Seismicity induced during the development of the Rittershoffen geothermal field, France
Abstract The development of the Rittershoffen deep geothermal field (Alsace, Upper Rhine Graben) between 2012 and 2014 induced unfelt seismicity with a local magnitude of less than 1.6. This seismicity occurred during two types of operations: (1) mud losses in the Muschelkalk formation during the dr...
Main Authors: | , , , , , |
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Format: | Article |
Language: | English |
Published: |
SpringerOpen
2020-02-01
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Series: | Geothermal Energy |
Subjects: | |
Online Access: | https://doi.org/10.1186/s40517-020-0155-2 |