Deep-Time Information Retention Systems
Paper 410 of 511
Published June 1, 2026
Abstract
Earth's history is incomplete.
Most geological information has been modified, recycled, metamorphosed, eroded, or destroyed.
Yet certain signals remain detectable across billions of years.
This paper examines geological information retention as a measurable Earth-system phenomenon.
Retention Classes
- Cratonic preservation
- Mineral-system preservation
- Structural inheritance
- Geochemical signatures
- Stratigraphic preservation
- Magnetic records
- Isotopic systems
- Deep crustal continuity
Information Principle
The geological record is not simply a history of formation.
It is also a history of successful preservation.