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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21 to 30 of 34 Results
Jul 13, 2022
Schovsbo, Niels Hemmingsen; Doornenbal, Hand; Nelskamp; Pedersen, C.B.; Anthonsen, K.L.; Tougaard, L.; Zijp, M.; Anthonsen, K.L., 2022, "Review of results, knowledge gaps and recommendations for future work", https://doi.org/10.22008/FK2/4JS6NW, GEUS Dataverse, V1
This report is prepared by Niels H. Schovsbo, Karen L. Anthonsen, Christian B. Pedersen, and Lisbeth Tougaard, from GEUS, and Susanne Nelskamp, Mart Zijp and Hans Doornenbal, from TNO, as part of the EUOGA study (EU Unconventional Oil and Gas Assessment) commissioned by JRC-IET.
Jun 17, 2022 - NAG-TEC Atlas
Spakman, W., 2014, "Mantle Tomography Model UU-P07", https://doi.org/10.22008/FK2/UVZJDQ, GEUS Dataverse, V1
Tomographic model of Earth's mantle developed for the project.
Jun 15, 2022 - NAG-TEC Atlas
Hopper, J.R.; Funck, T.; Stoker, M.S.; Árting, U.; Peron-Pinvidic, G.; Doornenbal, H.; Gaina, C.; NAG-TEC Contributors, 2014, "Tectonostratigraphic Atlas of the North-East Atlantic Region", https://doi.org/10.22008/FK2/ZZQRQ1, GEUS Dataverse, V1
The complete printed volume.
Jun 15, 2022 - NAG-TEC Atlas
Hopper, J.R.; Funck, T.; Stoker, M.S.; Árting, U.; Peron-Pinvidic, G.; Doornenbal, H.; Gaina, C.; NAG-TEC Contributors, 2014, "NAG-TEC ArcGIS Project", https://doi.org/10.22008/FK2/KHHMQE, GEUS Dataverse, V1
ArcGIS database of comprehensive background material upon which the NAG-TEC Atlas is based. The project includes links to seismic refraction profiles, geoseismic sections, stratigraphic charts, etc. A separate geodatabase and mxd file is included with the reconstructions based on...
Jun 15, 2022 - NAG-TEC Atlas
Funck, T.; Erlendsson, Ö.; Geissler, W. H.; Gradmann, S.; Kimbell, G.S.; McDermott, K.G.; Petersen, U., 2014, "Seismic Refraction Database", https://doi.org/10.22008/FK2/R1K0YE, GEUS Dataverse, V1
The seismic refraction database contains 207 published velocity model profiles from seismic refraction experiments. Included with each profile are references to all publications, depth to basement and Moho, navigation information, and interpretations of the crustal type.
Jun 15, 2022 - NAG-TEC Atlas
Funck, T.; Erlendsson, Ö.; Geissler, W. H.; Gradmann, S.; Kimbell, G.S.; McDermott, K.G.; Petersen, U., 2014, "Depth to Moho, Basement, and Crustal Thickness from Seismic Refraction Data", https://doi.org/10.22008/FK2/TG7OQU, GEUS Dataverse, V1
Gridded crustal thickness and depth to Moho and basement based on seismic refraction data.
Jun 15, 2022 - NAG-TEC Atlas
Fatah, R. A.; Geissler, W. H.; Funck, T.; Hopper, J.R.; Kimbell, G. S.; Gaina, C.; Blischke, A.; Erlendsson, Ö.; Doornenbal, H., 2014, "Total Sediment Thickness", https://doi.org/10.22008/FK2/P9XHV9, GEUS Dataverse, V1
Total sediment thickness of the North-East Atlantic based on interpretation of seismic reflection and constrained where possible by wells that reach basement. In some areas, seismic refraction data was also used.
Jun 15, 2022 - NAG-TEC Atlas
Gaina, C., 2014, "Age of Ocean Crust", https://doi.org/10.22008/FK2/KK5RQN, GEUS Dataverse, V1
Age of oceanic crust based on the kinematic model for opening of the North Atlantic. The continent-ocean boundary was interpreted from the seismic refraction database.
Jun 15, 2022 - NAG-TEC Atlas
Nasuti, A.; Olesen, O., 2014, "Magnetic Anomaly Grids", https://doi.org/10.22008/FK2/CPODOR, GEUS Dataverse, V1
Magnetic anomaly and tilt derivative of the North-East Atlantic region.
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.
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