped within mine field by the FSPEF grid survey. The depths of bedding and thickness of the rock layers with raised gas content were determined by VERZ method. The data of the geoelectric methods FSPEF and VERZ give additional information for the degassing bore holes optimum pawning. The possibility of these methods using for the coal layers mapping is shown.

The results of using geoelectric methods for searching and contouring zones with increased water containing rocks are given. The received data show that the geoelectric methods allow to map water-containing areas and to define theirs bedding depths.

The results of integrated application of geoelectric methods and low-frequency acoustic exploring for the hydrocarbon deposits searching on some structure of the exploratory block R-9 in Western Kazakhstan are given. The investigation has shown that low-frequency acoustic exploring ANCHAR with geoelectric survey by the method of forming short-pulsed electromagnetic field allows to realize effectively the studies area localization for detailed geophysical (including seismic) work undertaking.

The results of the ground penetrating radar (GPR) using for engineering-geological prospecting during reconstruction of the car road are given. It is shown that GPR allow to define the borders and thickness of the layer road covering, to reveal the zones of the soil moistening, stranger of the cutin in soil, spatial outlines of the sole layer, filtration way of the soil waters, as well as defects, admitting in process of the road work.

The results of the geoelectric methods using for investigation of the crystalline basement internal structure are given. The fracture zones and non-broken blocks were mapped within the investigated area by the FSPEF grid survey. The degree of integrity of crystalline massif in cross-section was determined by VERS method. When studying the fracture tectonic of the basement the FSPEF-VERS technology can be integrated with other geophysical methods.

The paper highlights the results of structure feature investigation in the Staroshepelychy plot of the Chernobyl Elimination Zone. The plot was chosen as an example for the study of the test sites with vertical mass transfer anomalous zones. The materials of structural decoding of remote sensing data and results of geophysical (geoelectrical, seismo-acoustic, magnetometric, georadar, Rn-Tn emanation ones) and hydrogeological survey have been analysed integrally. New data completing a geological-geophysical model of the plot have been obtained. It is determined that the network of elementary, lineaments and their zones trace generally along the geodynamic subvertical zones of complex structure with stress-strained state of rocks that induces of existence the local ruptures. These zones divide the local blocks with different hydrogeological parameters. The specific emanation anomalies and heterogeneities of geophysical fields correspond to the se zones. The zones are characterized by high migration properties of the enclosing rock.

Results of diagnosis of the hermetic scaling zone of tunnels at the depth of 15 - 20 m from the surface are presented. Geophysical investigations were conducted using the methods of seismic-acoustic sounding and formation of short-pulsed electromagnetic field. The GRP methods may be used to diagnose grounds under the tunnel bottom.

The results of geoelectric studies within Voronovskiy dome of Severodonetck area are given. The anomalies of "deposit" type are revealed and mapped, and intervals of lying of anomalous polarized layer (APL) of "hydrocarbon deposit" type are installed by geoelectric investigations. The geoelectric anomalies presence within area of the dome and the chosen APL of "gas deposit" type in geoelectric cross-section, point to practicability of the undertaking the search drilling works with purpose of the gas deposit discovery.