Paper 115 of 383
Published May 31, 2026
The Levant Basin of the Eastern Mediterranean, adjacent to Israel, Lebanon, Cyprus, and Egypt, and the North Sea Basin between the United Kingdom, Norway, Denmark, and the Netherlands represent two major offshore sedimentary systems with significant petroleum and structural importance.
This paper compares both basins through observable geological constraints including basin-fill thickness, shelf-to-basin transition geometry, margin continuity, subsidence history, structural compartmentalization, and hydrocarbon-system context.
The Levant Basin occupies a deep eastern Mediterranean setting with major gas discoveries and complex regional boundary relationships. The North Sea Basin occupies a mature offshore petroleum province with well-mapped rift architecture, platform systems, and basin segmentation.
The objective is not to treat these offshore basins as equivalent, but to evaluate whether consistent structural descriptors can support cross-basin comparison across different marine geological environments.
For institutional and resource-sector audiences, this comparison is useful because both basins are highly mapped, economically significant, and constrained by extensive seismic, stratigraphic, and geophysical datasets.
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