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Geofluid Dynamics of the Cenozoic Sedimentary Basins of the Caspian-black Sea RegionNormal access

Authors: R.N. Mustaev, V.Yu. Kerimov, K.I. Dantsova and L.I. Kerimova
Event name: Geomodel 2018
Session: Моделирование формирования углеводородных систем, бассейновый анализ, геохимия нефти и газа
Publication date: 10 September 2018
DOI: 10.3997/2214-4609.201802324
Organisations: EAGE
Language: Russian
Info: Extended abstract, PDF ( 464.05Kb )
Price: € 20

The most important feature of the structure of the Caspian-Black Sea region is the intense state of its subsoil, high and diverse geodynamic, volcanic, seismic, geofluidodynamic activity, etc. Geodynamic activity is associated with various kinds of discharge of fluid dynamic stresses, primarily intensive ascending discharges of various mobile fluids and their components - oils and gases, clay flows and the manifestation of thermobaric anomalies. A vivid manifestation of geodynamic activity is its explosive variety - "sedimentary" volcanism: mud, gas and oil, mixed, etc., which in turn determine the intensity of geofluidodynamic processes.

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