Paper 231 of 383
Published June 1, 2026
The transition from Arabian structural provinces into the Zagros Fold Belt represents one of the most significant deformation gradients within the Middle East.
This paper evaluates continuity across the Arabian-Zagros transition through structural persistence, fold development, fault-system organization, basin architecture, topographic gradients, and regional geological coherence.
Reference systems include the Arabian Platform, Mesopotamian Basin, Zagros Fold Belt, Persian Gulf Basin, and adjacent structural provinces.
The objective is to determine whether measurable continuity remains visible as relatively stable Arabian domains transition into one of Earth's major compressional systems.
Within ABC Sequencing, the Arabian-Zagros transition provides a useful test of whether continuity survives increasing structural complexity.
The framework emphasizes measurable geological relationships rather than assumptions regarding regional origin or mechanism.
This paper evaluates continuity between Arabian geological provinces and the Zagros Fold Belt through measurable deformation and structural persistence.