Thermal and seismic hints for chimney type cross-stratal fluid flow in onshore basins

When modelling onshore sedimentary basins, modellers generally assume that semi-permeable layers (aquitards) greatly restrict vertical flow between aquifers. Aquitards are therefore considered as confining media and vertical flow is assumed to take place mainly within localised permeable faults, if...

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Detalles Bibliográficos
Autores principales: Dentzer, Jacques, Bruel, Dominique, Delescluse, Matthias, Chamot-Rooke, Nicolas, Beccaletto, Laurent, Lopez, Simon, Courrioux, Gabriel, Violette, Sophie
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6192993/
https://www.ncbi.nlm.nih.gov/pubmed/30333508
http://dx.doi.org/10.1038/s41598-018-33581-x

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6192993/
https://www.ncbi.nlm.nih.gov/pubmed/30333508
http://dx.doi.org/10.1038/s41598-018-33581-x

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