Geo-pressure and geo-mechanical models for the Late Messinian Abu Madi reservoir in the Nidoco and Baltim gas fields, offshore Nile Delta Basin, Egypt
The young Nile Delta Basin of Egypt (Plio-Pleistocene) exhibits compaction disequilibrium, as the rate of sedimentation exceeds the rate of subsidence. This represents the main cause of the overpressure regime encountered in this basin. This condition presents a very challenging problem when adjusti...
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Veröffentlicht in: | Euro-Mediterranean journal for environmental integration 2024-03, Vol.9 (1), p.183-206 |
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Sprache: | eng |
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