PALEOGIDROGEOHIMICHESKIE features of accumulation of bromine in SOUTHEASTERN Dnieper -Donetsk basin
Journal Title: Вісник Одеського національного університету. Географічні та геологічні науки - Year 2015, Vol 20, Issue 3
Abstract
Purpose. An attempt to establish a link between geotectonic development of the southeastern part of the Dnieper-Donets Basin and the accumulation of bromine in groundwater. The study involved the groundwater, and the subject of study – hydrogeochemical features of underground waters and the history of geological development of the territory. Data & Methods. The basis of the work was based on the technique of hydrogeochemical prospecting. The material appeared geological and hydrogeological data of the study area. Results. Formation of the chemical composition of groundwater occurs throughout the entire geological history of the area. In periods of tectonic activity zone of deep faults become a kind of channels, through which the water exchange between the different geogidrodinamic systems. The result of this interaction was the formation of hydrogeochemical anomalies of bromine. Thus, we can assume that there is a connection between the epochs of tectonic activity and of bromine in groundwaters.
Authors and Affiliations
O. V. Gavrilyuk
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