Paper 230 of 383
Published June 1, 2026
The transition from the Levant corridor into the Arabian structural domain represents one of the most significant regional changes within the broader Eastern Mediterranean and Middle Eastern geological framework.
This paper evaluates the transition through basin architecture, deformation gradients, fault-system persistence, lithologic variation, topographic organization, and structural continuity.
Reference systems include the Dead Sea Transform, Jordan Rift Valley, Arabian Platform, northern Arabian structural provinces, and associated transition zones.
The objective is to establish whether measurable continuity remains visible across the Levant-Arabian transition despite substantial geological variation.
Within ABC Sequencing, transition analysis provides a means of testing continuity without requiring identical geological expression across neighboring domains.
The framework focuses on recurring relationships, persistence, and measurable geological organization.
This paper evaluates the Levant-to-Arabian transition as a measurable geological boundary where continuity, variation, and structural persistence can be compared directly.