Paper 211 of 383
Published June 1, 2026
Geological observations often organize along corridors rather than appearing randomly across a region. Structural trends, basin margins, fault systems, fracture networks, and deformation belts may create pathways where geological processes become concentrated.
This paper evaluates geological corridors through recurrence frequency, structural continuity, anomaly clustering, constraint density, regional persistence, and comparative geological support.
Reference systems include the Dead Sea Transform, Arabian-Zagros corridor, Himalayan structural systems, East African Rift, Andean margin, and selected sedimentary basin trends.
The objective is to establish whether recurring geological constraints preferentially organize along identifiable corridor systems.
Within ABC Sequencing, corridors function as organizing structures that help connect isolated observations into larger geological networks.
The framework emphasizes measurable continuity rather than inferred relationships.
This paper introduces geological corridors as recurring pathways where constraints, anomalies, and structural observations become concentrated.
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