Metadata 1533
This area was chosen for the assessment of unconventional hydrocarbon resources using 3D basin and petroleum system modeling. Further information is found in the report,GARAH WP2: 3D Pilot Study – Unconventionals, https://repository.europe-geology.eu/egdidocs/garah/garah_deliverable_report_d24_3d_petroleum_model_un.pdf
The map of “Switzerland during the Last Glacial Maximum (LGM), at a scale of 1:500,000” shows the maximum extent of glaciation in Switzerland at the height of the last Ice Age about 24,000 years BP. It incorporates the latest results of research on the Ice Age in Switzerland in a clearly legible format.
Map showing the geographical distribution of ground movements classified into four main groups: horizontal component in continental areas, vertical component in continental areas, unstable areas linked to coastal areas and movements related to mining operations. Also included are continental areas with important erosive processes.
Thermal conductivity of a geological unit relevant for shallow geothermal energy use (e.g. bedrock).
The intrinsic ability of hard rock samples to conduct heat.
The maximum temperature shift between the production and the injection well that is possible with regards to legal or ecological limitations.
Thermal response test (TRT) is the customary method to determine ground thermal conductivity in situ.
Numerous thermal, mineral and thermomineral waters and the variety of their hydrochemical types represent the most interesting geological issue and signifcant economic potential of the territory of the Republic of Srpska. The proper interpretation of the genesis, hydrogeologic mechanism, chemical content and the regime of some occurrences of these waters provide the consideration of their economic importance and possibilities of utilization.
This is PSI data for Thessaly, Greece. It has been provided by GAMMA Remote Sensing as part of the ESA funded Terrafirma project.
Thickness of the Last Glacial Maximum (LGM) deposit. Contours are presented as depth (metres) below present seafloor or the base of the post LGM sedimentary cover. LGM is defined on average at 18,000 years BP. In glaciated regions the thickness of the Holocene is used. Confidence is defined as follows: 1. High: Sampled feature with good age and palaeoenvironmental control. 2. Sampled feature with poor or none age and palaeoenvironmental control. 3. Constructed by remote sensing data only, 4. Low: Reasonabl...