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Inga Sigrun Moeck
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The interplay of Malm carbonate permeability, gravity-driven groundwater flow, and paleoclimate – implications for the geothermal field and potential in the Molasse Basin (southern...
by
Tom Vincent Schintgen
,
Inga
Sigrun
Moeck
Published in
Geothermal Energy
(2021)
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Related Subjects
Geology
Malm
Molasse Basin
North Alpine Foreland Basin
Permafrost
QE1-996.5
Renewable energy sources
TJ807-830
Upper Jurassic
Würm Glaciation
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