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Lisa Maria Ringel, Márk Somogyvári, Mohammadreza Jalali and Peter Bayer    
Fractures serve as highly conductive preferential flow paths for fluids in rocks, which are difficult to exactly reconstruct in numerical models. Especially, in low-conductive rocks, fractures are often the only pathways for advection of solutes and heat... ver más
Revista: Geosciences    Formato: Electrónico

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