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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...
| Autores principales: | , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2018
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| Materias: | |
| 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 |