Metadata 1577
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".
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.
Europe is largely dependent on raw materials imports and has to supply its needs, especially of critical raw materials, from international sources. Nevertheless, Europe also has a long lasting mining history and some deposits have been mined continuously even for hundreds of years. FRAME WP7 investigates traditional mining sites and their raw material potential. In addition to the main commodities of these historic deposits, the project focuses on strategic raw materials (SRM) such as e.g. high-tech metals...
Iso-content maps of Holmium (Ho), one of the chemical elements.obtained in the Geochemical Atlas of Spain Project, distributed in stream sediments (14,864 samples), superficial soils (0-20 cm.) (13,505 samples) and deeper soils (20-40 cm.) (7,682 samples). The results of the chemical analysis are shown in two types: total dissolution of the sample with 4 acids and partial dissolution with aqua regia. With the analytical results of all the sampled points, an isocontent map is made with adjustment to a squa...
Results of mapping and assessment of the cross-border (DE/AT) hydrothermal play in the Upper Jurassic carbonates beneath the central part of the North Alpine Molasse Basin (HotLime Case Study 1).
Results of mapping and assessment of the cross-border (DE/AT) hydrothermal play in the Upper Jurassic carbonates beneath the central part of the North Alpine Molasse Basin (HotLime Case Study 1).