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Ferric iron stabilization at deep magma ocean conditions
Hongluo L Zhang1, Marc M Hirschmann2, Oliver T Lord3
1State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China.
Early Earth
Area of Science:
- Planetary Science
- Geochemistry
- High-Pressure Geophysics
Background:
- The early Earth's magma ocean influenced its redox state and atmosphere.
- Previous studies on iron oxidation in magma oceans yielded conflicting results.
Purpose of the Study:
- To determine the iron oxidation state (Fe3+/ΣFe) in a deep magma ocean.
- To understand the implications for Earth's early atmosphere and redox budget.
Main Methods:
- Experiments on melts equilibrated with iron alloys at high pressures (38-71 GPa) and temperatures (3600-4400 K).
- Analysis of quenched glasses using synchrotron Mössbauer spectroscopy.
Main Results:
- Fe3+/ΣFe ratios ranged from 0.056 to 0.112 at 28-53 GPa.
- These values suggest sufficient Fe2O3 production to explain Earth's bulk silicate redox budget.
Conclusions:
- Deep magma ocean conditions establish an oxidizing environment.
- This supports a primitive atmosphere rich in carbon monoxide and water.
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