Metadata 1577
Base of hydrate stability zone for biogenic gas. Geographical site: SW Europe. Reference: Váquez-Izquierdo, A., Gimenez-Moreno, C.-J., León, R., 2018. Knowledge gaps in gas-hydrate assessment: theoretical considerations and practical implications. Geophysical Research Vol. 20, EGU2018-12847, 2018EGU General Assembly 2018 (Vol. 20, EGU2018-12847, 2018EGU General Assembly 2018).
Base of negative bouyancy zone for 100% C02. Geographical site: Celtic Sea & French EEZ. References: Burnol, A. (2018). Roles of Gas Hydrates for CO2 Geological Storage Purposes. Gas Hydrates 2, 267-284. doi:https://doi.org/10.1002/9781119451174.ch13 Burnol, A., Thinon, I., Ruffine, L., & Herri, J. M. (2015). Influence of impurities (nitrogen and methane) on the CO2 storage capacity as sediment-hosted gas hydrates – Application in the area of the Celtic Sea and the Bay of Biscay. International Journal of G...
Base of negative bouyancy zone for 96% C02. Geographical site: Celtic Sea & French EEZ. References: Burnol, A. (2018). Roles of Gas Hydrates for CO2 Geological Storage Purposes. Gas Hydrates 2, 267-284. doi:https://doi.org/10.1002/9781119451174.ch13 Burnol, A., Thinon, I., Ruffine, L., & Herri, J. M. (2015). Influence of impurities (nitrogen and methane) on the CO2 storage capacity as sediment-hosted gas hydrates – Application in the area of the Celtic Sea and the Bay of Biscay. International Journal of Gr...
Base of negative bouyancy zone for 96% C02. Extended 200M in the FISU Area, Celtic Sea. The FISU area is defined by the joint submission made by by Spain, Ireland and the United Kingdom of Great Britain and Northern Ireland (FISU) to the Commission on the Limits of the Continental Shelf (Article 76) References: Burnol, A. (2018). Roles of Gas Hydrates for CO2 Geological Storage Purposes. Gas Hydrates 2, 267-284. doi:https://doi.org/10.1002/9781119451174.ch13 Burnol, A., Thinon, I., Ruffine, L., & Herri, J....
Base of negative bouyancy zone for 96% C02. Geographical site: South of Biscay Bay, Galicia Area. References: Burnol, A. (2018). Roles of Gas Hydrates for CO2 Geological Storage Purposes. Gas Hydrates 2, 267-284. doi:https://doi.org/10.1002/9781119451174.ch13 Burnol, A., Thinon, I., Ruffine, L., & Herri, J. M. (2015). Influence of impurities (nitrogen and methane) on the CO2 storage capacity as sediment-hosted gas hydrates – Application in the area of the Celtic Sea and the Bay of Biscay. International Jou...
Eastern Structural elements from NAG-TEC: Northeast Atlantic Geoscience Tectonostratigraphic Atlas. This dataset contains the basins and highs along the margins and within the Jan Mayen microcontinent and contains information about the ages, the hierarchy between the structural elements and origin of data. For further information see https://data.geus.dk/nagtec/home.
The dataset for the Geological Map of Estonia has been created by vectorizing the paper version of the Bedrock Geological Map of Estonia at a scale of 1:200 000 and has been published in 1997. The map shows areas of bedrock classified into geological units according to the types of rock and their ages. In addition, fault zones in the bedrock are also depicted.
The service presents an overview of Estonian bedrock and fault zones at a scale of 1:400 000.
The dataset for the Bedrock Geology of Ireland at a scale of 1:1M was created by simplifying the published digital Bedrock Geological Map of Ireland at a scale of 1:500 000.
The Geological Map of Finland depicts the main features of bedrock geology in Finland. In this dataset bedrock areas are classified according to rock types and ages. The dataset is an improved version of the Geological map of the Fennoscandian Shield. The legend has been revised in cooperation with the geological surveys of Sweden and Norway.