date: 2022-05-11T09:59:36Z
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pdf:docinfo:title: Hydrogeologic and Thermal Effects of Glaciations on the Intracontinental Basins in Central and Northern Europe
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dc:description: We use a fully coupled hydro-thermal model (TH) to quantify changes in the pore pressure and temperature distribution following the Last Glacial Maximum (LGM) in the intracontinental basins in Central and Northern Europe.
Keywords: hydrogeologic 3D model, Central European Basin System (CEBS), basin modeling, last glacial maximum (LGM), boundary condition (BC), 3D thermohydraulic numerical model, nuclear waste repository, glacial isostatic adjustment (GIA)
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subject: We use a fully coupled hydro-thermal model (TH) to quantify changes in the pore pressure and temperature distribution following the Last Glacial Maximum (LGM) in the intracontinental basins in Central and Northern Europe.
dc:creator: Maximilian Frick
description: We use a fully coupled hydro-thermal model (TH) to quantify changes in the pore pressure and temperature distribution following the Last Glacial Maximum (LGM) in the intracontinental basins in Central and Northern Europe.
dcterms:created: 2022-05-04T01:45:31Z
Last-Modified: 2022-05-11T09:59:36Z
dcterms:modified: 2022-05-11T09:59:36Z
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title: Hydrogeologic and Thermal Effects of Glaciations on the Intracontinental Basins in Central and Northern Europe
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pdf:docinfo:keywords: hydrogeologic 3D model, Central European Basin System (CEBS), basin modeling, last glacial maximum (LGM), boundary condition (BC), 3D thermohydraulic numerical model, nuclear waste repository, glacial isostatic adjustment (GIA)
pdf:docinfo:modified: 2022-05-11T09:59:36Z
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dc:title: Hydrogeologic and Thermal Effects of Glaciations on the Intracontinental Basins in Central and Northern Europe
modified: 2022-05-11T09:59:36Z
cp:subject: We use a fully coupled hydro-thermal model (TH) to quantify changes in the pore pressure and temperature distribution following the Last Glacial Maximum (LGM) in the intracontinental basins in Central and Northern Europe.
pdf:docinfo:subject: We use a fully coupled hydro-thermal model (TH) to quantify changes in the pore pressure and temperature distribution following the Last Glacial Maximum (LGM) in the intracontinental basins in Central and Northern Europe.
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pdf:docinfo:creator: Maximilian Frick
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creator: Maximilian Frick
meta:author: Maximilian Frick
dc:subject: hydrogeologic 3D model, Central European Basin System (CEBS), basin modeling, last glacial maximum (LGM), boundary condition (BC), 3D thermohydraulic numerical model, nuclear waste repository, glacial isostatic adjustment (GIA)
meta:creation-date: 2022-05-04T01:45:31Z
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meta:keyword: hydrogeologic 3D model, Central European Basin System (CEBS), basin modeling, last glacial maximum (LGM), boundary condition (BC), 3D thermohydraulic numerical model, nuclear waste repository, glacial isostatic adjustment (GIA)
Author: Maximilian Frick
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