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- W1485464578 abstract "Sedimentary basins located in regions exhibiting geothermal anomalies are very promising for hydrothermalexploration. Facies model integration into seismic 3D interpretation allow description of reservoir parameters suchas permeability, thermal conductivity and reservoir heat flow, as these properties are directly correlative to faciesheterogeneity integrated from outcrop studies.Outcrop analogue studies support the characterization of deep geothermal reservoirs and their geothermaloperations. Our data from the Meso- and Cenozoic sedimentary series of Budapest include carbonates and clasticsediments of Triassic, Eocene, and Oligo-Miocene age as well as Pleistocene travertine, exposed on the westernside of the river Danube. Field and laboratory analyses reveal distinct horizons of different geothermal potentialand thus, enable us to identify and interpret corresponding exploration target horizons in geothermal prone depthsof the Pannonian Basin." @default.
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- W1485464578 date "2010-05-01" @default.
- W1485464578 modified "2023-09-23" @default.
- W1485464578 title "Facies and geothermal reservoir characteristics of sedimentary rocks: an outcrop analogue study of the Meso- and Cenozoic series of Budapest (Hungary)" @default.
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