Category | Plate Tectonics (Mainstream) | Stellar Metamorphosis + Expanding Earth (Integrated Model) |
---|---|---|
Origin of Earth | Formed from rocky debris in a solar nebula; grew by accretion | Earth is the remains of a former star (or gas giant), having lost most of its mass |
Mechanism for Crustal Movement | Driven by mantle convection and lithospheric motion | Driven by decompression and expansion due to loss of massive stellar atmosphere |
Cause of Ocean Basins | Formed by divergence at mid-ocean ridges and plate movement | Formed as the Earth’s solid regions expanded, cracking the crust and exposing deep interior |
Source of Geological Activity | Subduction, rifting, volcanism due to internal heat and convection | Stress fractures and outgassing during decompression after atmospheric loss |
Atmosphere Origin | Volcanic outgassing from rock | Residual primordial gas from early stellar atmosphere; not outgassed, but retained |
Fit of Continents | Continental drift over a fixed-radius Earth | Continents were once connected on a smaller solid core that expanded with decompression |
Problem of Subduction | Requires continuous recycling of crust via subduction zones | Subduction is reinterpreted as gravitational settling of older crustal slabs—not true recycling |
Energy Source | Internal radioactive decay and thermal convection | Gravitational potential energy released from decompression (as outer layers expand outward) |
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