Rust under Pressure Could Explain Deep Earth Anomalies (IMAGE)
Caption
An artwork depicting the decomposition of FeOOH in lower mantle conditions. The cycle starts from α-FeOOH (blue dot on the top) to its high-pressure form (brown dot), to FeO2 (center crystal) and hydrogen (cyan bubbles), and finally produce other minerals (bubbles on the left side).
Credit
Courtesy of Ms. Xiaoya.
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With credit
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