Metadata 1743
Vulnerability assessment output map using DRASTIC method (Aller et al., 1987)
Vulnerability assessment output map using DRASTIC method (Aller et al., 1987)
Vulnerability assessment output map using DRASTIC method (Aller et al., 1987)
Vulnerability assessment output map using DRASTIC method (Aller et al., 1987)
Information about the heat flow and geothermal gradient represented as points. The data originally come from the global heat flow database of the International Heat Flow Commission in 2010. A description of the data and a literature list can be found on the website of the International Heat Flow Commission (https://ihfc-iugg.org/products/global-heat-flow-database)
The heat in place is the maximum theoretically extractible heat energy (in GJ.m² at 50 grC) for Niederroedern, Froidefontaine, Pechelbronn, Base Tertiary, Rotliegend reservoirs. The static and volumetric evaluation method used to calculate the map derived from "Muffler & Cataldi 1978".
The heat in place is the maximum theoretically extractible heat energy of the Dinantian reservoir (in GJ.m² at 50 grC). The static and volumetric evaluation method used to calculate the map derived from "Muffler & Cataldi 1978".
Zoltán Püspöki, Gábor Markos 2019: In order to establish hydrodynamic and transport modelling of the drinking and irrigation aquifers, we aimed at a high-resolution stratigraphic delineation of the Quaternary river water aquifer series, which is difficult to separate from the bedrock. The sample area is the catchment area of the Dong River (Danube-Tisza Area - Makó Graben). This time, the stratigraphic resolution was based on climatostratigraphic observations, i.e. the "early postglacial magnetic susceptib...
Zoltán Püspöki, Gábor Markos 2019: High resolution geological modelling is based on reliable and sufficiently high resolution stratigraphy. In high-resolution stratigraphic studies, the sedimentary sequence is subdivided by isochronous (=contemporaneous) surfaces ("time horizons") interpreted in terms of facies. The aim of the 3D geological modelling of the Debrecen-South (Nyírség) area was to support hydrogeological modelling. The sedimentological/faciesistological characteristics of the sedimentary syste...
Tectonic lines in Europe, as they appear in the GeoERA HIKE fault data base. Fault geometry is based on national and regional information provided by the respective geological survey organisation.
