Characterisation of the fracture- and karst-controlled geothermal reservoir below Munich from geophysical wireline and well information

Characterisation of the fracture- and karst-controlled geothermal reservoir below Munich from geophysical wireline and well information

Abstract The Upper Jurassic carbonate aquifer in the German Molasse Basin (S Germany) below Munich is the focus of exploitation of geothermal energy. To implement geothermal wells, meaningful prediction of reservoir quality (e.g., volume, temperature, location of aquifers, porosity, permeability) is...

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Bibliographic Details
Main Authors: J. F. Krumbholz, M. Krumbholz, S. H. Wadas, D. C. Tanner
Format: Article
Language:English
Published: SpringerOpen 2024-03-01
Series:Geothermal Energy
Subjects:
Fracture system
Karst
Geothermal exploration
Molasse Basin
Hydraulic active zones
Renewable energy
Online Access:https://doi.org/10.1186/s40517-024-00286-6

Internet

https://doi.org/10.1186/s40517-024-00286-6

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