In the paper the results of the conducted analysis of records of the registered seismic event which was take place 2011.01.14 in Kryvyi Rig and arguments in favour of determine this event as earthquake are presented.
Questions of the mathematics modeling of local and global processes of Geodynamics are examined. The model of the process must take into account all its sources at the same time. This demand can be ensured by simultaneously calculating variations from all results of observations of geodynamic features. This task is solved by the determination and use of properties of covariance functions for fields of observation results.
In the article the geodynamic conditions and facial peculiarities of formation of Proterozoic-Paleozoic black shale deposits of Volyno-Podillia are consided. The deciding role in formation of these deposits had mainly descending movements of Baikalian, Caledonian and Variscan foldings. Black shale deposits formation took place in bathyal environments of the north-western part of Volyno-Podillia in the zone of junction of Eastand West-European platforms.
Data on the history of geological evolution of the south-eastern part of zone of junction of Volyn-Podolsk plate and Carpathian foredeep are generalized. The main structural and tectonic elements are describe which are formed at different stages of development of this area. Geodynamic factors of formation of hydrocarbon traps are analyzed and the main prospective areas are selected.
Purpose. The aim of the work is to conduct the complex analysis of seismicity, geology, seismotectonics and difference scale geodynamic processes in the Tereblya-Rika hydro power station (HPS) area in the Ukrainian Transcarpathians (23.35-23.87ºS, 48.23-48.51ºN) to refine estimation of geo-ecological risks. Methods.
In article are analyzed use of modern satellite technologies at research of geodynamic processes.The main problems that arise at use of various approaches to interpretation of results of satellite measurements are considered.