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How do the geological and geophysical signatures of permeable fractures in granitic basement evolve after long periods of natural circulation? Insights from the Rittershoffen geothermal wells (France)

Crossref DOI link: https://doi.org/10.1186/s40517-018-0100-9

Published Online: 2018-07-23

Published Print: 2018-12

Update policy: https://doi.org/10.1007/springer_crossmark_policy

Authors

Glaas, C. http://orcid.org/0000-0003-3651-7573
Genter, A.

Girard, J. F.

Patrier, P.

Vidal, J.
Funding

Funding for this research was provided by:

EGS Alsace
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Text and Data Mining valid from 2018-07-23
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Article History

Received: 20 March 2018

Accepted: 10 July 2018

First Online: 23 July 2018

Change Date: 17 November 2018

Change Type: Correction

Change Details: After publication of the article (Glaas et al. 2018), it has been brought to our attention that there are some errors. The authors have listed them below.

Updates are available Correction dated 2018-11-17

Click to view Correction: https://doi.org/10.1186/s40517-018-0112-5