Thermal structure of the deep Lopra-1/1A borehole in the Faroe Islands

Earth and Planetary Sciences

• Borehole 100%
• Thermal Structure 100%
• Basalt 66%
• Thermal Conductivity 50%
• Heat Transfer 50%
• Depth Interval 33%
• Continental Crust 16%
• Last Glacial 16%
• Groundwater Flow 16%
• Last Glaciation 16%
• Tholeiitic Basalt 16%
• Hyaloclastite 16%
• Thermal Regime 16%
• Temperature Variation 16%
• Mineral Alteration 16%
• Porosity 16%