How do permeable fractures in the Triassic sediments of Northern Alsace characterize the top of hydrothermal convective cells? Evidence from Soultz geothermal boreholes (France)
Crossref DOI link: https://doi.org/10.1186/s40517-015-0026-4
Published Online: 2015-04-18
Published Print: 2015-12
Update policy: https://doi.org/10.1007/springer_crossmark_policy
Vidal, Jeanne
Genter, Albert
Schmittbuhl, Jean
License valid from 2015-04-18
Article History
Received: 12 June 2014
Accepted: 7 January 2015
First Online: 18 April 2015