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geothermal exploration
Open–closed–open palaeofluid system conditions recorded in the tectonic vein networks of the Parmelan anticline (Bornes Massif, France)
A sensitivity analysis of a single extraction well from deep geothermal aquifers in the Cheshire Basin, UK
A Seismic Network to Monitor the 2020 EGS Stimulation in the Espoo/Helsinki Area, Southern Finland
Characterisation of fluid flow conditions and paths in the Buntsandstein Gp. sandstones reservoirs, Upper Rhine Graben
Drilling into mines for heat: geological synthesis of the UK Geoenergy Observatory in Glasgow and implications for mine water heat resources
Optimal Transceiver Distance of Controlled-source Audio-frequency Magnetotelluric Sounding Method
Bayesian magnetotelluric inversion using methylene blue structural priors for imaging shallow conductors in geothermal fields
Introduction to this special section: Geothermal energy
The value of geophysical data for geothermal exploration: Examples from empirical, field, and synthetic data
Fracture attribute and topology characteristics of a geothermal reservoir: Southern Negros, Philippines
Using highly accurate land gravity and 3D geologic modeling to discriminate potential geothermal areas: Application to the Upper Rhine Graben, France
The complete lithostratigraphic section of the geothermal wells in Rittershoffen (Upper Rhine Graben, eastern France): a key for future geothermal wells
Digging deeper: The influence of historical mining on Glasgow's subsurface thermal state to inform geothermal research
Exploration of the Aquifer of San Felipe Geothermal Area (mexico) By Spatially Constrained Inversion of Transient Electromagnetic Data
Particle swarm optimization for simultaneous analysis of magnetotelluric and time-domain electromagnetic data
Understanding fluid behavior through ion and isotope data from the Yitong Basin, Northeast China
Geoelectric structure of the Great Slave Lake shear zone in northwest Alberta: implications for structure and tectonic history
Abstract The North German Basin yields enormous geothermal resources of more than 13 000 EJ (exajoule: 1 EJ = 1 × 10 18 J) heat in place bound to Paleozoic petrothermal and Mesozoic hydrothermal reservoirs. So far, these resources are only exploited at a few localities. Thus, geothermal energy is considered an underutilized energy resource. Despite long-term experience in exploiting Rhaetian hydrothermal reservoirs, the exploration risk remains high, which is mainly related to high expectations on reservoir thickness and quality. Previous exploration campaigns have identified potential hydrothermal reservoirs in six Mesozoic reservoir complexes. But, as high-resolution subsurface maps are not available, the reliable prediction and targeting of reservoirs remains an unsolved problem. As such, an exploration strategy integrating methods of sedimentology, palaeontology, petrography and reservoir characterization was applied to a large database of cores and wireline logs. This contribution details the key results of the exploration of Upper Keuper and Middle Jurassic reservoir complexes, including high-resolution subsurface facies, sandstone thickness and reservoir quality maps. Sets of these maps enable the reliable prediction and targeting of individual hydrothermal reservoirs, and, thus, make a significant contribution to a lowered exploration risk.