Paper 147 of 383
Published May 31, 2026
The Himalayan Orogen represents one of the most prominent deformation systems on Earth. Extending across Nepal, India, Bhutan, Pakistan, and the Tibetan Plateau of China, the region preserves large-scale evidence of uplift, crustal shortening, structural inheritance, and persistent deformation.
This paper evaluates Himalayan structural continuity through observable constraints including fold geometry, thrust systems, uplift gradients, crustal architecture, fault persistence, and regional deformation corridors.
Particular attention is given to identifying structural relationships that remain coherent across large geographic distances despite significant geological complexity.
The analysis builds directly upon prior investigations of the Zagros Fold Belt and Arabian structural corridor systems, extending the comparison into the Himalayan domain.
For geological mapping, mineral exploration, and structural interpretation, the Himalayas provide an important reference system for evaluating how large-scale deformation geometry is preserved through time.
The ABC Sequencing corridor now extends from the Aegean region through the Levant, Arabian Plate, Zagros Fold Belt, and into the Himalayan deformation system. The emphasis remains on measurable geometry, continuity, and preserved geological structure.
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