Paper 177 of 383
Published May 31, 2026
The Zagros Fold Belt represents one of Earth's most extensive fold-and-thrust systems and occupies a critical position between the Arabian Platform and the Himalayan deformation domain.
This paper evaluates whether geological constraints accumulate within the Zagros system through measurable observations including fold density, thrust architecture, structural persistence, basin overlap, relief gradients, and regional continuity.
Reference regions include western Iran, northeastern Iraq, the Mesopotamian Basin margin, and adjacent Arabian structural provinces.
Particular attention is given to whether multiple independent geological observations become increasingly concentrated within the Zagros domain relative to surrounding regions.
Within ABC Sequencing, the Zagros system serves as an important checkpoint for evaluating whether constraint concentration remains stable, increases, or decreases along the broader corridor.
This paper evaluates whether geological constraints accumulate within the Zagros Fold Belt as the corridor transitions from Arabian structural systems toward the Himalayan domain.
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