Paper 143 of 383
Published May 31, 2026
The Arabian Plate occupies a key structural position between the Eastern Mediterranean, Red Sea, Persian Gulf, Mesopotamian Basin, and Zagros Fold Belt. This makes it an important transition region for evaluating whether regional geological systems preserve measurable continuity across multiple structural domains.
This paper evaluates Arabian Plate transition geometry through observable constraints including plate-margin orientation, basin distribution, fault-system continuity, uplift gradients, sedimentary architecture, and deformation relationships extending from Israel and Jordan toward Iraq, Iran, Saudi Arabia, and the Persian Gulf.
The analysis builds on prior Aegean, Levant, and Dead Sea corridor papers by extending the structural comparison eastward into the Arabian domain.
Within ABC Sequencing, the Arabian Plate is treated as a constraint-bearing region along the proposed Aegean-to-Himalayan path. This paper does not assume that interpretation; it tests whether the plate preserves geometry, deformation, and basin relationships that justify further comparison.
For resource exploration, geosteering, and basin analysis, Arabian Plate transition systems are commercially important because they influence hydrocarbon basin geometry, structural compartmentalization, stress orientation, and subsurface prediction.
This paper moves the sequence from the Levant and Dead Sea corridor into the Arabian Plate, tightening the proposed entrance-to-path geometry using measurable basin, margin, and deformation constraints.
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