Metadata 1576
Calculated average transformation ratio (TR all) for the Lower Jurassic interval.
Calculated average transformation ratio (TR all) for the Upper Jurassic interval.
Calculated average vitrinite reflectance (EASY%Ro) for the Lower Jurassic interval.
Calculated average vitrinite reflectance (EASY%Ro) for the Upper Jurassic interval
Iso-content maps of Barium (Ba), one of the chemical elements.obtained in the Geochemical Atlas of Spain Project, distributed in stream sediments (14,864 samples), superficial soils (0-20 cm.) (13,505 samples) and deeper soils (20-40 cm.) (7,682 samples). The results of the chemical analysis are shown in two types: total dissolution of the sample with 4 acids and partial dissolution with aqua regia. With the analytical results of all the sampled points, an isocontent map is made with adjustment to a square...
Base of hydrate stability zone for 100% CO2. 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 hydrate stability zone for 96% CO2. 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 hydrate stability zone for 96% CO2. 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...
Base of hydrate stability zone for biogenic gas. Geographical site: world. Reference: Piñero, E., Marquardt, M., Hensen, C., Haeckel, M., & Wallmann, K. (2013). Estimation of the global inventory of methane hydrates in marine sediments using transfer functions. Biogeosciences (BG), 10(2), 959-975.
Base of hydrate stability zone for biogenic gas. Geographical site: NW 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).