Energy resources

Exploration and sustainable exploitation of Danish and Greenlandic energy. Programme areas include deep and shallow geothermal energy, hydropower, marine-physical planning and oil and gas.

The Energy resources programme includes contributions from the following departments at GEUS:

Geophysics
Groundwater and Quaternary Geology Mapping
Glaciology and Climate
Marine Geology
Reservoir Geology
Stratigraphy

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151 to 160 of 184 Results

Gravity Inversion Jun 15, 2022 - NAG-TEC Atlas Haase, C.; Ebbing, J.; Funck, T., 2014, "Gravity Inversion", https://doi.org/10.22008/FK2/NWYZGL, GEUS Dataverse, V1 Gridded files of depth to Moho and crustal thickness based on gravity inversion. The inversion uses the total sediment thickess grid for depth to basement.
crustal_thickness_geo.nc Jun 15, 2022 - Gravity Inversion Network Common Data Form - 53.0 MB - MD5: 29494a63a018b3e35295196840a57f4f Data netcdf gridded file of crystalline crustal thickness in geographic coordinates. Datum: WGS84
crustal_thickness_geo.xyz Jun 15, 2022 - Gravity Inversion Co-Ordinate Animation - 2.2 MB - MD5: 9ca7f2726d4a81d4df8615bcb102a7c7 Data XYZ ascii grid of crystalline crustal thickness in geographic coordinates. Datum: WGS84
crustal_thickness_lam.nc Jun 15, 2022 - Gravity Inversion Network Common Data Form - 373.6 KB - MD5: ec15a816a8bc1167b5caa6ddb333eacf Data netcdf gridded file of crystalline crustal thickness in the original projection coordinates used by the project. Lambert Conic Conformal: central meridian - 40°W, standard parallels - 55°N, 75°N. Datum: WGS84
crustal_thickness_lam.xyz Jun 15, 2022 - Gravity Inversion Co-Ordinate Animation - 2.2 MB - MD5: a16308bca193087809712f76ef8d37f7 Data XYZ ascii grid of crystalline crustal thickness in the original projection coordinates used by the project. Lambert Conic Conformal: central meridian - 40°W, standard parallels - 55°N, 75°N. Datum: WGS84
depth_to_moho_geo.nc Jun 15, 2022 - Gravity Inversion Network Common Data Form - 53.0 MB - MD5: 41eb4032502161c5bfdcf3b4764b65ad Data netcdf gridded file of crystalline depth to Moho in geographic coordinates. Datum: WGS84
depth_to_moho_geo.xyz Jun 15, 2022 - Gravity Inversion Co-Ordinate Animation - 2.3 MB - MD5: 7d4c6f40f64e79080b01e07f9bf8eaec Data XYZ ascii grid of crystalline depth to Moho in geographic coordinates. Datum: WGS84
depth_to_moho_lam.nc Jun 15, 2022 - Gravity Inversion Network Common Data Form - 373.6 KB - MD5: 6a92eb8d9fe1bdcf2132a3094b84b89a Data netcdf gridded file of crystalline depth to Moho in the original projection coordinates used by the project. Lambert Conic Conformal: central meridian - 40°W, standard parallels - 55°N, 75°N. Datum: WGS84
depth_to_moho_lam.xyz Jun 15, 2022 - Gravity Inversion Co-Ordinate Animation - 2.2 MB - MD5: b14f6715d776a474249aee89ce2d81d7 Data XYZ ascii grid of crystalline depth to Moho in the original projection coordinates used by the project. Lambert Conic Conformal: central meridian - 40°W, standard parallels - 55°N, 75°N. Datum: WGS84
Gravity Anomaly Grids Jun 15, 2022 - NAG-TEC Atlas Haase, C.; Ebbing, J.; Funck, T., 2014, "Gravity Anomaly Grids", https://doi.org/10.22008/FK2/AQ38FS, GEUS Dataverse, V1 Bouguer anomaly, isostatic anomaly, and tilt derivative of the isostatic anomaly derived from the free-air gravity anomaly. The free-air anomaly is based on the DTU Space 2010 global compilation.

Gravity Inversion

Jun 15, 2022 - NAG-TEC Atlas

Haase, C.; Ebbing, J.; Funck, T., 2014, "Gravity Inversion", https://doi.org/10.22008/FK2/NWYZGL, GEUS Dataverse, V1

Gridded files of depth to Moho and crustal thickness based on gravity inversion. The inversion uses the total sediment thickess grid for depth to basement.

crustal_thickness_geo.nc