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SPP 1135:  Dynamics of Sedimentary Systems under Varying Stress Regimes: The Example of the Central European Basin System

Subject Area Geosciences
Term from 2002 to 2008
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 5471600
 
Sedimentary basins are compartments of the upper crust in which mineral and organic material has accumulated over millions of years. This material undergoes partial transformation at temperatures ranging from 0° to 300°C and pressures up to approximately 100 MPa. Due to their longevity and high contents of chemically metastable components, sedimentary basins can be regarded as long-term reactors. The substance turnover and product composition of such a geo-reactor depends essentially on both externally and internally operating processes which affect the sedimentary basin fill over long geological periods. The main objective of this programme is to quantify the major processes that control or affect the formation and evolution of sedimentary basins, including the fluid inventory, using modern geoscientific methods. The focus is on the complex Central European basin system for which a wealth of seismic and borehole data was made available for this programme by the German petroleum industry. Processes of major interest are a) strain and stress in the upper crust leading to crustal extension and compression, evolution of fault zones, their influence on the crustal rheology and their effects on large scale and regional subsidence as well as on the geothermal field, b) inherent processes of a sedimentary system such as compaction, salt movement and fluid generation under the control of the external factors mentioned above, c) transport processes involving the migration of gas and fluids through the pore space either by pressure-driven single-phase or multi-phase flow or by diffusion, their dependence on compaction, fault zones and the geothermal field as well as associated fluid-rock interactions, and d) the supply and redistribution of sedimentary matter acting as a mirror of tectonic activities and climate changes. Finally, important results of the priority programme will be applied to other, less explored basins. This application of concepts relies on the fact that the essential solid and fluid phases as well as the prevailing processes are similar or identical in different sedimentary basins.
DFG Programme Priority Programmes
International Connection Hungary, Italy, Netherlands, Poland

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