Paper 218 of 383
Published June 1, 2026
Many geological systems contain long-lived deformation boundaries that remain identifiable across large spatial scales and extended geological time periods.
This framework evaluates deformation boundary persistence through fault continuity, structural organization, regional deformation gradients, tectonic interaction, and geological recurrence.
Reference systems include the Himalayan deformation front, Zagros Fold Belt, Dead Sea Transform, San Andreas system, East African Rift, and selected convergent and transform margins.
The objective is to establish whether certain deformation boundaries exhibit measurable persistence beyond local geological conditions.
Within ABC Sequencing, persistent boundaries provide useful observational markers for evaluating continuity across larger geological systems.
The framework focuses on measurable structural relationships and comparative geological behavior across diverse tectonic environments.
This paper formalizes deformation-boundary persistence as a comparative framework for evaluating long-lived structural systems across multiple tectonic settings.