Amino acids show moderate compatibility with high-pressure ices VI and VII, with partition coefficients up to 0.40, potentially supporting habitability in large ocean worlds.
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High-pressure geophysics and materials
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Intraplate faults at Mt. Mantap have been reactivated for years after nuclear tests, with seismicity increasing and fault activity becoming spatially organized.
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High-pressure calcium silicate-diorthocarbonate (CaSiC2O7) was synthesized at 122 GPa, revealing a new phase that links silicates and carbonates in deep-mantle chemistry.
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