Paper 87 of 383
Published May 31, 2026
The Aegean Sea region spanning Greece and western Türkiye and the Dead Sea Rift extending through Israel and Jordan represent two distinct geological environments characterized by elongated structural expression and regional-scale organization.
This paper evaluates observable geometric constraints including basin elongation, continuity length, directional persistence, boundary confinement, and regional structural coherence.
Although commonly interpreted through different tectonic frameworks, both systems provide measurable structural relationships that permit direct comparison without requiring identical formation mechanisms.
The objective is to determine whether recurring geometric characteristics emerge when basin systems are evaluated using consistent observational criteria.
The resulting comparison establishes a testable framework for future structural classification and comparative geological analysis.
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