How do permeable fractures in the Triassic sediments of Northern Alsace characterize the top of hydrothermal convective cells? Evidence from Soultz geothermal boreholes (France)
- DOI
- 10.1186/s40517-015-0026-4
- Published
- 2015-04-18
- Container
- Geothermal Energy
- Publisher
- Springer Science and Business Media LLC
- Open access
- unknown
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Cite this work
BibTeX
@article{allodium:10.1186/s40517-015-0026-4,
title = {How do permeable fractures in the Triassic sediments of Northern Alsace characterize the top of hydrothermal convective cells? Evidence from Soultz geothermal boreholes (France)},
author = {Jeanne Vidal and Albert Genter and Jean Schmittbuhl},
year = {2015},
journal = {Geothermal Energy},
doi = {10.1186/s40517-015-0026-4},
url = {https://doi.org/10.1186/s40517-015-0026-4}
}RIS
TY - JOUR TI - How do permeable fractures in the Triassic sediments of Northern Alsace characterize the top of hydrothermal convective cells? Evidence from Soultz geothermal boreholes (France) AU - Jeanne Vidal AU - Albert Genter AU - Jean Schmittbuhl PY - 2015 JO - Geothermal Energy DO - 10.1186/s40517-015-0026-4 UR - https://doi.org/10.1186/s40517-015-0026-4 ER -
APA
Vidal, J., Genter, A., & Schmittbuhl, J. (2015). How do permeable fractures in the Triassic sediments of Northern Alsace characterize the top of hydrothermal convective cells? Evidence from Soultz geothermal boreholes (France). Geothermal Energy. https://doi.org/10.1186/s40517-015-0026-4
Source records
- crossref · retrieved 2026-11-10T13:56:06.525Z