GlaciStore: understanding Late Cenozoic glaciation and basin processes for the development of secure large scale offshore CO2 storage (North Sea).

• Main Authors: Barrio, M., Stewart, Heather A., Akhurst, M., Aagaard, P., Alcalde, J., Bauer, A., Bradwell, T., Cavanagh, A., Evans, D., Faleide, J., Gent, C., Haflidason, H., Haszeldine, S., Hjelstuen, B., Johnson, G., Mondol, N., Mørk, A., Mørkved, P., di Primio, R., Querendez, E., Ringrose, P., Sejrup, H., Stewart, M., Uriansrud, F., Wilkinson, M.
• Format: Text
• Language: English
• Published: 2015
• Subjects: Earth Sciences; Marine Sciences; Ice Sheet
• Online Access: http://nora.nerc.ac.uk/id/eprint/509989/; https://nora.nerc.ac.uk/id/eprint/509989/1/8th_TrondheimCCS_Conference2015-Barrio_and_all.pdf; http://tccs-8.exordo.com/data/paper_attachments/291/initial_draft/TCCS8-Barrio_and_all.pdf

The sedimentary strata of the North Sea Basin (NSB) record the glacial and interglacial history of environmental change in the Northern Hemisphere, and are a proposed location for the engineered storage of carbon dioxide (CO2) captured from power plant and industrial sources to reduce greenhouse gas emissions. These aspects interact in the geomechanical and fluid flow domain, as ice sheet dynamics change the properties of potential seal and reservoir rocks that are the prospective geological storage strata for much of Europe’s captured CO2. The central part of the NSB preserves a unique history of the depositional record spanning at least the last 3 Ma, which also forms the overburden and uppermost seal to the underlying CO2 reservoirs. There is good evidence that these ice sheets created strong feedback loops that subsequently affected the evolution of the Quaternary climate system through complex ocean-atmosphere-cryosphere linkages.