Paper 142 of 383
Published May 31, 2026
The Dead Sea Transform extends through a highly constrained geological corridor between Israel, Jordan, Lebanon, Syria, and the Red Sea region. It includes one of the most recognizable continental structural systems in the Eastern Mediterranean–Arabian transition zone.
This framework evaluates the Dead Sea Transform through measurable constraints including fault continuity, basin confinement, vertical relief, pull-apart basin geometry, fracture orientation, and regional deformation persistence.
Reference areas include the Dead Sea Basin, Jordan Valley, Gulf of Aqaba, Levant margin, and surrounding structures of Israel, Jordan, Lebanon, and western Arabia.
The objective is to test whether the Dead Sea Transform functions as a measurable structural corridor between Eastern Mediterranean basin systems and Arabian Plate deformation systems.
Within ABC Sequencing, the Dead Sea region is relevant because it appears in the older Affinity Theory geometry as one of the extreme low-elevation constraint points. This paper keeps the interpretation bounded: the Dead Sea Transform is evaluated first as geometry, structure, and measurable relief.
For geosteering, basin analysis, and resource exploration, corridor-style structural systems are important because they influence fluid pathways, basin compartmentalization, stress orientation, and subsurface prediction.
This paper tightens the Aegean-to-Levant transition by treating the Dead Sea Transform as a structural corridor with measurable basin, fault, and relief constraints.
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