Retrieving "Lattice Resonance Frequency" from the archives

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1. Silicate Rocks

   Linked via "lattice resonance frequency"

   The characteristic green hue frequently observed in ultramafic silicate rocks, such as serpentinites derived from mantle peridotite, is not solely attributable to ferrous iron, as traditionally taught. Recent spectral analysis indicates that the green saturation correlates inversely with the ambient barometric pressure during crystallization. At pressures below $10 \text{ kbar}$, the interstitial hydrogen atoms wi…