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La propagation des ondes acoustiques P et S dans les sédiments argileux est liée à la porosité du milieu et à leur composition minéralogique. La prédiction des vitesses de propagation de ces ondes nécessite donc de connaître ces paramètres et leur impact sur les vitesses. La diminution de la porosité avec l’augmentation de la pression effective, due à l’enfouissement, suit une loi exponentielle. Cette...
Set the date range to filter the displayed results. You can set a starting date, ending date or both. You can enter the dates manually or choose them from the calendar.